A holistic approach to the palaeoecology of Las Hoyas Konservat-Lagerstatte (La Huerguina Formation, Lower Cretaceous, Iberian Ranges, Spain)/ Una aproximacion holistica a la palaeoecologia del Konservat-Lagerstatte de Las Hoyas (Formacion La Huerguina, Cretacico Inferior, Cordillera Iberica, Espana).
Konservat-Lagerstatten deposits are distinguished by the quality of preservation of soft-bodied organisms (Seilacher, 1990). Konservat-Lagerstatten have been considered as the "end member of a continuum" in the preservational spectrum (Allison and Briggs, 1991). Various factors and combinations thereof can be involved in the genesis of any deposit, but exceptional deposits have been explained within the framework of three parameters: obrution, stagnation and bacterial sealing. This background, provided by Seilacher et al. (1985), thus offers a broad, simple classification. Konservat-Lagerstatten are usually interpreted as having resulted from the presence of specific palaeoecological and palaeoenvironmental factors, such as the presence of oxyclines or haloclines, biostratinomic factors involving rapid burial or factors related to necrolysis, such as the role of bacterial mats in slowing the rate of degradation of soft tissues and their authigenic replacement. Influenced by Seilacher's model most studies use the preservational potential of a particular environment (e.g., anoxic bottom, early phosphatization, rapid burial, etc.) to explain why fossils are exceptionally well preserved (see for instance Stinnesbeck et al. 2005 for the Late Cretaceous outcrop of El Rosario in Mexico). Concerning the relative abundance and absence of the preserved taxa, the composition of fossil assemblages is explained in ecological terms (environmental affinities and preferred habitats of species) rather than as taphonomic biases (see as an example Palci et al., 2008 for the Kolmen, Slovenia Cenomanian Lagerstatte).
For many decades Konservat-Lagerstatten have been considered a canon with maximum information, exceptional places where palaeobiological information has been somehow frozen, the succession of singular "catastrophic events" of mass mortality being the commonest explanation for these exceptional deposits (Shipman, 1975).
Konservat-Lagerstatten have revealed the existence of organisms that never fossilize under other conditions, and the anatomical details of organic structures that would otherwise remain unknown; in summary they have provided specialists with abundant key evolutionary biological data. Little would be known about the early evolutionary stages of marine life if the Burgess Shale and Chengjiang did not exist. They may be thought of as windows onto the fossil record, through which the best approaches to the studying the Earth's biological past can be pursued.
Assuming all these arguments are correct, it could also be argued that a realistic model of the representativity of this type of fossiliferous deposit with respect to palaeoecological aspects, among others, is methodologically handicapped. In other words, the Konservat-Lagerstatte model has become associated with a static or frozen view of palaeoecology that neglects the temporal sequence of events. In contrast a more dynamic perspective of a more holistic view, of the quality (i.e., preservation and bias) of the fossil record has been focused particularly in the marine realm, and structured within the sequence stratigraphic perspective (Holland, 2000). The advantage of this approach is that it accommodates many of the biases of the fossil record that vary over time and between environments.
It is not known yet if all of the Konservat-Lagerstatten are "palaeoecological windows" as they are for the studies on past biodiversity. It remains unclear what kind of palaeoecological information is transferred to the fossil record,that is, whether the Lagerstatten preserve their original dynamics and palaeoecological structure, and to what extent any bias is common to all Konservat-Lagerstatten.
Las Hoyas is a well-known Barremian (Lower Cretaceous) continental Konservat-Lagestatten, acknowledged as one of the most important Lower Cretaceous Lagersttaten in the world (Sanz et al., 2001). It is located at the Serrania de Cuenca (Iberian Ranges, east-central Spain) and occurs within the La Huerguina Limestone Formation. Since it was discovered in 1985 it has yielded several thousand ichnofossils and body fossils, the latter including Bacteria, Fungi, Protista (Foraminifera), Algae, and a wide spectrum of Plant and Animal phyla (Buscalioni et al., 2008; Fregenal-Martinez and Buscalioni, 2009, see below). It is especially well known as probably the best Mesozoic locality for fossil insects (Martinez-Delclos et al., 2004). The locality has provided palaeontologists with information critical to understanding the early radiation of birds and the development of flight (Sanz et al., 2002). It has also yielded significant information on the evolution and life habits of other organisms. For instance, articulated Characeae with their vegetative apparatus preserved were described first from Las Hoyas (Martin-Closas and Dieguez, 1998). The enigmatic Montsechia vidali has been interpreted as being an aquatic angiosperm on the basis of its ultrastructural preservation (Daviero-Gomez et al., 2006). The replacement of "holostean" by early teleostean faunas may be documented at Las Hoyas (Poyato-Ariza, 2005). Some of the most significant discoveries relate to the anatomy of the albanerpetontid Celtedens (McGowan and Evans, 1995), and the early evolution of Aves, for example the presence of a pygostile in Iberomesornis romeralli. The earliest known alula was recorded in Eoaulavis (Sanz et al., 1996; Sanz et al., 2002) (see http://www.yacimientolashoyas.es for a list of cases and references).
Most of the fossils are fully articulated (excluding macrophytes) and many preserve soft tissues, and organic patterns and structures rarely found in the fossil record: patterns of colouring, nerviation, gut tracts, and ommatidium of insects, stomach contents and muscles of fishes, skin and integumentary tissues of such as frogs, salamanders, lizards, crocodiles and dinosaurs.
The sedimentary succession of Las Hoyas is a continuous, cyclical accumulation of finely laminated limestones deposited in an area that on a regional-scale was a wetland environment, strongly influenced by subtropical, seasonal climatic conditions.
The comprehensive palaeontological and stratigraphical records of Las Hoyas, and the large amount of data retrieved from many years of layer-by-layer excavation, have allowed us to adopt a dual approach to reconstructing the palaeoecology of the fossil assemblage. The goals of the current study are therefore two-fold. The first is to perform a palaeoecological analysis based on sedimentological data, the taphonomic features of the fossil association, and the recorded biota. Since Las Hoyas is a Konservat-Lagerstatte, this analysis will consider the entire fossiliferous lithosome as a unique, minimally biased, taphonomic unit. The second goal is to determine whether palaeoecological information can be interpreted in the context of ecological dynamics, especially evolutionary dynamics, by analyzing Las Hoyas in the actual temporal and spatial framework provided by its stratigraphic record. This approach aims to be the starting point for advances in the concepts and methodologies of palaeoecology, encouraging analyses of dynamics, while questioning some traditional assumptions in this area of research.
In the light of the conclusions obtained from the palaeoecological analysis of Las Hoyas the value and meaning of Konservat-Lagerstatten from the palaeoecological perspectiveis also revised.
2. Geological setting
The Serrania de Cuenca is part of the Iberian Ranges, a NW-SE oriented mountain chain that covers an extensive area in the eastern half of the Iberian Peninsula and was generated by the tectonic inversion of the Iberian Basin. The Iberian Basin was an intracratonic extensional basin formed during the Late Permian-Early Triassic that remained active throughout the Mesozoic until the Alpine Orogeny.
During the Late Jurassic-Early Cretaceous the Iberian Basin experienced a rifting phase related to the opening of the central Atlantic and the rotation of the Iberian Plate (Salas and Casas, 1993). Four palaeogeographic domains have been defined for the Early Cretaceous of the Iberian Basin (Soria et al., 2000): Cameros, Central Iberian, Maestrazgo and South-western Iberian (Fig. 1A). Extensional tectonics divided each domain into many well-differentiated subbasins of graben and half-graben type.
The South-western Iberian Domain was limited by extensional fault systems running NW-SE (Vilas et al., 1982, 1983, Mas et al., 1982), with associated NE-SW systems of transfer faults that accommodated differences in extension rates.
The NE-SW Landete-Teruel transfer fault divides the South-western Iberian Domain into the Serrania de Cuenca and Valencia Basins. The Serrania de Cuenca Basin was in turn divided by the NW-SE extensional Hesperic fault to form two subsiding troughs (Una-Las Hoyas and La Huerguina). The Una-Las Hoyas Trough is composed of at least five small subbasins: Una, Buenache, Los Aliagares, Las Hoyas and La Cierva (Fig. 1B).
Barremian sedimentation in the Serrania de Cuenca occurred under continental environmental conditions and no direct marine influence is observed (Poyato-Ariza et al., 1998). Marine influence is restricted to the Valencia Basin which was bounded by the Tethys Sea at its eastern edge (Mas et al., 1982).
The climate of this area has always been considered to be seasonal subtropical with alternating wet and dry seasons. This interpretation is based on several sources of proxy climate data. Ziegler et al. (1983) performed a palaeogeographical and palaeoclimatic reconstruction and placed this area of the Western Tethys at the dry, divergent subtropical zone at a latitude of 25-30[degrees]N. Ziegler et al. (1987), on the basis of palaeobotanical data, proposed that seasonality occurred in tropical and subtropical areas, and a seasonal warm and semi-arid subtropical climate was assumed for the Iberian Plate during the Lower Cretaceous. Haywood et al. (2004) developed a model for Barremian Wealden climates of Western Europe using a Limited Area Model, which confirmed strong biannual seasonality of temperature, with mean cold-month temperatures of 4-8[degrees]C, and mean warm-month temperatures of 36-40[degrees]C. However, the model unexpectedly predicts an average precipitation rate of 4-8 mm/day for any one month, and more than 16 mm/day during the cold season. The model-predicted moisture budget results in very high evaporation rates, which greatly reduces moisture availability at ground level, thus accounting for the proxy data indicating dry conditions. Successive facies analyses of the Barremian deposits in different areas of the Serrania de Cuenca Basin have repeatedly shown sedimentological evidence of seasonality and highlighted climate as a extremely significant allocyclic control of sedimentation (Gierlowski-Kordesch et al., 1991, Gomez-Fernandez and Melendez 1991, Fregenal-Martinez and Melendez, 1993, Fregenal-Martinez 1998, Fregenal-Martinez and Melendez, 2000).
In the Serrania de Cuenca, Barremian sediments overlie Bathonian (Middle Jurassic) marine limestone unconformably (Fig. 1B); the latter underwent strong karstification during the Upper Jurassic and even during continental Early Cretaceous sedimentation.
Barremian continental deposits form two lithostratigraphic units linked by a lateral facies change: El Collado Sandstones Fm and La Huerguina Limestones Fm (Vilas et al., 1982).
The Una-Las Hoyas Trough exhibits little El Collado Fm, being filled mainly by deposits of the La Huerguina Fm. The thickest succession of the La Huerguina Fm occurs in the Las Hoyas Subbasin, which was infilled by almost 400 m of distal alluvial and palustrine-lacustrine deposits (Fregenal-Martinez 1998, Fregenal-Martinez and Melendez, 2000). The sedimentary record of Las Hoyas has been divided into four sequences (Fig. 1C) separated by local unconformities or paraconformities and named informally in ascending order as Rambla de Las Cruces I, Rambla de Las Cruces II, Pocillo del Pozuelo and Hoya de la Madre de Las Latas (Fregenal-Martinez, 1998, Fregenal-Martinez and Melendez, 2000).
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The fossil-bearing rhythmically laminated limestones of the Las Hoyas Konservat-Lagerstatte occur in the Rambla de Las Cruces II Sequence, which is entirely composed of carbonates and characterized by the dominance of palustrine-lacustrine facies over distal alluvial and flood-plain facies.
3. Conceptual and methodological framework
The two objectives proposed in this work relate to two distinct conceptual frameworks. The results will illustrate that the two approaches are complementary.
The first approach assumes a "static" palaeoecological interpretation, and is based on sedimentology and supplemented by palaeobiology and taphonomy. It enhances the functional relationships and the congruence among (i) the palaeoenvironmental hypothesis (addressed from the sedimentological analyses that establish the abiotic framework of the ecosystem), (ii) the taphonomic features of fossils (in terms of preservation of each fossil); and (iii) the relative abundance of fossils. The pattern of abundance refers herein not to the taxa themselves (as is common in this kind of study), but on the ecological categories that, according to the palaeoenvironmental hypothesis, should reflect a predicted structure. The use of ecological categories avoids the problem of rarity in species due to preservation, and furnishes the strong lines of the ecological structure, and it is thus likely to be a robust method of analysis. Epistemologically, the combination of the selected information about sedimentology, taphonomy and palaeobiology thus describes: 1) the potential for representativity, i.e., the fidelity of the composition of the palaeoecosystem, 2) the ecological dominance of the group of species that regulate the ecosystem, and 3) outstanding and significant palaeoecological processes that may explain the genesis of the deposit and its potential biases.
The second approach is "dynamic" in that it interprets the taphonomic assemblages with respect to environment and time. In other words, the significance of the taphonomic data including their distribution within the fossiliferous lithosome will be explained in terms of the sedimentological meaning (environment) of the various facies that host each different taphonomic assemblage, and the stratigraphic architecture that the facies sequences display (sedimentary evolution over time).
Dynamic reading with respect to the environment will provide key evidence about what Holland (2000) identified "facies bias", highlighting the environmental signal that controls differences in fossil abundance and richness. For this purpose the fossil associations present in all the facies have been compared.
Dynamic reading with respect to time will reveal the extent to which the structures of the fossil and sedimentary records are determined by the palaeoecological dynamics and whether there is an architectural taphonomic and sedimentary coupling. To this end, the succession of communities developed during every sedimentary sequence has been compared.
The taphonomic analysis performed to enable the dynamic reading includes the following criteria: the degree of demicity (vs. ademic) and autochthony (vs. allochthony) of the association (Fernandez-Lopez, 1989). Demic is a biological criterion, and is applied to those fossils that come from organisms that left ichnological traces or body parts, and/or that died in the same environment where they lived or that was their original habitat. Allochthonous is a taphonomic criterion applied to fossils that have been transported out of the place where the organism died or left any part. Whereas autochthonous refers to fossil that have been preserved where the organism died or left any part, no matter where they lived. For instance, in Solnhofen the famous horseshoe-crab fossil that left its trail before dying should be treated, applying those criteria, as ademic and autochthonous. This is the reason why Fernandez-Lopez (1989, 1991) suggested that each criterion should be considered independently to maximize its heuristic potential, and herein we follow his criteria (i.e., demicity and autochthony). The spatial fidelity concept used by Behrensmeyer et al. (2000) combines both sets of criteria (biological and taphonomic) without any explicit denomination of the weighting given to either, but the authors emphasised its relevance for understanding the preservational processes. Finally, this dynamic approach also gives a better appreciation of what has been called temporal resolution (Behrensmeyer et al., 2000), which is the finest scale temporal category into which the taphonomic association can be confidently assigned. Linked to temporal resolution is an evaluation of time-averaging (from virtually zero to millions of years), as the period of time represented by the biological components that comprise any fossil assemblage.
