Printer Friendly

Stegocornu and associated brachiopods from the Silurian (Llandovery) of Central Iran/ Stegocornu ja kaasnevad brahhiopoodid Kesk-Iraani Silurist (Llandovery).

INTRODUCTION

The only published report on the occurrence of Silurian brachiopods in Central Iran is the paper by Brice (1999). Her study was based on a small collection sampled by the late A. F. de Lapparent in 1973, from a small outcrop of Silurian sediments, now assigned to the Shabdjereh Formation, in the vicinity of the Khanuk village. A more substantial record of the Silurian brachiopods from Kope-Dagh in northeastern Iran can be found in the paper by Cocks (1979) where he described 23 taxa. His study was based on a collection sampled at 2.5 km northeast of Robat-e-Qarabil, from a single bed about 33 m above the base of the Qarabil Limestone Formation designated in that publication. This is the type locality of Xerxespirifer iranicus Cocks, 1979, which for some time became a taxonomic puzzle. In particular, Carter et al. (1994) suggested that Xerxespirifer is not a spiriferidine, but more likely has rhynchonellide or leptocoellid affinity. Alvarez & Rong (2002) questionably assigned this genus to the athyridide family Retziellidae, whereas Brice (1999) and Savage et al. (2002) considered Xerxespirifer as possible junior objective synonym of Stegocornu, which has found support in the present study.

The rhynchonellide Stegocornu is a core taxon in the shallow-water fauna of the Benthic Assemblage Zone 2 (BA 2) in Central Iran, which can be termed as the Stegocornu Association. It occurs also in Robat-e-Qarabil and the Saluk Mountains, both located in the Kope-Dagh region of northeastern Iran (Fig. 1; Cocks 1979 and new unpublished observations by M. Ghobadi Pour), and in Afghanistan (Durkoop 1970). The age of the Stegocornu fauna is defined as mid- to late Aeronian by co-occurrence with characteristic conodonts.

OUTLINE OF FOSSIL LOCALITIES

Kashmar region

The major source of the studied brachiopods in the area is Silurian deposits of the Niur Formation, exposed in the Boghu Mountains about 25 km southwest of the town of Kashmar (Fig. 1). The geographical coordinates of the base of the measured section are 34[degrees]04'6.2"N, 58[degrees]15'48.8"E, altitude 1222 m. The geographical coordinates for the top of the section are 35[degrees]04'43.3"N, 58[degrees]15'14.7"E, altitude 1266 m. Here a succession of the lower to middle Silurian sediments, assigned to the Niur Formation, is well exposed on the southern flank of the Boghu Mountains. It is underlain by an unnamed formation of Upper Ordovician siliciclastic rocks. The sampled section consists of highly fossiliferous limestones, shales and sandstone/siltstone units. The lowermost part of the measured section comprises green siltstone/shale beds intercalating with thin tentaculitid limestones and sandstones, which were assigned to the Niur Formation and dated by conodonts as lowermost Llandovery on the geological map of Kashmar (GSI 2001a, sheet 1 : 100 000). However, the occurrence of Icriodella in association with Amorphognathus within this interval (Fig. 2, unit 1, samples K5-K10) clearly indicates an Upper Ordovician (Sandbian-Katian) age (P. Mannik and C. G. Miller, pers. comm. 2011).

[FIGURE 1 OMITTED]

Conodonts from sample K25 (Fig. 2, unit 18) have been identified as Distomodus staurognathoides (Walliser, 1964), Wurmiella ex. gr. excavata, Ozarkodina spp. and Oulodus? sp., suggesting an age not older than the mid-Aeronian. Samples K28 and K29 (Fig. 2, unit 20) contain a similar conodont fauna, including Distomodus staurognathoides. The latter species is also documented from sample K37 (Fig. 2, unit 22), where it occurs together with Kockelella ranuliformis (Walliser, 1964), suggesting an early Sheinwoodian age.