3.1. Data sampling and analyses
To deal with biases the primary requisite is to collect high quality data using appropriate fieldwork strategies. The database has been constructed using a systematic layer-by-layer sampling method. For each layer, the size and total number of specimens were first determined. Orientation was occasionally measured because Las Hoyas fossils are randomly distributed. Layer-by-layer excavation of square areas of 25 [m.sup.2] on average was carried out (Fig. 2). A total volume of more than 3000 [m.sup.3] rocks was excavated.
To address the palaeobiological framework we used the complete taxonomic list of Las Hoyas, which includes information from systematic and random sampling methodologies. The taxonomic list is periodically improved by taxonomic revision carried out by specialists.
To address the sedimentary framework, the laminated limestones were exhaustively and continuously sampled. These limestones have a homogeneous appearance in the field and facies successions and associations have to be reconstructed under a petrographic microscope (Fig. 3). To this end, sampling covers the entire thickness of the excavated areas, and thin sections of rock sample were used for the microscopic description. Samples were taken while palaeontological excavation was being performed, in such a way that the fossil content of the sampled layers was always known. Herein we present the results of five years of excavations in which five contiguous areas were systematically sampled, each area being given the name of a colour (Figs. 2 and 4): 1) pink 1996, 2) pink 1998, 3) lower black, 4) upper black and 5) lowermost black. The sampled laminites were almost one metre thick in total and were composed of three elemental sequences (Fig. 4).
The raw data summarize the total number of fossils discovered (see Table 1 and Appendix 1). "N" takes into account only body fossils, although in the discussion other some relevant fossils are considered qualitatively, such as "worms", coprolites and ichnofossils, that have not been quantitatively analysed because the sampling technique and taxonomical identifications progressively improved, and thus data accuracy differed slightly between areas. Consequently, neither plant remains nor other trace fossils such as coprolites and ichnofossils are included in the account provided in Table 1.
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4. Characterization of Las Hoyas Konservat-Lagerstatte and its ecosystem: "static" approach
4.1. Paleoenvironmental reconstruction and sedimentology of Las Hoyas deposits
The picture that emerges when palaeogeographical, stratigraphical and sedimentological data are analyzed in terms of a palaeoenvironmental reconstruction for the Barremian in the Serrania de Cuenca is that of an extensive subtropical (seasonal, winter wet), continental (freshwater) wetland system, dominated by carbonate sedimentation that overlay a low-relief karstic terrain. A flat, smooth, topography with localized ridges of Jurassic limestones at the edge of the sub-basins at the time of deposition was the general landscape. Consequently, the watershed, and source areas of sediments would have been mostly composed of carbonates.
The groundwater and surface waters draining the basin would therefore have contained a high concentration of dissolved calcium carbonate that enhanced the pedogenic and biological production of carbonate and maintained basic pH conditions in ephemeral and permanent water bodies. The wetland landscape comprises the typical environmental mosaic within these depositional systems: alluvial plains, marshy and swampy palustrine plains, different types of channels, sloughs, ponds and shallow permanent lakes.
Strong seasonal differences in landscape geomorphology reflect water availability, which was greater during the wet season. During this season ponds and lakes had their highest water levels, palustrine and alluvial plains were flooded and all channels were active. During the dry season most ponds dried out, lakes had low water levels, alluvial and palustrine plains were subaerially exposed and dominated by pedogenic processes, and ephemeral channels remained inactive.
As in modern subtropical wetlands fire was an active element in these environments, and charcoal is abundant in different facies. Charcoal in flash-flood deposits is of particular significance, and suggests an association between fire and strong seasonal storms followed by flooding. Blacked pebbles and charcoal associated with palustrine deposits indicate that the other common cause of fire in these environments was spontaneous combustion with inorganic-rich palustrine soils.
The paleogeographical distribution of the different elements of the environmental mosaic reflected local conditions and each sub-basin had its own specific set of environments, e.g., permanently flooded wetlands and lakes located in specific depocentres. The type of channels varied depending on the proximity to watersheds and source areas, and palustrine and pedogenic environments were associated with non-subsiding areas, such as sub-basin margins.
The fossiliferous sediments of Las Hoyas are finely laminated limestones composed almost entirely of calcium carbonate with a small fraction of clays and organic matter. These sediments accumulated in a hard water, periphyton-dominated wetland, which was covered by thick microbial mats, and underwent strong, climatically driven cyclical oscillations of the water level.
Despite the homogeneous field appearance of laminated facies, two alternating facies associations, and several transitional facies between them have been distinguished petrographically (Fig. 3).
The first association is the result of sedimentation by traction and decantation of allochthonous detrital carbonate particles and vegetal debris, chemical and bio-induced precipitation of calcium carbonate, and accumulation of thin microbial mats (Fig. 3, blue framed). These were deposited during seasonal flooding and longer-term wet periods during which high water levels favoured more lacustrine conditions.
The second association reflects the autochthonous production of carbonate linked to the growth of microbial mats that grew massively during dry periods when the water column was drastically reduced to probably just a few centimetres deep. Microbial mats and laminae of very fine detrital carbonate sediments with debris of plants and other organic remains were transported during occasional floods and form sediments deposited during dry periods (Fig. 3, pink framed). The association of dry period sediments with dinosaur and crocodile trails and isolated tetrapod tracks, as well as the sparse presence of desiccation cracks, are indicative of extreme low water levels, and support strong water level oscillations between wet and dry periods. Preliminary geochemical data from carbon and oxygen isotopes (Talbot et al., 1995) suggest that Las Hoyas sediments were derived from karstic water. Therefore, the groundwater might have maintained a thin persistent water cover, or at least a certain level of humidity in the sediments, thereby avoiding frequent complete desiccation. Some drought events are implied by the presence of desiccation cracks.
Preservation of laminated sediments requires a special set of environmental conditions; in particular destruction of lamination, mainly by bioturbation, must be avoided. Anoxia is often invoked to explain such conditions. Since thermal or chemical water stratification processes are unlikely to occur in shallow freshwater subtropical lakes and wetlands, it has been hypothesized that the warm environment, prolonged periods of water stagnation, and the high rate of accumulation of organic debris carried by floods provided the conditions required to maintain anoxic to dysaerobic conditions in the sediments and bottom waters, and prevent reworking of sediments by bioturbators.
4.2. Fossil taphonomic features
Fossils from the laminated limestones of Las Hoyas show no evidences for having been transported over long distances, elements are not broken or abraded, indicating all were or produced close to their burial place (parautochthonous). 70-80% of the fossils are fully articulated. The exoskeletons of crustaceans show few disarticulated appendages or antennae (Rabada, 1993). Insects, which have been more extensively studied, are mostly articulated, especially aquatic species. Aquatic plants (Charophytes, the supposed angiosperm Montsechia and the fernWeichselia) have thalli, stems and fructifications preserved (Martin- Closas and Gomez, 2004). Fish scales preserved in situ and their axial columns and tails remain articulated. Tetrapod skeletons show limited dispersion of body elements with respect to the degree of articulation and overlapping. The autochthonous condition of fossils is consistent with data from molecular taphonomy, suggesting a dominant aliphatic composition of fossil fish scales, plants and decapods, which probably arose from the incorporation of lipids from the original organic sources, indicating preservation by in situ polymerization of labile aliphatic components (Gupta et al., 2008).
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Early ontogenetic stages (juveniles) and adults are commonly present. Numerous moults (exuviae) of young individuals of the heteropterans belostomatid Iberonepa romerali have been noted (Martinez-Delclos, et al, 1995), and mayflies, flies and coleopteran larvae are quite frequently present (Soriano, 2006; Fregenal-Martinez et al., 2007). Several juvenile salamanders, frogs and crocodilians have been discovered (Ortega et al, 2003). The presence of juvenile and adult dwarf organisms such as fish and belostomatid insects is a common pattern at Las Hoyas, which shows a remarkable bias toward small fossils.
Las Hoyas is a Konservat-Lagerstatte that preserves a broad range of organic components: mineralised muscle, tissue imprints, chitin, cellulose, lignified cellulose, shelly and apatite skeletons (Fig. 5). Preserved eyeballs and peritoneal membranes in fish, and even white banding that may correspond to mineralised replicas of myomeres are quite common. Other examples are the mineralised muscle of the dinosaur Pelecanimimus (Briggs et al, 1997), and the tissue imprints obtained from the albanerpetondid Celtedens. The scaly skin and eyelids, the fingers and toes tightly curled into the centre of the hands and feet, and the intact skin all suggest that this albanerpetondid may have died and dried out (become mummified) before arriving at the burial place (McGowan and Evans, 1995). The crocodile Montsecosuchus has preserved scaly skin and Eoalulavis has limonitized feathers preserved.
Insects and crustaceans are preserved as moulds or mineralised replicas, or as impressions preserving organic matter (Delclos et al. 2004). Some mecopterans and belostomatids preserve their colour pattern, and their tracheal and gut tracts. Some specimens of the Delclosia carid shrimp preserve digestive organs and eyes. Macroplants are preserved as impressions or as carbonaceous films. Articulated leaves and seeds are abundant, as are stems, twigs, cones and inflorescences. Palynomorphs have also been preserved.
Potential mechanisms that explain the taphonomic features of Las Hoyas are, in descending order of abundance: microbial mats (i.e., bacterial sealing), anoxia and rapid burial by sediments or rapid inclusion in microbial mats.
The contribution of microbial mats (coccoid and filamentous bacteria) has been directly observed in the preservation of tissue imprints in fish eyes (Gupta et al., 2008) and in the dinosaur Pelecanimimus polyodon (Briggs et al., 1997). In this latter, the existence of either a throat pouch or a soft occipital crest demonstrates the importance of microbial mats in preserving soft tissues. The presence of microbial mats might also be confirmed in aquatic insects (Delclos pers. comm.). In belostomatids (Iberonepa), the inference of microbial mats arises from the analysis of overlapping areas of a body. The mat prevents sediment infilling the cavities and spaces between body parts. The leg and abdomen of Iberonepa may be observed only in the absence of sediment. The confining effects of microbial mats and algae might also promote phosphatization of soft parts, such as gut tracts of fish and aquatic insects and of insect ommatidium.
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The near-completeness of articulated appendages in carid decapods, such as the aquatic Delclosia, and bony elements in the terrestrial lizard Hoyalacerta and the aerial aves Concornis, suggest that burial events (or entombing inside microbial mats) were rapid. The comparison of the taphonomic features observed and the results of taphonomic experiments indicate that burial might have taken place in less than 20 days (Briggs, 1995; Cambra-Moo, 2003; Cambra-Moo and Buscalioni, 2003).
The initial results of a laboratory study using tanks to grow microbial mats under controlled conditions were reported by Iniesto et al., (2009). Fish and insect carcasses are placed upon the mat to measure the time elapsed until embedding by the mat growth, and to observe the decay processes inside the mat. Rapid entombment occurs during this process, and in as little as two weeks individuals become completely covered. They remain fully articulated, retaining delicate anatomical details even after months of decay.
Preservation of body and trace fossils along with laminated facies requires a special set of environmental conditions. As discussed above anoxia is inferred from sedimentological and palaeoichnological analyses to account for such a preservation of fossils and sediments. Ichnological analysis indicates that the Las Hoyas invertebrate ichnofauna (Mermia ichnofacies)displays evidence, such as dominance of superficial structures, the paucity of infaunal traces and a small size that indicate environmental stress due to lack of oxygen, (Buatois et al., 2000) consistent with an environment with short periods of oxygenated bottom waters, but permanently anoxic interstitial waters.
4.3. Ecological structure
In terms of biodiversity, metazoans are represented by at least five or six phyla (Porifera, Mollusca, Arthropoda, Chordata and Vermiform animals, such as Nemertina and Annelida) and plants by four (Phycophyta, Bryophyta, Pteridophyta and Spermatophyta). Around 15 families and 17 genera of plants, and 50 families and 80 genera of metazoans have been documented, aquatic organisms being the most abundant. To date, the list of genera has yielded N=132, of which arthropods are by far the most diverse group, representing 45% of the genera from Las Hoyas (Fig. 6). The arthropod Classes present are Arachnida, Diplopoda, Crustacea and Hexapoda. The hexapoda is represented by 13 orders (Ephemeroptera, Odonata, Blattodea, Isoptera, Orthoptera, Archaeorthoptera-Chresmodidae, Hemiptera, Coleoptera, Hymenoptera, Trichoptera, Neuroptera, Mecoptera and Diptera) and 40 families (Fregenal-Martinez et al., 2007). The next most abundant groups are the Pteridophyta (15%) and Ostheichtya (14%), while the others (Charophyte, Bryophyta, Mollusca, Amphibia, Squamata and Archosauria) make up the remaining percentage of the taxa identified so far (Fregenal-Martinez and Buscalioni, 2009). Thus, the bulk of the taxonomic diversity (67%) at Las Hoyas is based on arthropods (mainly insects) and plants (Pterydophytes, Spermatophytes, Bryophytes and Algae).
Consistent with sedimentological and palaeonvironmental studies, our working hypothesis is that Las Hoyas was a shallow periphyton-dominated wetland that formed part of a regional-scale depositional system made up of seasonal tropical wetlands. Consequently we would expect the ecological structure to contain: 1) a complex vegetation structure, 2) animal ecology dominated by aquatic taxa, and 3) as wetlands are a mixture of transitional habitats, a hybrid of ecotones with aquatic to terrestrial plants and animals present. This broadly defines this ecosystem as an open system with no clear ecotones that generates a wide variety of microhabitats and environmental mosaicism linked to water availability. This definition is in accordance with the essence of modern wetlands provided by van der Valk (2006).
Complex vegetation structure and insects
Trophically modern wetland systems are based on the abundance of macrophytes, algae and organic detritus, and on the quality and relative abundance of insects as the second scale of primary production (Batzer et al, 2006). As a wetland Las Hoyas is characterized by the extraordinary dominance of periphytons as revealed by features of its sediment and the exceptional fossil preservation.
The depositional system in which Las Hoyas was located would have been profusely vegetated (Martin-Closas, 2005). The complexity of the vegetation is characterized by the presence of submerged aquatic algae and plants. A very important part of the Las Hoyas fossil assemblage is comprised of aquatic plants. Two types of aquatic macrophytes are the most abundant: charophyte algae (Martin-Closas and Dieguez, 1998), and the early aquatic angiosperm Montsechia (Daviero et al., 2006). Their taphonomic preservation and relative abundance reveals these to be autochthonous. Other aquatic hydrophytes such as the enigmatic Ranunculus ferrerii, or the floating plant Proteaephyllum reniforme are rare at Las Hoyas.