[FIGURE 2 OMITTED]

In the Boghu section Stegocornu procerum Durkoop, 1970 was sampled from two horizons (Fig. 2). In the lowermost sample K25 it occurs in association with a few specimens of Clorinda sp. and Mesoleptostrophia (Mesoleptostrophia) sp., whereas in sample K28 it forms a monotaxic association. The first occurrence of Stegocornu denisae sp. nov. is documented from sample K29, about 25 m above sample K28. The second horizon with Stegocornu denisae in association with a few Striispirifer? ocissimus sp. nov. is about 15 m higher (Fig. 2, sample K30).

Derenjal Mountains

The area is located about 65 km northwest of Tabas (Fig. 1; see also Ruttner et al. 1968; Hairapetian et al. 2008). Here Silurian sediments assigned to the Niur Formation are exposed on the eastern side of the Dahaneh-e-Kolut gorge and have a faulted contact against the lower Early-Middle Ordovician Shirgesht Formation (Bruton et al. 2004; Ghobadi Pour et al. 2006). The upper boundary of the Niur Formation represents a conformable contact with the presumably Lower Devonian Padeha Formation (Ruttner et al. 1968).

A measured section of the Niur Formation, in total 551 m thick, is exposed in three major hills named A, B and C (Hairapetian et al. 2008). The sedimentary succession through Hill A (units 1-4) consists of medium- to thin-bedded limestones, siltstones and argillites with abundant corals, brachiopods, ostracods, crinoids and trilobites (Fig. 2). Unit 2 is sandwiched between two horizons of volcanic rocks representing submarine basaltic lava flows (Fig. 2, units 1 and 3). The sedimentary unit was dated as mid-Aeronian, based on ostracods and brachiopods (Hairapetian et al. 2011).

Silurian deposits exposed on Hill B (base of the section at 34[degrees]5'2.9"N, 56[degrees]48'14"E; altitude 1040 m) comprise sandstone and bioclastic sandy limestone. The limestone beds yield an abundant fauna of brachiopods, corals, cephalopods, tentaculitids, conodonts, ostracods and trilobites. The Stegocornu Brachiopod Association was sampled from a single sample S14 in the middle part of Unit 7 (Fig. 2). It is dominated by two species, namely Isorthis (Ovalella) inflate sp. nov. (54%) and Stegocornu denisae sp. nov. (32%). Other associated brachiopod taxa include Dalejina? rashidii sp. nov. (4%), Hercotrema sp. (< 2%), Mesoleptostrophia (Mesoleptostrophia) sp. (1%), Rhytidorhachis? sp. (<1%) and Striispirifer? ocissimus sp. nov. (6%).

A conodont assemblage from the underlying Unit 6 (Fig. 2, sample S12) contains Wurmiella excavata cf. puskuensis (Mannik, 1994), Distomodus staurognathoides (Walliser), Ozarkodina sp. and a few elements of Panderodus and Oulodus? suggesting a mid- to late Aeronian age (unpublished data by P. Mannik, C. G. Miller and V. Hairapetian). Similar conodonts were recovered also from the overlying Unit 7 (Fig. 2; S15, S16 and S17). The occurrence of Pterospathodus amorphognathoides lennarti Mannik, the index species of the conodont biozone, in sample S19 in the uppermost part of Unit 11 (Fig. 2) indicates a mid-Telychian age (unpublished data by P. Mannik, C. G. Miller and V. Hairapetian). Thus from the available conodont data the age of the brachiopod fauna from sample S14 is probably mid- to late Aeronian.

The part of the Niur Formation exposed on Hill C (Fig. 2, units 13-20) is dated from Wenlock to Pndoli (Flugel & Saleh 1970; Hairapetian et al. 2008). It comprises dark grey argillaceous limestones, dolomitic limestones and dolomites with abundant brachiopods, gastropods, ostracods, corals and fish microremains.

Kerman region

Geographical coordinates of the locality, in the vicinity of the Khanuk village published by Brice (1999) are undoubtedly erroneous and the precise location and sedimentary logs of the sampled section remain unknown. Probably it was located somewhere southeast of the village, where the Shabdjereh Formation is exposed (Fig. 1). The specimens of Stegocornu aff. procerum Durkoop, 1970 (here re-assigned to Stegocornu denisae sp. nov.) have been identified from two individual samples. According to Brice (1999), they occur in association with Hedeinopsis spp. and Nikiforovaena? sp. The latter shells are probably assignable to Striispirifer? ocissimus.