There is a high diversity of terrestrial macrophytes. Of the heliophytic plants, conifers are the best represented, with a great diversity of Cheirolepidaceans, Taxodiaceans and Podozamites preserved as leaves, branches and cones. One of the most abundant is the Cheirolepidaceae Frenelopsis. Ferns are dominated by the Mantoniaceae species Weichselia, fossils of which vary in the type of preservation: articulated, fragments of pinnas and pinnulas (occasionally burnt). Bryophtes (Thallites) and herbaceous ferns such as Onychiopsis are fairly abundant, while other herbaceous ferns, such as Cladophlebis and Coniopteris, are frequent to rare in the assemblage. Terrestrial angiosperms are rare, although several leaf types have been recorded in the locality (Barral-Cuesta and Gomez, 2009). Frenelopsis might be adapted to riparian habitats and grew in lacustrine environments (Gomez et al., 2003), while ferns and mosses might form part of moist soil species, or form part of limestone outcrop communities.
High insect diversity and the wide spectrum of ecomorphotypes represented (zooplanktivorous, herbivorous, carnivorous, scavengers, xylophagous, saprophagous) reflect the environmental mosaicism of wetland systems. Abundance is biased towards aquatic insects that exhibit a wide range of ontogenetic stages (from larvae, pupae and exuviae to adults). Conversely, terrestrial forms are less abundant but more diverse, and in terms of preservation insects are represented by complete specimens and by isolated body parts mostly wings. This is demonstrated by coleopterans (Soriano, 2006) where abundance is concentrated in the aquatic family Coptoclavidae, but diversity increases in the terrestrial forms Cupedidae and Scarabaeidae. Semi-aquatic insects and other groups living around vegetation and water bodies include grasshoppers, crickets, dragonflies, or neuropterans, caddis fly larvae and some larvae of the beetle Coptoclavidae (for details see Ponomarenko & Martinez-Delclos 2000, Soriano et al. 2007). Parandrexidae beetles, Cupedid reticulated beetles, weevils and several forms of cockroaches and termites are associated with terrestrial environments, above all with wood and fungi (Martinez-Delclos 1991, 1993, Zherikhin and Gratshev 2003, Soriano et al. 2006, Soriano and Delclos 2006). Arachnids, particularly orbweaver spiders, also form part of the terrestrial cluster (Selden and Penny, 2003).
The lentic freshwater ecosystem of Las Hoyas contains one of the most significant records described for the Early Cretaceous (Sanz et al., 2001). The organization of animal ecology at Las Hoyas has been analysed using the ecological categories defined for extant wetlands. The aim is to test to the extent to which an ancient ecosystem might correspond in composition and relative abundance those characteristics of modern systems. These categories are founded on the life cycles and the dependence of animals on wetland hydrology. The species can be grouped in the following categories: (1) obligate aquatic: found either in the water column or in flooded soils, (2) amphibious: species considered to spend at least part of their life cycle in wetlands and the remainder in some terrestrial environment, (3) facultative: species that may be found in wetlands and terrestrial environments, and (4) incidental: species occasionally found in wetlands.
Results from Buscalioni et al. (2008) reveal that Las Hoyas was dominated by obligate aquatic taxa (64%; in this previous study arthropods and macrophytes were excluded, although crustaceans, and some insects groups are also obligate aquatic), 24% of amphibious taxa, but fewer facultative to incidental forms (12%).
Of the obligate aquatic organisms, there are thousands of fish specimens. They are focal wetland animals because they are keystone species in terms of their ecological role, the productivity of wetlands being mainly based on fish biomass (Batzer et al., 2006). As a general condition, most dominant fishes in modern wetlands are small-sized species and small individuals. Protected wetland areas, as seems to be the case for Las Hoyas, are places selected by fished for protection from predators and as nesting areas. This would explain the bias towards juvenile individuals at this locality. Las Hoyas is not special in this sense, since the most abundant individuals are small juveniles of Notagogus (Wenz and Poyato-Ariza, 1994), anda basal teleostean fish, formerly related to "leptolepids" (Poyato-Ariza, 1997). Other teleostean species, such as the genera of the family Chanidae, Gordichthys and Rubiesichthys, are frequent, and are also small species. Species with a medium-to-large body size are less abundant. These include pycnodontiform fish like Turbomesodon, the coelacanth "Holophagus" (one of the largest), Lepidotes, and several amiiform species (Vidalamia, Caturus and Amiopsis) (Poyato-Ariza and Wenz, 2004).
The most abundant aquatic insect is the belostomatid Iberonepa, which has adaptations for active swimming, with its appendicular segments transformed into paddles. Less abundant although still frequent are insects that exhibit morphological aquatic adaptations for locomotion or feeding strategies, such as coptoclavid coleopterans, chresmodids, dipterans larvae, odonates, anisopterans (see Fregenal-Martinez et al, 2007 for a summary). Most aquatic insects depend on plant shelter. The presence of mayflies (Ephemeroptera), preserved as nymphs and adults at Las Hoyas, might indicate oxygenated waters, since oxygen stress prevents many aquatic animals groups from occupying poorly oxygenated wetlands (Mendelssohn and Batzer, 2006). This condition is supported by the absence of midges (Chironomids), which are the aquatic insects best adapted to low oxygen levels in modern wetlands (van der Valk, 2006).
Decapods are the most abundant invertebrates in Las Hoyas. Their trophic regimes range from omnivorous to scavenging (for the astacid decapod Austropotamobius, Garassino, 1996) to feeding on periphyton (as may be the case for the shrimp Declosia, since it occurs in modern relatives; Burns and Walker, 2000). The presence of peracarids, the minute spelaeogriphaceans, with a poor and patchy fossil record, and today live in fresh groundwater limestone caves should also be noted (Jaume, 2008). Other crustaceans, such as ostracods, have also been recovered at Las Hoyas, associated with mass mortality or invasion, as well as other invertebrates made up of a plethora of rather small- to medium-sized worm-like organisms whose taxonomy is difficult to establish because no fossil record is described for them.
Unionid bivalves and conchostraceans are also present and reveal that Las Hoyas water would have been alkaline, since the recent equivalents of these organisms typically live in alkaline waters, ranging in pH from 6.6 to 9.5 (for unionids see Good, 2004). Water alkalinity was deduced from independent criteria using sedimentological and geochemical sources (Poyato-Ariza et al, 1998). The amphibious category gathers those species that are considered to spend at least part of their life cycle in wetlands and the remainder in a terrestrial environment; albanerpetontids, anurans, caudates as well as chelonians and crocodylomorphs form part of this category. Albanerpetontids and crocodylomorphs are by far the most dominant groups.Turtles are rare (a new centrocrytodyrian turtle is represented by three juvenile specimens that do not exceed 20 cm in body length). Within this category some taxa might be more terrestrial and less water-dependent. For instance, the albanerpetontid Celtedens had terrestrial adaptations. In contrast, the salamander 'Hylaeobatrachus' retained its external gills and is therefore definitely fully aquatic (Evans and Milner, 1996). In the same sense, two groups of crocodylomorphs are included in this biota, one with terrestrial adaptations (a gobiosuchid, Buscalioni et al, 1996, Ortega, 2004) and the other possessing aquatic life habits (advanced neosuchians). It is worth noting that most of the recovered specimens in the amphibious category are juveniles and/ or small-sized species.
Facultative species are diverse but rare. Lizards and dinosaurs were facultative and incidental terrestrial components of this biota, respectively. The terrestrial habits of the Las Hoyas lizard biota include the runner Meyasaurus (the most abundant species), the climber Scandensia and the burrower Hoyalacerta (Evans and Barbadillo, 1998). Non-avian dinosaur body fossils are extremely rare, and the group comprises medium- to small-sized individuals, among including the ornithomimosaur Pelecanimimus (Perez-Moreno et al, 1994). Dinosaur ichnofossils are fairly common, although their presence seems to be linked to particular palaeoenvironmental settings (see below). Pterosaurs have also been categorized as facultative to incidental organisms. Fossils belonging to this group occur as isolated teeth and a partially articulated skull (Vullo et al., 2009).
Birds, the other focal wetland animals, can be considered to fall within a wide range of categories from amphibious to incidentals. Las Hoyas has yielded a high diversity of Enantiornithes aves. Species recorded (Iberomesornis romerali, Eoalulavis hoyasi and Concornis lacustris) have interpreted as being perching enantiornithines of reduced size with enhanced flight capabilities, allowing low speed flight and good manoeuverability (Sanz et al, 2000, 2002; Ortega et al, 1999). The life history of enantiornithes may be more strongly linked to wetland ecosystems than was previously thought. For instance, Eoalulavis (Sanz et al., 1996) adopted limicol habits, feeding on worms and crustaceans at the shores of water bodies, and the morphology of these birds (e.g., long legs with long toes) might also represent limb adaptations as in modern wading birds.
4.4. Concluding remarks
In summary, the interplay among the sedimentary analyses, taphonomy and ecological structure confirms the palaeonvironmental hypothesis that stresses four important features of the fossil record at Las Hoyas: 1) Compared with modern wetland ecosystems in terms of recorded phyla and diversity, Las Hoyas is highly representative, i.e., it has a high fidelity of composition: its fossil record "captures the original biological information faithfully, accurately, truthfiilly" (sensu Behrensmeyer et al, 2000). 2) When relative abundance is taken into account, macrophytes, arthropods (crustacean and aquatic insects), and small teleostean fish are the dominant taxa, as would be expected from the freshwater environmental setting. A diverse assemblage of animals including aquatic insects, ostracods, crayfish, and juvenile and small adult fishes depended on plant cover for their development and shelter. In fact, with respect to the obligate aquatics, the epibenthos and epiphyton of the Las Hoyas ecosystem is the habitat containing the greatest relative abundance. 3) The strong influence biofilms in the association are abundant and play a major role in fossil preservation. 4) Some groups in the fossil association corroborate or improve our knowledge of particular abiotic conditions of the ecosystem.
5. Assembling the taphonomic and stratigraphical records: assessing biases and interpreting dynamics. "Dynamic" approach
The palaeoecological reconstruction of Las Hoyas ecosystem outlined above is part of an integrated research effort. Many of the details that can be identified regarding particular morphological adaptations reflect the unique conditions of preservation of the Konservat-Lagerstatten. From this perspective, it may be said that Las Hoyas as a Konservat-Lagerstatte is a "canon" of preservation with maximum information, i.e., a minimally biased association in which information can be directly read because of the very high fidelity of its composition (Behrensmeyer et al, 2000). If this is true Las Hoyas might be used a priori as a reference or model to reconstruct the palaeobiology and palaeoecology of other, similar, Lower Cretaceous freshwater deposits.
Reconstructions made by considering the complete fossil content are essentially a "frozen picture" of the landscape with its flora and fauna. This "static" approach is compromised by the intuitive observation that ecological dynamics are never preserved as such. In effect, this method cannot avoid flattening the ecological and taphonomic processes to a single entity, amalgamating data or processes that came from different ecological dynamics in the palaeoecological reconstruction. As no other sources of bias are taken into account, the diversity recorded might be distorted and result in an incongruent assemblage.
To address this problem, we employ a dynamic approach to palaeoecological reconstruction, and explore whether Las Hoyas in particular, and Konservat-Lagerstatten in general, behave assingle entities. In other words, we attempt to establish whether Las Hoyas represents a unique ecosystem that can be regarded as a taphonomic unit. Therefore, we will place the palaeobiology and taphonomy of Las Hoyas within its actual spatio-temporal framework, and address the following key questions:
What is the specific bias of Konservat-Lagerstatten deposits? How can we prospect the resolution (temporal) and fidelity (spatial) of the "canon" itself? Does a unique taphonomic structure explain the abundance?
Is the total recorded diversity better explained in terms of time resolution? By this we mean: does Las Hoyas provide such temporal stratigraphic resolution that would reveal successive ecosystems? Alternatively, is the more general explanation in terms of spatial fidelity the better one? In other words, does Las Hoyas provide evidence of isochronous laterally coexisting ecosystems?
How are sedimentary tempo and, biological and/or ecological tempo related?
5.1. The stratigraphic record of Las Hoyas
Temporal distribution of palaeobiological information is strongly dependent on the structure of the stratigraphic record. An adequate palaeobiological interpretation requires a detailed understanding of the stratigraphical architecture in terms of time and sedimentary environments. However, this relationship has not always been well understood or given sufficient emphasis. Different approaches to assess either palaeobiological or stratigraphic completeness have been used (Kidwell, 1991, 1993). Holland (1997, 2000) showed how introducing sequence stratigraphy in macroevolutionary analyses results in a predictive model for bias in the large-scale structure of the fossil record.
Sedimentology is an essential tool for establishing the environmental context, the landscape of reconstructed fossil ecosystems, and for comparing data with the biostratinomic hypothesis. For these reasons, it is currently considered extremely relevant in palaeoecology (Behrensmeyer et al., 2000). Nevertheless, on reviewing the palaeoecological literature it becomes obvious that the potential when analyses of the stratigraphical architecture, sedimentology and the fossil record are combined to provide palaeoecological hypotheses, has been underestimated. The stratigraphical record of each sedimentary basin has a specific set of features or patterns that, as in biostratigraphy, may contribute to creating or enhancing bias and artefacts at different scales. These may be relevant to our understanding of the dynamics of palaeoecological communities.
The record from Las Hoyas, as with other lacustrine localities, is an exceptional palaeoenviromental archive with high temporal resolution (Cohen, 2003). The continuity and temporal resolution of the lacustrine deposits of Las Hoyas (low time averaging) and its unique palaeobiological and taphonomic features qualifies Las Hoyas as a natural laboratory where reconstruction of ancient Mesozoic continental ecosystems can be carried out within a dynamic context (Buscalioni and Fregenal Martinez, 2003).
Las Hoyas is made up of two facies associations that correspond to sedimentation during wet and dry periods (see section 4.1 and Fig. 3).
The stratigraphic arrangement of facies follows a cyclic vertical pattern (Figs. 3 and 4), primarily controlled by the seasonal alternation of wet and dry environmental conditions. This basic alternation is arranged in elemental sequences made up of a variable number of single laminites, numbering up to several hundred (Figs. 3 and 4). These sequences are 20- to 50-cm-thick, laterally persistent sequences, with sharp and well defined lower and upper boundaries. The lower part is dominated by facies developed during a wet period, gradually moving upwards to facies representing drier periods. Thus, each elemental sequenceisconsidered equivalent in terms of temporal meaning and tendency to other well-known cycles, such as metric to decimetric cycles made up of marls, charophyte limestones and palustrine limestones representing infilling and reduction of the depth of small lakes and ponds.