The precise taxonomical affiliation of two other taxa referred to Howellella and Rhynchotrema is questionable.

Another small collection from the Kerman region was handed to T. L. Modzalevskaya by the late Prof. Stepanov (St Petersburg University) and has recently been donated to the Central Geological Research and Exploration Tschernyshev Museum (St Petersburg). These brachiopods were sampled by an anonymous Iranian geologist from an outcrop in the vicinity of the Shabdjereh village (Fig. 1). Geological and geographical information for the collection is not available. The specimens were most likely derived from a loose sample, as they include both Stegocornu procerum and Stegocornu denisae, which do not co-occur in the same horizon.

SIGNIFICANCE OF THE FAUNA

In Central Iran Stegocornu is represented by two species, namely Stegocornu procerum and Stegocornu denisae, which succeed each other in the sequence. Both species either dominated in low-diversity associations, usually including Striispirifer? (Kashmar and Kerman regions), or were an important part of more diverse associations together with various orthides, spiriferides and strophomenides (e.g. the Derenjal Mountains and Kope-Dagh).

In the Derenjal Mountains abundant Stegocornu denisae, and Striispirifer? ocissimus and rare Hercotrema sp. and Rhytidorhachis? sp. occur as conjoined valves, whereas Isorthis (Ovalella) inflata and Dalejina? rashidii are preserved as numerous disarticulated valves in shell accumulations with a few disarticulated valves of Stegocornu. It is probable that the brachiopod association from sample S14 represents a mixture of mainly autochthonous rhynchonellide and spiriferide shells, and allochthonous shells of Isorthis (Ovalella) and Dalejina?, which were transported into the area during seasonal storms.

In the type locality in Dascht-e-Nawar, eastern Afghanistan, Stegocornu procerum occurs together with conodonts identified as Lonchodina cf. fluegeli (Walliser, 1964) (Durkoop 1970, p. 159), which may be an element of Aspelundia? fluegeli (Walliser, 1964) known from the late Aeronian-Telychian. In the Kashmar section, eastern Central Iran, Stegocornu procerum co-occurs with a conodont assemblage, suggesting an age not older than mid-Aeronian. The succeeding species Stegocornu denisae is found in the Shirgesht section well below the first documented appearance of the index species of the mid-Telychian Pterospathodus amorphognathoides lennarti Biozone and within the range of Wurmiella excavata cf. puskuensis (Mannik), which is considered as the early member of the W. excavata lineage. These finds suggest that the proliferation of Stegocornu in Afghanistan and Central Iran took place within a narrow time span from the mid- to late Aeronian.

Dispersion of the Stegocornu Association in Central Iran, Kope-Dagh and Afghanistan in the late Aeronian represents a significant regional event. Stegocornu has a short stratigraphic range and its occurrence can be considered as a good indication of Aeronian age, in particular, for the faunas described earlier by Cocks (1979) from Kope-Dagh and by Brice (1999) from the Kerman Region.

Boucot & Blodgett (2001) consider the presence of Xerxespirifer (= Stegocornu) in Iran as indication of biogeographical differentiation within their North Silurian Realm in Wenlock time. New data suggest that proliferation of the Stegocornu Association had occurred already in the mid- to late Llandovery. At that time peri-Gondwanan terranes of Central Iran, KopeDagh and Afghanistan supported shallow-water faunas bearing a common biogeographical signature, suggesting their position in relative proximity to each other, and probably in temperate southern palaeolatitudes.

SYSTEMATIC PALAEONTOLOGY

Abbreviations for parameters measured on specimens are: W, L, T = maximum width, length, thickness of the shell; Lv, Ld = maximum length of the ventral and the dorsal valve; Iw = maximum width of the interararea; Sw, St = width and depth of the sulcus at the anterior margin; Mw, Ml = width, length of the muscle field; SVl = length of the ventral median septum; BBw = distance between outer margins of brachiophores; BBl = brachiophore length; Sl = distance from the umbo to anterior termination of the median ridge; X = mean; S = standard deviation from the mean; N = number of specimens; max = maximum observed size; min = minimum observed size. All measurements are in millimetres.