Wet and dry periods of the elemental sequences reflect cyclicity imposed over the annual seasonal cycles. Such long term cyclicity might have been controlled by a combination of climate and other allocylical processes. Determining the time represented by each elemental cycle is not easy, but given their nature and origin, the order of 103 years might be a reasonable estimate (Buscalioni and Fregenal-Martinez, 2003).
5.2. Environmental dynamics: facies bias
Due to the specific nature of the sedimentation processes involved in forming Las Hoyas (continuity and high temporal resolution) each lamina is considered to represent a snapshot, with fairly instant (census) time averaging. Assuming this, we can infer associations (recognised by the presence of the same species in several assemblages) made of the piles of successive assemblages. Many associations at Las Hoyas are characterised by: i) instantaneous events such as daily activity (e.g., digestion, mass mortality), or ii) high proportion of demic organisms (e.g., with serial of ontogenetic stages) and autochthonous fossils accreted in short-scale events of fossil accumulation, all of which are of similar size and preservation type.
[FIGURE 7 OMITTED]
The relationships between the sedimentation during wet and dry periods and fossil associations in each facies have been compared independently of the elemental sedimentary cycle from which they were retrieved. The objective is to reveal the changes that each environmental signal produces in the pattern of association.
There were 764 fossil specimens in the dry association, and 76 in the wet association (Table 2). When coprolites and "worms" were considered the total number of sampled fossils was 829 and 93, respectively. This disparity in the results can be interpreted by using rarefaction curves (Fig. 7) that compare taxon counts in samples of different size. The curve shows that wet and dry facies have different rarefaction curves. Wet associations are richer despite their low abundance, while dry associations are strikingly abundant although homogeneous. Wet and dry episodes differ not only with respect to the total number of fossils but also in their richness and taxon content. These peculiarities are reflected in the resulting richness and diversity indices (Table 2).
Characterisation of the association in dry facies follows its own model, in which time-averaging seems to be of a lesser order of magnitude than for wet periods. This rich association could be the by-product of dense microbial mats, probably acting under a shallow water layer. Fossils trapped by the microbial mat show that a reliable sequence of ecological events occurred in the wetland during periods of environmental stress: bioturbation (invertebrate traces), ostracod invasion, periodic storms, coprolite or "worm-larva" accumulations, and mass mortality of small juvenile basal teleosteans and/or crayfish. Accumulation by mass mortality and tetrapod traces contributes hundreds of elements.
The analysis of the fossil associations shows that demicity and autochthony are the major features of the dry associations. This can also be applied to shallow water inhabitants of the dry episodes formed by small juvenile teleostean fishes, carid shrimps (Delclosia), peracarid spelaeogriphaceans and astacid decapods (Austropotamobius) together with the presence of the aquatic angiosperm Montsechia. Necktonic fish, epibenthonic shrimps, and peracarids are dominant elements (up to 65% and 25% of the total amount of body fossils in dry facies, respectively).
The fish association is characterised mainly by small animals (mean body length, 15 to 20 mm). In dry associations, juvenile basal teleosteans ("leptolepid-like") are dominant elements whose ecomorphotypes have been associated with plankton filter organisms (Poyato-Ariza, 2005). Furthermore, the fish assemblage (i.e.,"leptolepid-like", Notagogus, Pleuropholis, Rubieschthys and Gordichthys) features low fusiform bodies, whose skeletons have led these species to being functionally interpreted as active swimmers (Rubieschthys), or dwellers of superficial waters (basal teleosteans and Gordichthys) (see Poyato-Ariza, 2005, for fish ecomorphology). One of the striking characteristics of the association is the low proportion of insects, as a whole (except for aquatic heteropterans), during long drier intervals. Finally, occasional exclusion between the aquatic plants, Charophytes and Montsechia, apparently occurs.
Wet facies are proportionally rich, because almost all specimens belong to different taxa (genera or species). Plant debris is the most commonly found type of remain. Fieldwork observations record "bad-preservation" for these fossils (in the Las Hoyas preservational context), and denote the presence of isolated elements such as scales, or non-articulated fish bones. Wet facies show different fossil preservation compared with dry facies. Although the wet sample is limited, insects, Lepidotes and Pycnodontiform fish dominate wet assemblages. Fish have distinct bulky and globular body shapes characteristic of oscillatory locomotion, with average sizes of up to 55 mm at Las Hoyas (the largest individuals are about 500 mm). Insect distribution is bounded by wet episodes, i.e., they were collected in the wettest facies and in wet facies bounded by drier ones. Insects collected are either aquatic (Iberonepa, Torcanepa, Diptera, Ephemeroptera and Odonata larvae) or terrestrial (Blattodea, Chresmodidae, Chrysopidae and Kalligrammatidae). The abundance of aquatic forms exceeds the terrestrial ones. Moulds of Iberonepa have also been retrieved, implying a demic production of these body fossils. The insect diversity (more than six species) in these facies is extraordinary. The increase in insect diversity in wetter facies is not unexpected since, as a general pattern, their life cycles are related to flooding or wetter periods in modern wetlands (Mendelssohn and Batzer, 2006).
Neuston may represent 44% of the total sample in some cases, while nektonic organisms account for only 13%. During wet periods the positive water balance would promote more lacustrine conditions and a deeper water layer. The presence of big fishes in the association strengthens this assessment. Medium- to large-bodied fish are thought to be bottom dwellers (Pycnodontiforms), and show an efficient hydrodynamic design (Lepidotes) (Poyato-Ariza, 2005). Transport of materials, including potentially carcasses, is common in wet facies; some laminae have a tractive origin. Wet episodes might recover carcasses previously exposed subaerially (mummified in some cases) or in litter (i.e., plant debris), whereas dry episodes are able to capture organisms produced by means of microbial mats.
Cluster analysis reveals the internal structure of the data (Table 3 and Fig. 8) segregating wet from dry cases. This result demonstrates that fossil association is sensitive to environmental conditions. Discriminant analysis (using the percentage of relative abundance for each variable) performed to classify each type of environment, yields equivalent results (Table 4). When cross-validation is carried out with respect to the discriminant predictors obtained, the fossil associations are correctly classified in 89% of cases (95% of wet cases N=20, and 90% of dry N=26 are well classified). Discriminant analysis is used to confirm visually the hypothesis that there are two distinct associations, whereby the wet association is characterized by higher insect diversity plus Lepidotes fish, while the dry association typically features an abundance of "leptolepid-like" fishes and crustaceans (Fig. 9 and Table 5).
The environmental conditions in wet and dry facies associations define two distinctly biased taphofacies. There are differences in fossil abundance, richness and preservation quality. Since facies characterisation documents two ends of a spectrum of environmental conditions, a mixture of environmental conditions influencing ecological dynamics and determining the nature of the taphonomic bias is the more likely explanation. Environmental variation has a biotic response that can be read in wet and dry alternation as the dominance of one set of species over others: insects-Lepidotes-Pycnodontiform fish in wet periods and crustaceans-small basal teleosteans in dry periods. In addition, dry periods are related to periphyton dominance that affects the quality and abundance of preservation. Therefore, a sedimentological, taphonomic and palaeoecological coupling might be concluded at Las Hoyas.
5.3. Sequence dynamics
The succession of communities developed during an elemental sedimentary sequence (e.g. a cycle of environmental variation from wet to dry conditions in the order of 103 years of duration, see section 5.1) has been considered as a unit, and the sequences have been comparedamong them. Three complete sequences have been defined (Fig. 4), all of which show a strong commonality in their behaviour and faunal composition. Every elemental sequence records the average features of the dominant facies association.
The first sequence is poorly characterized and incomplete. Its association is characterised by wet periods with undetermined insects and, in addition, its dry periods are far less abundant in fossil content than the equivalent dry periods of other sequences. The second and third sequences do not have different fossil assemblages, and both are dominated by the abundance and frequency of "leptolepid-like-fish" and "belostomatid insects" (Fig. 10).
The succession of elemental sequences, herein considered, do not show any superimposed trend, neither sedimentary, nor taphonomic. In other words, taphonomic structure seems to be rather monotonous or homogeneous and taphonomic gradients are repeated cyclically. Accepting the idea of a coupling between taphonomy and palaeoecology means that ecological trends on the chosen scale of analysis are also monotonous or homogeneous. The palaeoecological dynamics that arise or that can be inferred indicate an extremely stable ecological system.
[FIGURE 8 OMITTED]
There is a second hypothesis that might explain our findings, which depends on the accuracy of temporal resolution of the sedimentary record. If the resolution is assumed to be extremely near to biological timing, palaeoecological dynamics and events might be recorded with such temporal fidelity that either no significant macroecological trends occurred during formation of the whole site, or the stratigraphic interval and its corresponding temporal span analyzed are not long enough to document such trends. Beyond the actual evidence, the nature of the stratigraphic record itself makes this hypothesis unreliable or extremely unlikely. The first hypothesis suggests that the evolution of these ecosystems has the ability to integrate fluctuating environmental episodes in which no successions of communities are detected. The hypothesis also supports the idea of a fairly stable (or it should be said "consistently unstable") ecological system. Those stable ecosystems might be the result of stressed environmental conditions, whereby the stress itself prevents the ecological climax being reached, or sustained development and evolution over time towards a new ecosystem. Palaeobiological evidence is needed to account for these stressed-stable ecosystems, wherein dramatic variations in water budget and insolation from the rainy to dry seasons cause hydrological stress, anoxia in ponds and small lakes, as well as changes in nutrient availability, biomass and diversity. In these ecosystems it would take thousands of years to reach the ecological climax.
[FIGURE 9 OMITTED]
[FIGURE 10 OMITTED]
The estimate of the possible time span represented by the sequences studied herein (each of the order of 103 years), suggests that stability of the ecological dynamic might have been of an order of magnitude of thousands to tens of thousands of years. Whether the system was stable for the whole time span represented needs to be checked. However, not yet fully analysed data from the quarry (same facies and fossil association throughout the site) supports and predicts the long-term (tens of thousands years) stability hypothesis concerning functional relationships, whereas cases of specific taxonomic replacement are expected.
The model described above is the result of placing data from the Las Hoyas Konservat-Lagerstatte in spatial and temporal framework. This"dynamic" approach helps to reveal that the ecological reconstruction of Las Hoyas based on a "static" approach masks biases and reflect false biases. The frozen picture (that amalgamates dry and wet association) is a good representation of the palaeoecology of dry periods corresponding to the maximum abundance that should explain why some taxa are neither dominant nor ever retrieved. For instance, the scarcity and rareness of medium to large fish species might be thought to be a taphonomic bias (differential potential of preservation) linked to size. Thus, it should be expected that other large sized species were had not been preserved as well.
The dynamic approach shows that the two collections of fossil associations that are significantly coupled with facies yields two very different pictures of abundance and richness. This could imply that there were two different ecosystems or, indicate effects of a differing taphonomic bias on the same original faunal and floral structure. Accepting the idea of a link between taphonomy, ecological composition and sedimentology (differences in the taphonomic associations and ecological composition are closely related to environmental conditions), the best supported hypothesis would be the existence of two alternating ecosystems. The ecological trends on the chosen scale of sequence analysis are also monotonous or homogeneous, as the three complete sequences delimited all show a strong commonality of behaviour and faunal composition.
Therefore, effort is required to develop methods and concepts for extracting dynamic information from the fossil record, avoiding static reconstruction wherever possible.
6. The palaeoecological meaning of Konservat-Lagerstatten
The study reported here has also raised some implications and new questions concerning the real meaning of Las Hoyas and other Konservat-Lagerstatten and the assumptions underpinning the concept of Konservat-Lagerstatten.
Our analysis clearly shows that this type of fossil occurrence cannot be considered as result of dramatic, unusual, sedimentary processes. The mechanisms that generated Las Hoyas are anything but dramatic events on a geological scale. Sediments and their stratigraphic arrangement are easily explained by a stratigraphic framework dominated by background sedimentation. Bacterial mats, and subordinately anoxia and rapid burial, mainly due to the fast growth of mats, account for almost all of the processes involved in the genesis of the site following the classification of Seilacher et al. (1985). Since those processes may occur over a broad spectrum of depositional environments developed at any geological time, and within sedimentary basins constrained by different climate and tectonics conditions, the model is not very specific as a predictive tool. Thus, the classification provides a collection of cases that, despite being similar in the model, are independent and lacking a common pattern of causation.
Many attempts at classifying Konservat-Lagerstatten (Briggs and Crowther, 1990) with respect to various criteria such as type of sedimentary basin, depositional system and geological age, among others, have failed to capture the actual spectrum of known lagerstatten and to give the original concept a concrete and universal meaning from a genetic, palaeoecological and palaeobiological point of view. This can be easily understood if we accept that apart from taphonomic genetic processes included in Seilacher's classification and the unusual amount of palaeobiological information (anatomical details, evolutionary novelties and unusual taxa) they might not share any palaeoecological commonality.
Following this line of reasoning we need to reconsider whether all those "windows" onto the fossil record are equally sized or equivalent, i.e., whether palaeoecological information, or information about taphonomic trends and other types of palaeontological information are maximized to the same extent in Konservat-Lagerstatten as the information about body fossils seems to be.
To address this issue requires every case to be reviewed in greater depth. For example, whereas Las Hoyas seems to be a clear example placed at the end of a spectrum due to its palaeontological, stratigraphic and environmental features, others can be placed within a wide scope. For instance, in Solnhofen the information about dynamic and functional palaeoecology is troublesome. Likewise, obrution Konservat-Lagerstatten linked to geological catastrophic events, such as Pompey, are severely biased by randomness. In fact, these are effectively frozen pictures of determinate ecosystems since they reflect maximum composition fidelity, and, in the case of Pompey, even great spatial fidelity (i.e., demic and autochthonous humans). In these deposits, which were produced by a "series of catastrophic events" that yielded accumulations with mass mortality (Shipman, 1975), a fine-scale census of the original biological community might be studied. In this particular case, they can be considered to be a unique taphonomic unit. Knowing the genesis of the deposit and the catastrophe the biases are under control and we would be equally justified in interpreting the taphonomic association with a static as with a dynamic approach.
Considered from this point of view, many Konservat-Lagerstatten might be closer to palaeontological occurrences that are not classified as Konservat-Lagerstatten as exceptional "windows" on the fossil record. Conversely, some fossil associations preserved in taphonomic environments, which result in worse preservational quality, contain better quality palaeoecological information than some Konservat-Lagerstatten. This is the case for some microfossil assemblages of La Huerguina Limestone Formation located close to Las Hoyas, whose paleoecology is similar to that revealed by the Las Hoyas analysis (Buscalioni et al, 2008). In this sense, it would be worth comparing Las Hoyas to other fossil localities with respect to their palaeogeography and age, in an attempt to determine whether they share taphonomic and palaeobiological commonalities that can contribute to our understanding of the potential megabias during the Lower Cretaceous and to contrast the dynamic hypothesis of long-term ecological stability.
7. Conclusions and prospects
-Las Hoyas is a Konservat-Lagerstatten in the sense of the concept defined by Seilacher et al. (1985). Further, it can be considered a "paleoecological Lagerstatten" that holds information that, if read in its spatial and temporal framework, and by integrating stratigraphic with palaeontological information, reveals a dynamic and evolutionary ecological picture of the original ecosystem that is not available from traditional palaeocological analysis.
-Taphonomic structure of Las Hoyas Konservat-Lagerstatte is ecologically induced. The biotic response to environmental cycles induced a coupling between taphonomic and sedimentary processes that resulted in the characteristic cyclical arrangement of the stratigraphic and palaeontological record of Las Hoyas. Therefore Las Hoyas shows a significant facies bias that allows us to build a predictive model with which any newly recovered sample might be tested.
-The results of the dual approach used to reconstruct Las Hoyas ecosystem are not contradictory. Nonetheless, while the traditional approach leads to something of a dead end by providing a frozen picture of the ecosystem, the second approach moves frontiers forward, and generates new hypotheses about ecological dynamics.
-Las Hoyas was a subtropical seasonal wetland that is heavily influenced by ecological stress that impeded short-term ecological evolution and resulted in a stable ecosystem that lasted for thousands of years. The organization of the ecosystem follows a similar pattern to that of extant lentic ecosystems. It is characterized by the dominance of obligate aquatic and amphibious organisms and by the scarcity of facultative terrestrial organisms. There are multiple lines of evidence from flora and fauna of ecological strategies linked to strong seasonality and water stress. Despite the presence of shallow lakes, ecological lacustrine structures cannot be clearly recognized and Las Hoyas shows a strong bias towards wetland ecological conditions.
-The dynamic approach for the analysis of other similar preserved biotas is encouraged in order to improve the knowledge on the paleoecological meaning of Konservat-Lagerstatten.
Data. Raw data were obtained by sampling the fossil association layer-by-layer (Table 1). Each sampling area is denoted by a colour: pink 1996 (Rosa 96), pink 1998 (Rosa 98), lower black (Negra I, inferior), upper black (Negra S, superior), and lowermost black (Negra S/C). The layer itself is herein named in Spanish as capa and numbered (0 or 0.1, 0.2, 1, 2, etc.). Since the objective is to test the taphonomic association for each facies type, the layers have been grouped accordingly. For instance, NegraIcapa02 to NegraScapa from layers 5 to 9 correspond with dry facies. The table below summarizes the total number of fossils found according the above variables and the groups formed by the layers, by facies types (dry or wet).
Number of Facies fossils in Groups of layers- types association NegraIcapa02NegraScapa5-9 Dry 110 NegraIcapa2-NegraIcapa9 Wet 10 NegraIcapa10-NegraIcapa15 Dry 112 NegraScapa1-NegraScapa4 Wet 3 NegraScapa5-NegraScapa9 Dry 51 NegraScapa10NegraScapa14 Wet 4 NegraS/Ccapa1-NegraS/Ccapa5 Wet 3 NegraS/Ccapa6-NegraS/Ccapa10 Dry 193 NegraS/Ccapa11 Wet 2 Rosa98capa01Rosa98capa5 Wet 10 Rosa98capa6Rosa98capa15 Dry 48 Rosa98capa16Rosa98capa17 Wet 35 Rosa96capa 1.1 Wet 9 Rosa96capa2Rosa96capa6 Dry 373
This work is a contribution to the research project CGL-2009-11838/BTE funded by the Spanish Ministry of Science and Innovation. Excavations at Las Hoyas are funded every year by the local government of the Junta de Comunidades de Castilla-La Mancha. We thank Fernando Escaso, curator of Las Hoyas collection, Gilberto Herrero for his skilful production of hundreds of thin sections of laminated limestones from Las Hoyas, and the many students who have participated in the fieldwork, suffering the stress of taphonomic sampling. We are grateful to all the specialists who have contributed to a better understanding of Las Hoyas diversity and whose dedication has been crucial to our synthesis. We are pleased to acknowledge Dr. Francisco Jose Poyato Ariza and Dr. Patrick Orr, who carefully reviewed and notably improved the original version of this manuscript. We are also delighted to acknowledge the Chinese and Japanese restaurants where, since 2003, the authors consumed tons of sushi, noodles and the waiters' patience while discussing the best way of understanding the palaeocology of Las Hoyas. Once again, Phil Mason has improved the English language of our original manuscript.
Allison, P. A., Briggs, D. E. G. (eds.) (1991): Taphonomy, releasing the data locked in the fossil record. Plenum Press, New York. Pp: 546.
Barral-Cuesta, A., Gomez, B. (2009): Dicot-like angiosperm leaves from the Upper Barremian of Las Hoyas (Serrania de Cuenca, Spain): morphological description and morphometrical approach. In: A. D. Buscalioni, M. Fregenal-Martinez. (eds.). Mesozoic Terrestrial Ecosystems and Biota. 10th International Meeting. Ediciones UAM, Madrid: p. 125.
Batzer, D. P., Cooper, R., Wissinger, S. A. (2006): Wetland animal ecology. In: D. P. Batzer, R. Sharitz (eds.), Ecology of Freshwater and Estuarine wetlands. University of California Press, Berkeley, Los Angeles, London: 242- 284.
Behrensmeyer, A. K., Kidwell, S. M., Gastaldo, R. A. (2000): Taphonomy and paleobiology. In: D. H. Erwin, S.L. Wing., (eds.) Deep in time.Paleobiology's perspective. The paleontological society, Supplement to volume 26 (4), USA: 103-147. http:// dx.doi.org/10.1666/0094-8373(2000)26[103:TAP]2.0.CO;2
Briggs, D. E. G. (1995): Experimental taphonomy. Palaios, 10: 539-550. http://dx.doi.org/10.2307/3515093
Briggs, D. E. G., Crowther, P. R. (1990): Taphonomy. In: D. E. G. Briggs, P. R. Crowther, (eds.) Palaeobiology. A synthesis. Blackwell Scient. Publ., Oxford: 211-303.
Briggs, D. E. G., Wilby, R., Perez-Moreno, B. P., Sanz, J. L., Fregenal Martinez, M. (1997): The mineralization of dinosaur soft tissue in
the Lower Cretaeous of Las Hoyas, Spain. Journal of the Geological Society, London, 154: 587-588. http://dx.doi. org/10.1144/gsjgs.154.4.0587
Buatois, L. A., Mangano, M. G., Fregenal-Martinez, M. A., De Gibert, J. M. (2000): Short-term colonization trace-fossil assemblages in a carbonate lacustrine konservat-lagerstatte (Las Hoyas fossil site, Lower Cretaceous, Cuenca, central Spain). Facies, 43: 145-156. http://dx.doi.org/10.1007/BF02536988
Burns, A., Walker, K. F. (2000): Biofilms as food for decapods (Atyidae, Palaemonidae) in the River Murray, Souyh Australia. Hydrobiologia, 437: 83-90.
Buscalioni, A. D., Ortega, F., Perez-Moreno, B. P., Evans, S. E. (1996): The Upper Jurassic Maniraptoran Theropod Lisboasaurus estesi (Guimarota, portugal) reinterpreted as a crocodylomorph. Journal of Vertebrate Paleontology, 16: 358-362. http://dx.doi.org/10.1080/02724634.1996.10011322
Buscalioni, A. D., Fregenal-Martinez, M. A. (2003): A dynamic reading of the palaeoecology of the early cretaceous continental ecosystem of Las Hoyas based on stratigraphic and taphonomic patterns. Abstracts European Palaeontological Association Workshop 2003: Exceptional Preservation, Teruel, Spain: 15-16.
Buscalioni, A. D. Fregenal-Martinez, M. A., Bravo, A., Poyato Ariza, F. J., Sanchiz, B., Baez, A. M., Cambra Moo, O., Martin-Closas, C., Evans, S. E., Marugan-Lobon, J. (2008): The vertebrate assemblage of Buenache de la Sierra (Upper Barremian of Serrania de Cuenca, Spain) with insights into its taphonomy and paleoecology. Cretaceous Research, 29: 687-710. http://dx.doi. org/10.1016/j.cretres.2008.02.004
Cambra-Moo, O., Buscalioni, A. D. (2003): Biostratinomic patterns in archosaur fossils: influence of morphological organization on dispersal. Journal of Taphonomy, 1: 247-268.
Clarke, K. R., Warwick, R. M. (2001). Change in marine communities; an approach to statistical analysis and interpretation. 2nd Edition. PRIMIER-E:Plymouth
Cohen, A. S., (2003): Paleolimnology: The History and Evolution of Lake Systems. Oxford University Press, Oxford: 500 p.
Daviero-Gomez, V., Gomez, B., Martin-Closas, C., Philippe, M. (2006):--Montsechia vidalii (Zeiller) Teixeira, in search of a systematic affinity. Resume de la reunion conjointe de la Linnean Society et de l'Organisation Francophone de Paleobotanique, Montpellier, France: 8.
Evans, S. E., Milner, A. R. (1996): A metamorphosed salamander from the early Cretaceous of Las Hoyas, Spain. Phylosophical Transations Royal Society of London, 351: 627-646. http:// dx.doi.org/10.1098/rstb.1996.0061
Evans, S. E., Barbadillo, L. J. (1998): An unusaul lizard (Reptilia: Squamata) from the Early Cretaceous of Las Hoyas, Spain. Zoological Journal Linnean Society, 124: 235-265.
Fernandez-Lopez, S. (1989): La materia fosil. Una concepcion dinamicista de los fosiles. En: E. Aguirre (ed.). Nuevas Tendencia en Paleontologia. Consejo Superior de Investigaciones Cientificas, Madrid, 10: 25-45.
Fernandez-Lopez, S. (1991): Taphonomic concepts for a theoretical Biochronology, Revista Espanola de Paleontologia, 6: 37-49.
Fregenal-Martinez, M. A. (1998): Analisis de la cubeta sedimentaria de Las Hoyas y su entorno paleogeografico (Cretacico Inferior, Serrania de Cuenca). Sedimentologia y aspectos tafonomicos del yacimiento de Las Hoyas. Tesis Doctoral Universidad Complutense de Madrid: 354 p.
Fregenal-Martinez, M. A., Melendez, N. (1993): Sedimentologia y evolucion paleogeografica de la cubeta de Las Hoyas, Cuadernos de Geologia Iberica, 17: 231-256.
Fregenal-Martinez, M. A., Melendez, N. (2000): The lacustrine fossiliferous deposits of the Las Hoyas sub-basin (Lower Cretaceous, Serrania de Cuenca, Iberian Ranges, Spain). In: E. H. Gierlowski-Kordesch, K. Kelts (eds.), Lake basins through space and time. AAPG Studies in Geology, 46: 303-314.
Fregenal-Martinez, M., Delclos, X., Soriano, C. (2007): The Barremian continental wetlands and lakes of the Serrania de Cuenca Basin, and their entomobiotas. In: X. Delclos, C. Soriano (eds.), Mesozoic and Cenozoic Spanish insect localities. International Palaeoentomological Association and Diputacion Foral de Alava: 48-64.
Fregenal-Martinez, M. A., Buscalioni, A. D. (2009): Las Hoyas Konservat-lagesrttatte: a fieltrip to a Barremian subtropical continental wetland ecosystem. In: L. Alcala, R. Royo-Torres (eds.), Mesozoic Terrestrial Ecosystems in Eastern Spain. Fundamental, 14, Fundacion Conjunto Paleontologico de Teruel. Dinopolis: 131-147.
Garassino, A. (1996): The macruran decapod crustaceans of the Lower Cretaceous (lower Barremian) of Las Hoyas (Cuenca, Spain). Atti. Societa Italiana Science Naturale Museo Civico di Storia Naturale di Milano, 137: 101-126.
Gierlowski-Kordesch, E. H., Gomez-Fernandez, J. C., Melendez, N. (1991): Carbonate and coal deposition in an alluvial lacustrine setting: Lower Cretaceous (Weald) in the Iberian Range (East-Central Spain). In: P., Anadon, LL. Cabrera, K. Kelts (eds.), Lacustrine Facies Analysis, International Association of Sedimentologists Special Publication, 13: 111-127.
Gomez-Fernandez, J. C., Melendez-Hevia, N. (1991): Rhythmically laminated lacustrine deposits in the lower Cretaceous of la Serrania de Cuenca basin (Iberian Ranges, Spain). In: P., Anadon, LL. Cabrera, K. Kelts (eds.), Lacustrine Facies Analysis, International Association of Sedimentologists Special Publication, 13: 247-258.
Gomez, B., Martin-Closas, C., Barale, G, Sole de Porta, N., Thevenard, F., Guignard, G. (2003): Frenelopsis (Coniferales: Cheirolepidiaceae) and related male organ genera from the Lower Cretaceous of Spain. Palaeontology, 45: 997-1036.
Good, S.C. (2004): Paleoenvironmental and paleoclimatic significance of freshwater bivalves in the Upper Jurassic Morrison Formation. Sedimentary Geology, 167: 163-177. http://dx.doi. org/10.1016/j.sedgeo.2004.01.005
Gupta, N. S., Cambra-Moo, O., Briggs, D. E.K., Love, G. D., Fregenal-Martinez, M. A., Summons, R. E. (2008): Molecular taphonomy of macrofossils from the Cretaceous Las Hoyas Formation, Spain. Cretaceous Research, 29: 1-8. http://dx.doi. org/10.1016/j.cretres.2006.12.009
Haywood, A. M., Valdes, P. J., Markwick, P. J. (2004): Cretaceous (Wealden) climates: a modelling perspective. Cretaceous Research, 25: 303-311. http://dx.doi.org/10.1016/j.cretres.2004.01.005
Hammer, O., Harper, D. (2008): Paleontological data analysis. Blackwell Publishing, Oxford: 351.
Holland, S. M. (1997): Using time/environment analysis to recognize faunal events in the Upper Ordovician of the Cincinati Arch. In: C. E. Bret, G. C. Baird, (eds.), Paleontological event: stratigraphic, ecological and evolutionary implications. Columbia University Press, New York: 309-334.
Holland, S. M. (2000): The quality of the fossil record: a sequence stratigrphic perspective. In: D. H. Erwin, S. L. Wing. (eds.), Deep in time. Paleobiology's perspective. The paleontological society, Supplement to volume 26, USA: 148-168.