The illustrated and described material is housed in the National Museum of Wales, Cardiff (NMW), in the Central Geological Research and Exploration Tschernyshev Museum (St Petersburg) and Azad University, Esfahan (AEU). The authorship of the new taxa is as follows: Popov, Modzalevskaya & Ghobadi Pour.

Order STROPHOMENIDA Opik, 1934

Superfamily STROPHOMENOIDEA King, 1846

Family LEPTOSTROPHIIDAE Caster, 1939

Genus Mesoleptostrophia Harper & Boucot, 1978

Type species. Mesoleptostrophia kartalensis Harper & Boucot, 1978 (nom. nov. pro Stropheodonta (Leptostrophia) explanata Paeckelman & Sieverts, 1932, non Sowerby, 1842); Lower Devonian, Emsian, Kartal-Schichten, Turkey.

Mesoleptostrophia (Mesoleptostrophia) sp. Figure 3A, B

Material. NMW 2011.11G.10, 11, ventral valves; NMW 2011.11G.8, 9, 12, dorsal valves; sample K25, Boghu Mountains. NMW 2011.11G.6, 7, ventral valves; sample S14, Derenjal Mountains. Total four ventral and three dorsal valves.

Description. Shell weakly concavoconvex to almost biplanate, transverse subrectangular with maximum width slightly anterior to the hinge line; anterior commissure rectimarginate.

[FIGURE 3 OMITTED]

Ventral valve very weakly convex with a low, planar, apsacline interarea; delthyrium covered by a small pseudodeltidium. Dorsal valve planar anteriorly, weakly concave between the umbo and midlength. Dorsal interarea linear, anacline. Radial ornament subequally parvicostellate with one, rarely two parvicostellae between accentuated ribs and with up to 9 ribs per 3 mm in mature specimens. Concentric ornament of regular, very fine, densely spaced fila.

Ventral interior with transverse denticulate plates on both sides of the delthyrium and a large, open anteriorly, subtriangular muscle field terminated almost at midvalve and bisected medially by a faint median ridge. Posterolateral muscle bounding ridges prominent, straight, widely divergent.

Remarks. In shell outline and characters of ventral and dorsal interior Iranian specimens show close similarity to the shells from the Llandovery (Telychian) of Britain illustrated by Harper & Boucot (1978, pl. 1, figs 12-15, 18). They differ from two other British Llandovery (Telychian) species Mesoleptostrophia (Mesoleptostrophia) tenuis (Williams, 1951) and Mesoleptostrophia (Mesoleptostrophia) ostrina (Cocks, 1967) in having obtuse cardinal extremities, more prominent ventral muscle bounding ridges and subequally parvicostellate radial ornament with only one or two parvicostellae between accentuated ribs. The Iranian shells also lack distinct rugellae in the posterior part of the shell reported in the British species. They may represent a new, not yet recognized species of Mesoleptostrophia (Mesoleptostrophia), but inadequate preservation of the cardinalia makes its formal taxonomic designation impossible.

Order ORTHIDA Schuchert & Cooper, 1932

Suborder DALMANELLIDINA Moore, 1952

Superfamily DALMANELLOIDEA Schuchert, 1913

Family ISORTHIDAE Schuchert & Cooper, 1931

Genus Isorthis Kozlowski, 1929

Isorthis (Ovalella) Walmsley & Boucot, 1975

Type species. Dalmanella (Isorthis) szajnochai Kozlowski, 1929; Lower Devonian, Borshchov Formation, Podolia, Ukraine.

Isorthis (Ovalella) inflata sp. nov. Figures 3C-J, 4; Tables 1, 2

Derivation of name. Latin inflatus--swollen.

Holotype. NMW 2011.11G.91, holotype, dorsal valve, Llandovery, mid-late Aeronian, Niur Formation, sample S14, Derenjal Mountains, Iran.