Iniesto, M., Lopez-Archilla A. I., Buscalioni, A. D., Penalver, E., Fregenal-Martinez, M. A., Guerrero, M. C.(2009): Experimental simulation of initial stages of fossilization by bacterial sealing: implications for the formation of Las Hoyas Konservat-Lagerstatte (Lower Cretaceous, Iberian Ranges, Spain). In: A. D. Buscalioni, M. A. Fregenal-Martinez, (eds.), Mesozoic Terrestrial Ecosystems and Biota. Abstracts 10th International Meeting. UAM Ediciones, Madrid: p. 273.
Jaume, D. (2008): Global diversity of spelaeogriphaceans and thersbaenaceans (Crustacea; Spelaeogriphacea & Thermobaenacea) in freshwater. Developments in Hydrobiology, 198: 219224. http://dx.doi.org/10.1007/s10750-007-9017-1
Kidwell, S. M. (1991): The stratigraphy of shell concentrations. In: P. A. Allison, D. E. G. Briggs, (eds.), Taphonomy, releasing the data locked in the fossil record. Plenum Press, New York: 211-290.
Kidwell, S. M. (1993): Taphonomic expressions of sedimentary hiatus: field observations on bioclastic concentrations and sequence anatomy in low, moderate and high subsidence settings. Geologische Rundschau, 82: 189-202. http://dx.doi. org/10.1007/BF00191825
Martin-Closas, C. (2005): El paisaje vegetal del Cretacico inferior de la Cordillera Iberica. En: G. Melendez, M. Morero-Azanza (eds.), La vida y los ambientes sedimentarios en el Periodo Cretacico. Publicaciones del Seminario de Paleontologia de Zaragoza, 7: 49-61.
Martin-Closas, C., Dieguez, C. (1998): Charophytes from the Lower Cretaceous of the Iberian ranges, Spain. Palaeontology, 41: 1133-1152.
Martin-Closas, C., Gomez, B. (2004): Taphonomie des plantes et interpretations paleoecologiques. Une synthese. Geobios, 37: 65-88.
Martin-Closas, C., Martinez-Delclos, X., Buscalioni, A. D., De La Fuente, M., Fregenal-Martinez, M. A., Gomez, B., PoyatoAriza, F. J., Soriano, C. (2003): Preservation bias in the Aquatic Ecosystem of "Las Hoyas" (Late Barremian, Spain). In: L. Alcala (ed.), Abstracts European Palaeontological Association Workshop 2003: Exceptional Preservation, Teruel, Spain: 67-68.
Martinez-Delclos, X. (1991): Insects from the lithographical limestones of the Serra del Montsec. Lower Cretaceous of Catalonia, Spain. In: X. Martinez-Delclos (ed.), The Lower Cretaceous Lithographic limestones of Montsec (Catalonia, Spain): 10years of Paleontological Expeditions, Institut d'Estudis Ilerdencs, Lleida: 61-71.
Martinez-Delclos, X. (1993): Blatidos (Insecta Blattodea) del Cretacico inferior de Espana. Familias Mesoblattinidae, Blattulidae y Poliphagidae. Boletin Geologico y Minero de Espana, 104: 516-538.
Martinez-Delclos, X., Nel, A., Popov, Y. A. (1995): Systematic and functional morphology of Iberonepa romerali n. Gen. N. Sp. Belostomatidae, Stygeonepidae from the Spanish Lower Cretaceous (Insecta, Heteroptera, Neopomorpha). Journal of Paleontology, 69: 469-508.
Martinez-Delclos, X., Briggs, D. E. G., Penalver, E. (2004): Taphonomy of insects in carbonates and amber. Palaeogeography, Palaeoclimatology, Palaeoecology, 203: 19-64.
Mas, J. R., Alonso, A., Melendez, N. (1982): El Cretacico basal "Weald" de la Cordillera Iberica Suroccidental (NW de la provincia de Valencia y E de la de Cuenca). Cuadernos de Geologia Iberica, 8: 309-335.
McGowan, G., Evans, S.E. (1995): Albanerpetontid amphibians from the Cretaceous of Spain. Nature, 373: 143-145. http:// dx.doi.org/10.1038/373143a0
Mendelssohn, I. A., Batzer, D. P. (2006): Abiotic constraints for wetland plants and animals. In: D. P. Bazter, R. Sharitz (eds.), Ecology of Freshwater and Estuarine wetlands. University of California Press, Berkeley, Los Angeles, London: 82-114.
Ortega, F. (2004): Historia Evolutiva de los cocodrilos Mesoeucrocodylia. Tesis Doctoral, Universidad Autonoma de Madrid. Facultad de Ciencias: 350 pp.
Ortega, F., Sanz, J. L., Barbadillo, J. L., Buscalioni, A. D., Dieguez, C., Evans, S. E., Fregenal-Martinez, M. A., De la Fuente, M., Madero, J., Martin-Closas, C., Martinez-Delclos, X., Melendez, N., Moratalla, J. J., Perez-Moreno, B. P., Pinardo-Moya, E., Poyato-Ariza, F. J., Rodriguez-Lazaro, J., Sanchiz, B., Wenz, S. (1999): El yacimiento de Las Hoyas (La Cierva, Cuenca): Un Konservat-Lagerstatte del Cretacico inferior. Patrimonio Historico Arqueologia Castilla-La Mancha. In: E. Aguirre, I. Rabano (coord.) La Huella del pasado. Fosiles de Castilla-La Mancha, Comunidad de Castilla- La Mancha: 195-216.
Ortega, F., Buscalioni, A. D., Delclos, X., Fregenal-Martinez, M. A., Martin-Closas, C., Poyato-Ariza, F. J., Sanz, J. L., Soriano, C. (2003): Los fosiles del Cretacico de Las Hoyas: un yacimiento excepcional. In: R. Nuche del Rivero (ed.), Patrimonio Geologico de Castilla- La Mancha. Enresa, Madrid: 422-448.
Palci, A., Jurkovsek, B., Kolar-Jurkovsek, T., Cadwell, M. W. (2008): New palaeoenvironmental model for the Komen (Slovenia) Cenomanian (Upper Cretaceous) fossil lagerstatte. Cretaceous Research, 29: 316-328. http://dx.doi.org/10.1016/). cretres.2007.05.003
Perez-Moreno, B. P., Sanz, J. L., Buscalioni, A. D., Moratalla, J. J., Ortega, F., Rasskin-Gutman, D. (1994): A unique multi-toothed ornithomimosaur from the Lower Cretaceous of Spain. Nature, 30: 363-367. http://dx.doi.org/10.1038/370363a0
Ponomarenko, A., Martinez-Delclos, X. (2000): New beetles (Insecta: Coleoptera) from the Lower Cretaceous of Spain. Acta Geologica Hispanica, 35: 47-52.
Poyato-Ariza, F. J. (1997): A new assemblage of Spanish Early Cretaceous teleostean fishes, formerly considered "leptolepids": phylogenetic relevance. Comptes Rendus de l'Academie des Sciences--Series IIA - Earth and Planetary Science, 325: 373-379.
Poyato-Ariza, F. J. (2003): Dental characters and phylogeny of pycnodontiform fishes. Journal of Vertebrate Paleontology, 23: 937940. http://dx.doi.org/10.1671/17
Poyato-Ariza, F. J. (2005): Palaeoecology of the fishes from the Early Cretaceous lake of Las Hoyas, Cuenca, Spain, with a hypothesis of sexual dimorphism for the chanidae Rubiesichthys. Bulletin of the Kitakyushu Museum of Natural History and Human History series A, Natural History), 3: 153-168.
Poyato-Ariza, F. J., Wenz, S. (2004): The new pycnodontid fish genus Turbomesodon, and a revision of Macromesodon based on Lower Cretaceous new material from Las Hoyas, Cuenca, Spain. In: G. Arratia, A. Tintori (eds.), Mesozoic Fishes 3: Systematics, Palaeoenvironment and Biodiversity. Munchen Verlag Dr. Pfeil: 341-378.
Poyato-Ariza, F. J., Talbot, M. R., Fregenal-Martinez, M. A., Melendez, N., Wenz, S. (1998): First isotopic and multidisciplinary evidence for nonmarine coelacanths and pycnodontiform fishes: palaeoenvironmental implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 144: 64-84.
Rabada i Vives, D. (1991): Crustaceos Decapodos de las Calizas Litograficas del Cretacico Inferior de Espana: las Hoyas (Cuenca) y el Montsec de Rubies (Lleida), Universitat de Barcelona: Barcelona. 184 p.
Rabada, D. (1993): Crustaceos decapodos lacustres de las calizas litograficas del Cretacico Inferior de Espana. Cuadernos de Geologia Iberica, 17: 345-370.
Salas, R., Casas, A. (1993): Mesozoic extensional tectonics, stratigraphy and crustal evolution during the Alpine cycle of the eastern Iberian basin. Tectonophysics, 228: 33-55. http://dx.doi. org/10.1016/0040-1951(93)90213-4
Sanz, J. L., Chiappe, L. M., Perez-Moreno, B. P., Buscalioni, A. D., Moratalla, J. J., Ortega, F., Poyato-Ariza, F. J. (1996): An Early Cretaceous bird from Spain and its implications for the evolution of avian flight. Nature, 382: 442-445. http://dx.doi. org/10.1038/382442a0
Sanz, J. L., Dieguez, C., Poyato-Ariza, F. J. (2000): Die UnterKreide von Las Hoyas, Cuenca, Spanien. In: G. Pinna (coord.) Europaische Fossillagerstatten. Springer-Verlag Berling Heidelberg: 155-160.
Sanz, J. L., Fregenal-Martinez, M. A., Melendez, N., Ortega, F. (2001) : Las Hoyas. In: D. E. G. Briggs, P. R. Crowther (eds.) Palaeobiology II. Blackwell Science, Oxford: 356-359.
Sanz, J. L., Perez-Moreno, B. P., Chiappe, L. M., Buscalioni, A. D. (2002) : The birds from the Lower Cretaceous of Las Hoyas (Province of Cuenca, Spain). In: L. M. Chiappe, L. M. Witmer (eds.) Mesozoic Birds. University of California Press: 209-229.
Seilacher, A. (1990): Taphonomy of Fossil-Lagerstatten: an overview. In: D. E. G. Briggs, P. Crowther (eds.), Paleobiology. Blackwell Science, Oxford: 266-270.
Seilacher, A., Reif, W. E., Westphal, F. (1985): Sedimentological, ecological and temporal patterns of fossil lagerstatten. Phylosophical Transactions of the Royal Soc. London B, 311: 5-23. http://dx.doi.org/10.1098/rstb.1985.0134
Selden, P., Penney, D. (2003): Lower Cretaceous spiders (Arthropoda: Arachnida: Araneae) from Spain. Neues Jahrbuch fur Geologie und Palaontologie, Abhandlungen, 2003: 175-192.
Shipman, P. (1975): Implications of drought for vertebrate fossil assemblages. Nature, 257: 667-668. http://dx.doi. org/10.1038/257667a0
Soria, A. R., Melendez, A., Aurell, M., Liesa, C. L., Melendez, M. N., Gomez-Fernandez, J. C. (2000): The Early Cretaceous of the Iberian Basin (Northeastern Spain). In: In: E. H. Gierlowski-Kordesch, K. Kelts (eds.), Lake basins through space and time. AAPG Studies in Geology, 46: 257-262.
Soriano, C. (2006): Paleobiologia de los coleopteros del Cretacico inferior espanol. Tesis Doctoral. Universitat de Barcelona. 345 pp.
Soriano, C., Delclos, X. (2006): New cupedid beetles from the Lower Cretaceous of Spain and the palaeogeography of the family. Acta Paleontologica Polonica, 51: 185-200.
Soriano, C., Kirejtshuk, A. G., Delclos, X. (2006): The Mesozoic Laurasian family Parandrexidae (Insecta: Coleoptera), new species from the Lower Cretaceous of Spain. Comptes Rendus Palevol, 5: 779-784. http://dx.doi.org/10.1016/j.crpv.2006.03.006
Soriano, C., Ponomarenko, A., Delclos, X. (2007): Coptoclavid beetles (Coleoptera: Adephaga) from the Lower Cretaceous of Spain: A new feeding strategy in beetles. Palaeontology, 50: 1-12. http://dx.doi.org/10.1111/j.1475-4983.2007.00642.x
Stinnesbeck, W., Ifrim, C., Schmidt, H., Rindfleisch, A., Buchy, M-C., Frey, E., Gonzalez-Gonzalez, A-H., Vega, F. J., Cavin, L., Keller, G., Smith, K. T. (2005): A new lithographic deposit in the Upper Cretaceous Austin Group at El Rosario, county of Muzquiz, Coahuila, northeaster Mexico. Revista Mexicana de Ciencias Geologicas, 22: 401-418.
Talbot, M. R., Melendez, N., Fregenal-Martinez, M. A. (1995): The waters of the Las Hoyas lake: Sources and limnological characteristics. In: N. Melendez (ed.), Las Hoyas. A lacustrine Konservat-Lagerstatte, Cuenca, Spain. Universidad Complutense, Madrid: 11-16.
Van der Valks, A.G. (2006): The Biology of freshwater wetlands. Oxford University Press: 173 p.
Vilas, L., Mas, R., Garcia, A., Arias, C., Alonso, A., Melendez, N., Rincon, R. with the collaboration of Elizaga, E., Fernandez-Calvo, C., Gutierrez, C., Melendez, F. (1982): Iberica Suroccidental. In: El Cretacico de Espana. Editorial de la Universidad Complutense de Madrid: 457-513.
Vilas, L., Alonso, A., Arias, C., Mas, R. Rincon, R., Melendez, N. (1983): The Cretaceous of the Southwestern Iberian Ranges (Spain). Zitteliana, 10: 245 254.
Vullo, R., Buscalioni, A. D., Marugan-Lobon, J., Moratalla, J. J. (2009): Pterosaur remains from the Early Cretaceous Lagerstatte of Las Hoyas, Spain: palaeoecological significance. Geological Magazine, 146: 931-936. http://dx.doi.org/10.1017/ S0016756809990525
Wenz, S.,Poyato-Ariza, F.(1994): Les Actinopterygiens juveniles du Cretace inferieur du Montsec et de Las Hoyas (Espagne). Geobios Memoire special, 16: 203-212. http://dx.doi.org/10.1016/ S0016-6995(94)80035-9
Zherikhin, V. V., Gratshev, V. G. (2003): A New Weevil-Beetle (Insecta, Coleoptera, Nemonychidae) from the Lower Cretaceous of Spain. Paleontological Journal, 37: 407-408.
Ziegler, A. M., Barret, S. F., Scotese, C. R. (1983): Mesozoic and Cenozoic paleogeographic maps. In: P. Brosche, J. Sundermann (eds.), Tidal Friction and the Earth's Rotation, II. Springer-Verlag, Berlin: 240-252.