Paratypes. NMW 2011.11G.373 (L = 11.8, W = 12.5, T = 6.2, Iw = 11.2); NMW 2011.11G.14-89, 114.3, 114.5, ventral valves; NMW 2011.11G.90, 91-112, 114.1, 114.2, 114.4, 114.6, 114.7, 115-192, dorsal valves; locality and stratum as for the holotype. Total one articulated shell, 78 ventral and 95 dorsal valves.

Diagnosis. Shell dorsibiconvex; transverse suboval to almost subrectangular outline, with maximum width between hinge line and midlength; radial ornament multicostellate, with 11-13 rounded ribs per 3 mm along the anterior margin; ventral muscle field large, bilobed, elongate, extended anterior to midlength; cardinal process undivided.

Description. Shell dorsibiconvex, slightly transverse suboval to almost subrectangular in outline, about 95% as long as wide, with maximum width between hinge line and midlength. Hinge line about four fifths as wide as the shell; cardinal extremities rounded. Anterior commissure weakly sulcate. Lateral profile of the ventral valve moderately and evenly convex with maximum height slightly posterior to midlength; transverse profile subcarinate. Ventral interarea gently curved, apsacline, with an open delthyrium. Dorsal valve lateral profile gently convex with maximum height at about one third valve length from the umbo. Dorsal sulcus originating at the umbo, slightly deepening towards midvalve and fading towards anterior margin in mature specimens. Dorsal intearea low, planar, anacline. Radial ornament finely and equally multicostellate with 11-13 rounded ribs per 3 mm along the anterior margin of mature specimens.

Ventral interior with small subtriangular teeth supported by slightly divergent dental plates. Ventral muscle field bilobed, elongate, strongly impressed, extending beyond the midvalve length and surrounded by faint muscle bounding ridges. Ventral median ridge long and narrow, slightly widening anteriorly. Ventral vascula media short, divergent. Dorsal interior with a small, bulbous undivided cardinal process bearing posteriorly a crenulated myophore and supported anteriorly by faint, ridge-like shaft. Brachiophores blunt, subtriangular, slightly divergent anteriorly with almost subparallel bases. Dental sockets large, subtriangular, supported by thickened socket pads. Dorsal adductor muscle field narrow, elongate, surrounded by faint muscle bounding ridges, extending anteriorly beyond midlength and bisected by low and broad median ridge.

Remarks. Distinctive features of Isorthis (Ovalella) and its affinity to Isorthis (Arcualla) were discussed repeatedly in publications by Walmsley & Boucot (1975), Zhang (1989), Strusz (2002) and Li & Copper (2006). The Iranian shells are referred to Isorthis (Ovalella), because they have a narrow ventral median ridge, an undivided cardinal process, low and broad dorsal median ridge and indistinctly quadripartite, weakly defined dorsal adductor muscle field. Isorthis (Ovalella) inflata sp. nov. differs from other species of the genus in having a large ventral muscle field extending slightly anterior to midvalve and a long, very narrow ventral median ridge bisecting the muscle field. It differs also: (a) from I. (Ovalella) beechhillensis Walmsley & Boucot, 1975 (Llandovery, Rhuddanian, of Nova Scotia, Quebec) in having a wider delthyrium and maximum shell width only slightly anterior to the hinge line; (b) from I. (Ovalella) mackenziei Walmsley, 1966 (Llandovery, Telychian to lower Wenlock of New Brunswick, Maine and Wales) in having a more transverse shell with maximum width posterior to midlength.

[FIGURE 4 OMITTED]

Isorthis (Ovalella) arndellensis Laurie, 1991, from the Llandovery, Westfield Sandstone of Tasmania and I. (Ovalella) natiscoteca Li & Copper, 2006, from the Llandovery, Rhuddanian, of Anticosti Island, have a bilobed cardinal process unlike I. (Ovalella) inflata, which is undivided.

Family RHIPIDOMELLIDAE Schuchert, 1913

Subfamily RHIPIDOMELLINAE Schuchert, 1913

Genus Dalejina Havlicek, 1953

Type species. Dalejina hanusi Havlicek, 1953; Lower Devonian, Pragian, Zlichov Limestone, Bohemia.