Ziegler, A. M., Raymond, A. L., Gierlowski, T. C., Horrell, M. A., Rowley, D. B., Lottes, A. L. (1987): Coal, climate and terrestrial productivity: the present and Early Cretaceous compared. In: A. C. Scott (ed.), Coal and Coal-bearing Strata: Recent Advances. Geological Society of London Special Publications, 32: 25-49. http://dx.doi.org/10.1144/GSL.SP.1987.032.01.04
A.D. Buscalioni (1), M.A. Fregenal-Martinez (2)
(1) Unidad de Paleontologia, Departamento de Biologia, Facultad de Ciencias, Universidad Autonoma de Madrid, c/ Darwin 2, Campus Universitario de Cantoblanco, 28049 Madrid, Spain. firstname.lastname@example.org
(2) Departamento de Estratigrafia e Instituto de Geologia Economica (UCM-CSIC) Facultad de Ciencias Geologicas, Universidad Complutense de Madrid, c/ Jose Antonio Novais 2, 28040 Madrid, Spain. email@example.com Authors in alphabetical order
Received: 08/12/09 / Accepted: 30/06/10
Table 1. Raw data. SL. Sampling labels. F. Facies type: W (wet), D (dry). Q=sequence; NAS=total number of fossil sampled in the layer; I=ichnofossils; C=coprolites; W="worms"; O=ostracods; NF= total number of fish; NC=total number of crustraceans; NI=total number of insects; NB= total number of bivalves; crustaceans: Delclosia shrimps (A); peracarids-espeleogriphaceans (B); austrapotamobius decapods (C); insects: coleopterans (D); belostomatids (E); chrisopids (F); kalligrammatids (G); ephemeropters (H); chresmodids (I). Fish: "leptole-pids" (primitive teleostean juveniles) (1); pleuropholidids (2); amiidid (3); Notagogus (4); Gordichthys (5); Lepidotes (6); pycnodontiforms (7); Rubiesichthys (8) Tabla 1. Datos brutos. SL. Etiquetas del muestreo. F. Tipo de facies W (humeda), D (arida). Q=secuencia; NAS=numero total de fosiles mues-treados en la capa; I=icnofosiles; C=coprolitos; W="gusanos"; O=ostracodos; NF=numero total de peces; NC=numero total de crustaceos; NI=numero total de insectos; NB= numero total de bivalvos; Crutaceos: gambas Delclosia (A); peracaridos-espeleogrifaceos (B); decapodo Austropotamobius (C);Insectos: coleopteros (D); belostomatidos (E); crisopidos (F); kalligramatidos (G);efemeropteros; chresmodidos (I). Peces: "leptolepidos" (teleosteos primitivos juveniles) (1); pleurofolididos (2); amiididos (3); Notagogus (4); Gordichthys (5); Lepidotes (6); pycnodontiformes (7); Rubiesichthys (8). SL F Q NAS I C W O NF NC NI NB A NgI02R D 3 59 N Y N N 5 46 9 1 45 NgI2A W 2 1 N N N N 0 0 1 0 0 NgI6A W 2 1 N N N N 0 0 1 0 0 NgI7A W 2 7 N N N N 4 0 3 0 0 NgI9A W 2 1 N N N N 0 0 1 0 0 NgI10R D 2 47 N Y N N 46 1 0 0 1 NgI11R D 2 1 N Y N N 1 0 0 0 0 NgI12R D 2 31 Y Y N N 19 8 4 0 8 NgI1314R D 2 3 N N N N 2 0 1 0 0 NgI1415R D 2 30 N Y Y N 3 6 4 0 5 NgS1A W 3 0 N Y N N 0 0 0 0 0 NgS2A W 3 1 N Y N N 1 0 0 0 0 NgS4A W 3 2 N N N N 0 0 2 0 0 NgS5R D 3 5 N Y N N 1 2 1 0 2 NgS7R D 3 3 N Y Y N 0 0 2 0 0 NgS8R D 3 2 N N N N 0 0 2 0 0 NgS9R D 3 41 N N Y N 4 2 29 1 1 NgS1012A W 2 3 N Y N N 1 0 2 0 0 NgS14A W 2 1 N N N N 0 0 1 0 0 NSC1A W 2 0 N N N N 0 0 0 0 0 NSC3A W 2 2 N N N N 2 0 0 0 0 NSC45A W 2 1 N N N N 0 0 1 0 0 NSC6R D 2 108 N N N N 101 6 1 0 6 NSC7R D 2 22 N Y Y Y 13 4 2 0 4 NSC8R D 2 12 Y N N N 3 0 0 0 0 NSC910R D 2 51 Y Y N Y 4 6 3 0 2 NSC11A W 1 2 N Y N N 2 0 0 0 0 RS0198A W 1 4 N N N N 1 0 3 0 0 RS298A W 1 2 N N N N 0 0 4 0 0 RS3 498A W 1 0 N N Y N 0 0 0 0 0 RS598A W 1 2 N Y Y N 1 0 1 0 0 RS698 * D 1 1 N Y Y N 0 1 0 0 0 RS798 * D 1 0 Y N N N 0 0 0 0 0 RS1198 * D 1 8 N Y N N 0 8 0 0 0 RS1398R D 1 8 N N N N 0 6 0 2 0 RS1498R D 1 26 N N N N 0 26 0 0 0 RS1598R D 1 5 N N N N 0 4 0 1 0 RS1698A W 1 6 N N Y N 0 0 6 0 0 RS1798A W 1 29 N Y Y N 5 5 18 0 3 RS1.196A W 2 9 N N N N 8 1 0 0 0 RS296R D 2 27 N N N N 23 4 0 0 3 RS396R D 2 36 Y Y N Y 22 13 2 0 4 RS496R D 2 29 Y Y N N 12 17 0 0 9 RS596R D 2 275 Y Y Y Y 212 59 2 2 32 RS696R D 2 6 Y Y N N 2 3 0 0 2 SL B C D E F G H I NgI02R 0 0 2 7 0 0 0 0 NgI2A 0 0 0 0 1 0 0 0 NgI6A 0 0 0 0 0 1 0 0 NgI7A 0 0 1 0 1 0 0 0 NgI9A 0 0 0 1 0 0 0 0 NgI10R 0 0 0 0 0 0 0 0 NgI11R 0 0 0 0 0 0 0 0 NgI12R 0 0 2 1 0 0 0 0 NgI1314R 0 0 0 0 0 0 0 0 NgI1415R 0 1 0 0 0 0 0 0 NgS1A 0 0 0 0 0 0 0 0 NgS2A 0 0 0 0 0 0 0 0 NgS4A 0 0 0 2 0 0 0 0 NgS5R 0 0 0 0 0 0 1 0 NgS7R 0 0 1 0 0 0 0 0 NgS8R 0 0 0 2 0 0 0 0 NgS9R 0 0 3 19 2 1 1 2 NgS1012A 0 0 1 0 0 1 0 0 NgS14A 0 0 0 1 0 0 0 0 NSC1A 0 0 0 0 0 0 0 0 NSC3A 0 0 0 0 0 0 0 0 NSC45A 0 0 0 1 0 0 0 0 NSC6R 0 0 0 0 0 0 0 0 NSC7R 0 0 2 0 0 0 0 0 NSC8R 0 0 0 0 0 0 0 0 NSC910R 0 1 1 0 0 0 0 1 NSC11A 0 0 0 0 0 0 0 0 RS0198A 0 0 0 2 1 0 0 0 RS298A 0 0 1 2 0 0 0 0 RS3 498A 0 0 0 0 0 0 0 0 RS598A 0 0 0 0 0 0 0 0 RS698 * 0 0 0 0 0 0 0 0 RS798 * 0 0 0 0 0 0 0 0 RS1198 * 1 7 0 0 0 0 0 0 RS1398R 2 3 0 0 0 0 0 0 RS1498R 21 0 0 0 0 0 0 0 RS1598R 4 0 0 0 0 0 0 0 RS1698A 0 0 0 1 0 0 0 0 RS1798A 2 0 1 6 1 0 1 0 RS1.196A 1 0 0 0 0 0 0 0 RS296R 1 0 0 0 0 0 0 0 RS396R 6 2 0 0 0 0 0 0 RS496R 5 3 0 0 0 0 0 0 RS596R 4 13 0 0 0 0 0 0 RS696R 1 0 0 0 0 0 0 0 SL 1 2 3 4 5 6 7 8 NgI02R 0 0 0 0 0 5 0 0 NgI2A 0 0 0 0 0 0 0 0 NgI6A 0 0 0 0 0 0 0 0 NgI7A 0 0 0 0 0 4 0 0 NgI9A 0 0 0 0 0 0 0 0 NgI10R 46 0 0 0 0 0 0 0 NgI11R 0 0 0 0 1 0 0 0 NgI12R 19 0 0 0 0 0 0 0 NgI1314R 2 0 0 0 0 0 0 0 NgI1415R 2 0 0 1 0 0 0 0 NgS1A 0 0 0 0 0 0 0 0 NgS2A 0 0 0 0 0 0 0 0 NgS4A 0 0 0 0 0 0 0 0 NgS5R 1 0 0 0 0 0 0 0 NgS7R 0 0 0 0 0 0 0 0 NgS8R 0 0 0 0 0 0 0 0 NgS9R 1 0 0 1 0 2 0 0 NgS1012A 0 0 0 0 0 0 0 0 NgS14A 0 0 0 0 0 0 0 0 NSC1A 0 0 0 0 0 0 0 0 NSC3A 1 0 0 0 0 1 0 0 NSC45A 0 0 0 0 0 0 0 0 NSC6R 100 0 0 0 0 0 0 1 NSC7R 13 0 0 0 0 0 0 0 NSC8R 1 0 0 2 0 0 0 0 NSC910R 4 0 0 0 0 0 0 0 NSC11A 0 0 0 0 0 1 1 0 RS0198A 0 0 0 0 0 1 0 0 RS298A 0 0 0 0 0 0 0 0 RS3 498A 0 0 0 0 0 0 0 0 RS598A 1 0 0 0 0 0 0 0 RS698 * 0 0 0 0 0 0 0 0 RS798 * 0 0 0 0 0 0 0 0 RS1198 * 0 0 0 0 0 0 0 0 RS1398R 0 0 0 0 0 0 0 0 RS1498R 0 0 0 0 0 0 0 0 RS1598R 0 0 0 0 0 0 0 0 RS1698A 0 0 0 0 0 0 0 0 RS1798A 2 0 0 0 0 1 0 0 RS1.196A 8 0 0 0 0 0 0 0 RS296R 21 0 0 0 0 0 0 0 RS396R 21 0 0 1 0 0 0 0 RS496R 12 0 0 0 0 0 0 0 RS596R 208 1 1 2 0 0 0 0 RS696R 2 0 0 0 0 0 0 0 Table 2.--1. Total number of fossils in wet and dry associations. VAR= variables; NAS=total number of fossil sampled in the layer; I=ichnofossils; C=Coprolites; W="worms; O=ostracods; * asterisk denotes number of observations, and it does not represent the total number of individuals recorded. NF= total number of fish; NC=total number of crustraceans; NI=total number of insects; NB= total number of bivalves; Crustaceans: Delclosia shrimps (A); peracarids-spelaeogriphaceans (B); Austropotamobius decapods (C); Insects: coleopterans (D); belostomatids (E); Chri-sopids (F); Kalligrammatids (G); Ephemoropterans (H); Chremodids (I). Fish: "leptolepids" (primitive teleostean juveniles) (1); pleuropholidids (2); amiidid (3); Notagogus (4); Gordichthys (5); Lepidotes (6); pycnodontiforms (7); Rubiesichthys (8). 2. Data used in the estimation of rare- faction curves. Data are represented in figure 6. FI= undetermined fish; CI= undetermined crustaceans, II= undetermined insects; BI= undetermi-ned bivalves; NASS=total number of collected fossils. 3. Richness and diversity indices for the two samples (wet and dry), with probabilities of equality p<0.05. To evaluate species richness in the two samples, note that Menhinick richness index is higher is the wet association. This index attempts at compensating for sample size (Hammer and Harper, 2008). Other indices such as Dominance, Evenness and Berger- Parker, attempt to incorporate relative abundance. Note here that the higher abundance and homogeneous composition of the dry association result in greater values of Dominance and Berger-Parker indices. Results from PAST[c] program (Hammer and Harper, 2008). Tabla 2.--Arriba: Numero toral de fosiles en las asociaciones secas y aridas. VAR= variables; NAS=numero total de fosiles muestreados en la capa; I=icnofosiles; C=coprolitos; W="gusanos"; O=ostracodos; *el asterisco senala el numero de observaciones, pero no indica el numero total de individuos registrados. NF= numero tal de peces; NC= numero total de crustaceos; NI= numero total de insectos; NB= numero total de bivalvos; Crustaceos: gamba Delclosia (A); peracaridos-espeleogrifaceos (B); decapodo Austropotamobius (C); Insectos: coleopteros (D); belostomatidos (E); Crisopidos (F); Kalligrammatidos (G); Efemeropteros (H); Cresmodidos (I). Peces: "leptolepidos" (teleosteos juveniles pri-mitivos) (1); pleurofolididos (2); amiididos (3); Notagogus (4); Gordichthys (5); Lepidotes (6); pycnodontiformes (7); Rubiesichthys (8). Abajo: Datos utilizados en la estimacion de las curvas de rarefaccion. Los datos han sido representados en la figura 6. FI= peces sin identificar; CI= crustaceos indeterminados; II=insectos indeterminados; BI= bivalvos indeterminados; NASS= numero total de fosiles recogidos. 