Dalejina? rashidii sp. nov. Figure 5A-P

Derivation of name. After Dr Koorosh Rashidi (Payame Noor University of Ardakan) in recognition of his kind assistance during the fieldwork in the Tabas region. Holotype. NMW 2011.11G.205 (Ld = 19.0, W = 19.0, T = 7.4, BBw = 6.2, BBl = 3.5, Sl = 4.6), Llandovery, mid-late Aeronian, Niur Formation, sample S14, Derenjal Mountains, Iran.

Paratypes. NMW 2011.11G.194, 197 (Lv = 13.6, W = 16.4), 198 (Lv = 10.2, W = 12.9, Iw = 9.7, Ml = 5.8, Mw = 5.7, Sl = 6.6), 199, 200 (Lv = 15.2, W = 18.0. Ml = 7.6, Mw = 5.8, SVl = 9.5), 201 (Lv = 16.2, W = 19.8, Iw = 11.3, Ml = 9.8, Mw = 7.3, Sl = 11.9), 208, ventral valves; NMW 2011.11G.195 (Ld = 17.3, W = 20.1; T = 4.4), 202, 206 (Ld = 12.5, W = 14.7, T = 4.3, BBw = 4.7, BBl = 2.8, Sl = 4.1), 208-212, 370, dorsal valves; locality and stratum as holotype. Total seven ventral and nine dorsal valves.

Diagnosis. Shell strongly dorsibiconvex, about 80% as long as wide; anterior commissure weakly uniplicate; ventral muscle field large, subcordate, slightly elongated, extending anterior to the midvalve and bisected by long median ridge terminating at about one third valve length from the anterior margin; dorsal interior with undivided cardinal process with a broad shaft on a high notothyrial platform; brachiophores stout, divergent at about right angle; dorsal median ridge terminated at about middle of a weakly impressed dorsal adductor muscle field.

[FIGURE 5 OMITTED]

Description. Shell strongly dorsibiconvex, slightly transverse suboval, about four fifths as long as wide. Hinge line about two thirds of maximum shell width at midlength, cardinal extremities broadly rounded. Anterior commissure weakly uniplicate. Ventral valve sagittal profile gently convex with maximum height at about one third valve length from the umbo. Ventral interarea low, curved with an open, triangular delthyrium. Ventral sulcus very broad and shallow, almost indistinguishable, originating at 3-4 mm from the umbo. Dorsal valve strongly and evenly convex in sagittal and transverse profiles, with rudimentary, strongly apsacline interarea. Radial ornament equally multicostellate with up to 6 ribs per 3 mm along the anterior margin of mature specimens. Concentric ornament of fine, evenly spaced fila and growth lamellae, in the anterior half of the shell.

Ventral valve interior with strong teeth and short, widely divergent dental plates. Ventral muscle field strongly impressed, large, subcordate, about four fifths as long as wide, extending well beyond the midvalve, surrounded by strong muscle bounding ridges. Thickened pedicle callist present in the posterior part of the delthyrial cavity bottom. Ventral median ridge bisecting the entire muscle field, extending anteriorly and terminating at about one third valve length from the anterior margin. Ventral diductor muscle scars large, strongly impressed, enclosing completely weakly defined adductor muscle scars in the posterior half of the muscle field.

Dorsal interior with high, stout brachiophores divergent at about right angles and deep, subtriangular dental sockets supported by socket pads. Fulcral plates present. Cardinal process undivided, with a broad, thickened shaft and crenulated myophore facing posteriorly, situated on a high, subtriangular notothyrial platform. Dorsal adductor muscle field weakly impressed, with only smaller anterior pair of adductor scars clearly discernable. Dorsal median ridge very short, terminated at the midpart of the adductor muscle field.