3. Indices de riqueza y de diversidad para las dos muestras (humeda y arida), con probabilidades de semejanza p<0.05. Para evaluar la riqueza de especies en las dos muestras, notese que el indice de riqueza Menhinick es mas alto en la asociacion humeda. Este indice intenta compensar el tamano de la muestra (Hammer and Harper, 2008). Otros indices como el de Dominancia, Rareza y Berger-Parker incorpora la abundancia relativa. Notese la alta abundancia y la composicion homogenea de las asociacion arida que dan valores mayores en los indices de Dominancia y de Berger-Parker. Resultados de PAST[c] (Hammer and Harper, 2008). 1) WET 0 0 5 4 25 6 0 44 3 DRY 8 4 15 6 473 222 7 62 124 VAR I * O * C * W * NF NC NB NI A WET 3 0 4 16 4 2 1 0 12 DRY 45 30 11 29 2 1 2 3 453 VAR B C D E F G H I 1 WET 0 0 0 0 8 1 0 DRY 1 1 7 1 7 0 1 VAR 2 3 4 5 6 7 8 2) 3 3 0 4 16 4 2 1 0 12 124 45 30 11 29 2 1 2 3 453 A B C D E F G H I 1 3 0 0 0 0 8 1 0 4 0 124 1 1 7 1 7 0 1 2 23 A 2 3 4 5 6 7 8 FI CI 3 18 0 76 WET 124 14 7 764 DRY A II BI NASS VAR 3) 0 wet dry Boot p(eq) Perm p(eq) Taxa S 12 19 0.615 0.888 Individuals 76 757 0 0 Dominance 0.1489 0.3932 0 0.001 Shannon H 2.127 1.465 0 0.001 Evenness e^AH/S 0.6994 0.2278 0 0 Simpson index 0.8511 0.6068 0 0.001 Menhinick 1.376 0.6906 0.256 0.139 Margalef 2.54 2.715 0.76 0.903 Equitability J 0.8561 0.4976 0 0 Fisher alpha 4.008 3.538 0.464 0.565 Berger-Parker 0.2368 0.5984 0 0 Table 3.--Root transformed data for Cluster Analysis. Leyend as in Table 1. See figure 8 for the resulting Cluster. Tabla 3.--Datos transformados para el analisis de aglomeracion. Leyenda como en la Tabla 1. SQ F NASS NF NC A B C 1 NI02NS5_9 D 10.48 3.16 7.07 6.92 0 0 1.41 NI2NI9 W 3.1 2 0 0 0 0 0 NI10NI15 D 10.58 8.42 3.87 3.74 0 1 8.30 NS1NS4 W 1.73 1 0 0 0 0 0 NS5NS9 D 7.14 2.23 2 1.73 0 0 1.41 NS10NS14 W 2 1 0 0 0 0 0 NSC1NSC5 W 1.73 1.41 0 0 0 0 1 NSC6NSC10 D 13.90 11 4 3.46 0 1 10.86 NSC11 W 1.41 1.41 0 0 0 0 0 R9801R985 W 3.16 1.41 0 0 0 0 1 R986R9815 D 6.92 0 6.70 0 5.29 3.16 0 R9816R9817 W 5.91 2.23 2.23 1.73 1.41 0 1.41 R961.1 W 3 2.82 1 0 1 0 2.82 R962R966 D 19.31 16.46 9.80 7.07 4.12 4.24 16.24 SQ 2 3 4 5 6 7 8 NB NI D NI02NS5_9 0 0 1 0 2.64 0 0 1.41 6.55 2.44 NI2NI9 0 0 0 0 2 0 0 0 2.44 1 NI10NI15 0 0 1 1 0 0 0 0 3 1.41 NS1NS4 0 0 0 0 0 0 0 0 1.41 0 NS5NS9 0 0 1 0 1.41 0 0 1 5.83 2 NS10NS14 0 0 0 0 0 0 0 0 1.73 1 NSC1NSC5 0 0 0 0 1 0 0 0 1 0 NSC6NSC10 0 0 1.41 0 0 0 1 0 2.44 1.73 NSC11 0 0 0 0 1 1 0 0 0 0 R9801R985 0 0 0 0 1 0 0 0 2.82 1 R986R9815 0 0 0 0 0 0 0 1.73 0 0 R9816R9817 0 0 0 0 1 0 0 0 4.90 1 R961.1 0 0 0 0 0 0 0 0 0 0 R962R966 1 1 1.73 0 0 0 0 1.41 2 0 SQ E F G H I NI02NS5_9 5.29 1.41 1 1.41 1.41 NI2NI9 1 1.41 1 0 0 NI10NI15 1 0 0 0 0 NS1NS4 1.41 0 0 0 0 NS5NS9 4.58 1.41 1 1.41 1.41 NS10NS14 1 0 1 0 0 NSC1NSC5 1 0 0 0 0 NSC6NSC10 0 0 0 0 1 NSC11 0 0 0 0 0 R9801R985 2 1 0 0 0 R986R9815 0 0 0 0 0 R9816R9817 2.64 1 0 1 0 R961.1 0 0 0 0 0 R962R966 0 0 0 0 0 Table 4.--Data of the discriminant analysis. Variables are the same as Table 1, except for FI = undetermined fish. II = undetermined insects. c = cycles. Tabla 4.--Datos para el analisis discriminante. Las variables son las mismas que en la Tabla 1, excepto FI y II que indican peces e insectos indeterminados, respectivamente; c=ciclos. SL F N FI A B C 1 NgI02R D 59 0 76.2 0 0 0 NgI2A W 1 0 0 0 0 0 NgI6A W 1 0 0 0 0 0 NgI7A W 7 0 0 0 0 0 NgI9A W 1 0 0 0 0 0 NgI10R D 47 0 2.13 0 0 97.87 NgI11R D 1 0 0 0 0 0 NgI12R D 31 0 25.8 0 0 61.2 NgI1314R D 3 0 0 0 0 66.6 NgI1415R D 30 0 16.6 0 3.33 6.66 NgS1A W 0 0 0 0 0 0 NgS2A W 1 100 0 0 0 0 NgS4A W 2 0 0 0 0 0 NgS5R D 5 0 40 0 0 20 NgS7R D 3 0 0 0 0 0 NgS8R D 2 0 0 0 0 0 NgS9R D 41 0 2.43 0 0 2.43 NgS1012A W 3 33.3 0 0 0 0 NgS14A W 1 0 0 0 0 0 NSC1A W 0 0 0 0 0 0 NSC3A W 2 0 0 0 0 50 NSC45A W 1 0 0 0 0 0 NSC6R D 108 0 5.55 0 0 92.59 NSC7R D 22 0 18.18 0 0 59.09 NSC8R D 12 0 0 0 0 8.333 NSC910R D 51 0 3.92 0 1.960 7.843 NSC11A W 2 0 0 0 0 0 RS0198A W 4 0 0 0 0 0 RS298A W 4 0 0 0 0 0 RS3 498A W 0 0 0 0 0 0 RS598A W 2 0 0 0 0 50 RS698 * D 1 0 0 0 0 0 RS798 * D 0 0 0 0 0 0 RS1198 * D 8 0 0 12.5 87.5 0 RS1398R D 8 0 0 25 37.5 0 RS1498R D 26 0 0 80.76 0 0 RS1598R D 5 0 0 80 0 0 RS1698A W 6 0 0 0 0 0 RS1798A W 29 0 10.34 6.89 0 6.89 RS1.196A W 9 0 0 11.11 0 88.8 RS296R D 27 0 11.11 3.70 0 77.7 RS396R D 36 0 11.11 16.66 5.55 58.33 RS496R D 29 0 31.03 17.24 10.34 41.37 RS596R D 275 0 11.63 1.45 4.72 75.63 RS696R D 6 0 33.33 16.66 0 33.33 SL 2 3 4 5 6 NB NgI02R 0 0 0 0 8.47 1.694 NgI2A 0 0 0 0 0 0 NgI6A 0 0 0 0 0 0 NgI7A 0 0 0 0 57.14 0 NgI9A 0 0 0 0 0 0 NgI10R 0 0 0 0 0 0 NgI11R 0 0 0 100 0 0 NgI12R 0 0 0 0 0 0 NgI1314R 0 0 0 0 0 0 NgI1415R 0 0 3.33 0 0 0 NgS1A 0 0 0 0 0 0 NgS2A 0 0 0 0 0 0 NgS4A 0 0 0 0 0 0 NgS5R 0 0 0 0 0 0 NgS7R 0 0 0 0 0 0 NgS8R 0 0 0 0 0 0 NgS9R 0 0 2.44 0 4.87 2.43 NgS1012A 0 0 0 0 0 0 NgS14A 0 0 0 0 0 0 NSC1A 0 0 0 0 0 0 NSC3A 0 0 0 0 50 0 NSC45A 0 0 0 0 0 0 NSC6R 0 0 0 0 0 0 NSC7R 0 0 0 0 0 0 NSC8R 0 0 16.6 0 0 0 NSC910R 0 0 0 0 0 0 NSC11A 0 0 0 0 50 0 RS0198A 0 0 0 0 25 0 RS298A 0 0 0 0 0 0 RS3 498A 0 0 0 0 0 0 RS598A 0 0 0 0 0 0 RS698 * 0 0 0 0 0 0 RS798 * 0 0 0 0 0 0 RS1198 * 0 0 0 0 0 0 RS1398R 0 0 0 0 0 25 RS1498R 0 0 0 0 0 0 RS1598R 0 0 0 0 0 20 RS1698A 0 0 0 0 0 0 RS1798A 0 0 0 0 3.44 0 RS1.196A 0 0 0 0 0 0 RS296R 0 0 0 0 0 0 RS396R 0 0 2.77 0 0 0 RS496R 0 0 0 0 0 0 RS596R 0.36 0.363 0.72 0 0 0.72 RS696R 0 0 0 0 0 0 SL II 7 D E F G NgI02R 0 0 3.389 11.86 0 0 NgI2A 0 0 0 0 100 0 NgI6A 0 0 0 0 0 100 NgI7A 0 0 14.28 0 14.28 0 NgI9A 0 0 0 100 0 0 NgI10R 0 0 0 0 0 0 NgI11R 0 0 0 0 0 0 NgI12R 3.225 0 6.451 3.225 0 0 NgI1314R 33.33 0 0 0 0 0 NgI1415R 13.33 0 0 0 0 0 NgS1A 0 0 0 0 0 0 NgS2A 0 0 0 0 0 0 NgS4A 0 0 0 100 0 0 NgS5R 0 0 0 0 0 0 NgS7R 66.66 0 33.33 0 0 0 NgS8R 0 0 0 100 0 0 NgS9R 2.43 0 7.31 46.34 4.87 2.43 NgS1012A 0 0 33.33 0 0 33.33 NgS14A 0 0 0 100 0 0 NSC1A 0 0 0 0 0 0 NSC3A 0 0 0 0 0 0 NSC45A 0 0 0 100 0 0 NSC6R 0.925 0 0 0 0 0 NSC7R 0 0 9.090 0 0 0 NSC8R 0 0 0 0 0 0 NSC910R 1.960 0 1.960 0 0 0 NSC11A 0 50 0 0 0 0 RS0198A 0 0 0 50 25 0 RS298A 25 0 25 50 0 0 RS3 498A 0 0 0 0 0 0 RS598A 50 0 0 0 0 0 RS698 * 0 0 0 0 0 0 RS798 * 0 0 0 0 0 0 RS1198 * 0 0 0 0 0 0 RS1398R 0 0 0 0 0 0 RS1498R 0 0 0 0 0 0 RS1598R 0 0 0 0 0 0 RS1698A 83.33 0 0 16.66 0 0 RS1798A 31.03 0 3.44 20.6 3.44 0 RS1.196A 0 0 0 0 0 0 RS296R 0 0 0 0 0 0 RS396R 5.55 0 0 0 0 0 RS496R 0 0 0 0 0 0 RS596R 0 0 0 0 0 0 RS696R 0 0 0 0 0 0 SL H I 8 c NgI02R 0 0 0 3 NgI2A 0 0 0 3 NgI6A 0 0 0 3 NgI7A 0 0 0 3 NgI9A 0 0 0 3 NgI10R 0 0 0 2 NgI11R 0 0 0 2 NgI12R 0 0 0 2 NgI1314R 0 0 0 2 NgI1415R 0 0 0 2 NgS1A 0 0 0 4 NgS2A 0 0 0 4 NgS4A 0 0 0 4 NgS5R 20 0 0 3 NgS7R 0 0 0 3 NgS8R 0 0 0 3 NgS9R 2.43 4.87 0 3 NgS1012A 0 0 0 3 NgS14A 0 0 0 3 NSC1A 0 0 0 3 NSC3A 0 0 0 3 NSC45A 0 0 0 3 NSC6R 0 0 0.92 2 NSC7R 0 0 0 2 NSC8R 0 0 0 2 NSC910R 0 1.960 0 2 NSC11A 0 0 0 2 RS0198A 0 0 0 2 RS298A 0 0 0 2 RS3 498A 0 0 0 2 RS598A 0 0 0 2 RS698 * 0 0 0 1 RS798 * 0 0 0 1 RS1198 * 0 0 0 1 RS1398R 0 0 0 1 RS1498R 0 0 0 1 RS1598R 0 0 0 1 RS1698A 0 0 0 1 RS1798A 3.44 0 0 1 RS1.196A 0 0 0 3 RS296R 0 0 0 3 RS396R 0 0 0 2 RS496R 0 0 0 2 RS596R 0 0 0 2 RS696R 0 0 0 2 Table 5.--Discriminant Function. Function offset constant =0.634897. Variables are the same than in Table 4. Tabla 5.--Funcion discriminante. FI A B C 1 2 -0.0585 0.10853 0.053022 0.060514 0.030257 -0.20845 FI 3 4 5 6 NB -0.0585 -0.20845 0.3605 0.056578 -0.10785 0.074483 FI II 7 D E F -0.0585 -0.03394 0.011488 0.06540 -0.03378 -0.04671 FI G H I 8 -0.0585 -0.05868 -0.00739 1.4611 2.3516 Fig. 6.-Diversity recorded in Las Hoyas. Specimens figured correspond: Ostheichthyes-Turbomesodon MCCMLH-9266; Amphibia-Eodiscoglossus; Squamata-MeyasaurusMCCMLH-370; Dinosauria-Pelecanimimus MCCMLH-777; Dicksoniaceae: Onychiopsis; MCCMLH-29503; Heteroptera: Iberonepa MCCMLH-17087, and Caridea: Declosia.MCCMLH-280. Fossils housed at Museo de las Ciencias de Castilla-La Mancha in Cuenca (Spain) Fig. 6.-Figura compuesta de la diversidad registrada en el yacimiento de Las Hoyas. Los especimenes figurados correspondena: Ostheichthyes-TurbomesodonMCCMLH-9266; Amphibia-Eodiscoglossus; Squamata-MeyasaurusMCCMLH-370; Dinosauria-Pelecanimimus; MCCMLH-777; Dicksoniaceae: OnychiopsisMCCMLH-29503; Heteroptera: Iberonepa MCCMLH-17087, and Caridea: Declosia MCCMLH-280. Fosiles pertenecientes a las coleccion del Museo de las Ciencias de Castilla-La Mancha en Cuenca (Espana). Archosauria 9% Squamata 3% Amphibia 5% Ostheichtyyes 14% Antropoda 45% Mollusca 2% Pteridophyta + Spermatophyta 15% Bryophyta 1% Charophyta 6% Note: Table made from pie chart.
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|Author:||Buscalioni, A.D.; Fregenal-Martinez, M.A.|
|Publication:||Journal of Iberian Geology|
|Date:||Jul 1, 2010|
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