Remarks. The generic assignment of Dalejina? rashidii sp. nov. is questionable, because, unlike almost all other known species of the genus (e.g. Boucot et al. 1965), it has a simple, undivided cardinal process. It probably represents the oldest documented species of Dalejina. Williams & Harper (2000) considered the stratigraphic range of Dalejina as Wenlock to Emsian, however, there is a species assignable to Dalejina from the Llandovery of the East Baltic, described originally as Rhipidomelloides phaseola Rubel, 1963, from the Adavere Regional Stage (Telychian) of Estonia. Unlike Iranian shells it has a bilobed cardinal process, a strongly dorsibiconvex shell and a larger ventral muscle field extending anterior to midvalve.

Dalejina? rashidii sp. nov. differs from Dalejina hybrida (J. de. Sowerby, 1839), which is widespread in the Wenlock to Ludlow of Britain and Baltoscandia, in having a simple, undivided cardinal process, a more strongly dorsibiconvex shell, a weakly defined anterior border of the ventral muscle field, a very short dorsal median ridge and coarser radial ornament. Iranian shells are also almost twice as large as the average size of Dalejina hybrida given by Bassett (1972).

Among the early species of the genus, Dalejina phedodra Bassett, 1972 from the Wollhope Limestone (base of the Wenlock Series) of the Welsh Borderland is probably the closest species to the newly described taxon. It also has a large, weakly defined anteriorly ventral muscle field, an undivided, inflated cardinal process, a short dorsal median ridge and a relatively large shell size. Iranian shells can be distinguished from the British species in complete absence of the dorsal sulcus and in having a ventral median ridge extending beyond the anterior border of the muscle field, a very short dorsal median ridge bisecting only the posterior half of the dorsal muscle field and less strongly transverse adult shells.

Order PENTAMERIDA Schuchert & Cooper, 1931

Suborder PENTAMERIDINA Schuchert & Cooper, 1931

Superfamily CLORINDOIDEA Rzhonsnitskaya, 1956

Family CLORINDIDAE Rzhonsnitskaya, 1956

Subfamily CLORINDIDINAE Rzhonsnitskaya, 1956

Genus Clorinda Barrande, 1879

Type species. Clorinda armata Barrande, 1879, Hlubocepy Limestone, Prague region, Czech Republic.

Clorinda sp.

Figure 6N-Q

1979 Clorinda? sp.; Cocks, p. 36, fig. 27.

Material. Conjoined valves: NMW 2011.11G.1 (Lv = 16.1, Ld = 13.5, T = 10.8, Sw = 8.6), sample K25, Boghu Mountains.

Remarks. A single specimen from the Niur Formation of the Boghu Mountains is characterized by a low, flattened ventral sulcus and dorsal median fold originating at the umbonal area and smooth flanks. It shows distinct similarity to the ventral valve of Clorinda? sp. illustrated by Cocks (1979, fig. 27). These shells may well be conspecific, but the limited material and absence of data on the interior of both valves makes their precise taxonomic discrimination impossible.

Order RHYNCHONELLIDA Kuhn, 1949

Superfamily RHYNCHOTREMATOIDEA Schuchert, 1913

Family RHYNCHOTREMATIDAE Schuchert, 1913

Subfamily RHYNCHOTREMATINAE Schuchert, 1913

Genus Stegocornu Durkoop, 1970

Type species. Stegocornu procerum Durkoop, 1970; Silurian, Aeronian, Dascht-e Nawar, eastern Afghanistan.

Remarks. Stegocornu was originally described by Durkoop (1970) from eastern Afghanistan, but was subsequently also identified by Brice (1999) from a small collection of the Silurian brachiopods sampled by A. F. de Lapparent in 1973 northwest of Kerman. Brice also pointed out the close resemblance of these shells to Xerxespirifer iranicus Cocks, 1979 from the Silurian Qarabil Formation of Kope-Dagh. There was, however, an issue of taxonomic relationship of the illustrated specimens with the holotype of Xerxespirifer iranicus, which represents a small, strongly biconvex shell with a short hinge line, a single narrow rib in the sulcus and four ribs on flanks of the ventral valve. It looks rather atypical for Stegocornu according to Brice (1999). Subsequently Savage et al. (2002) also considered Xerxespirifer as junior objective synonym of Stegocornu.

From the studied collection it is likely that the holotype of Xerxespirifer iranicus is within the margins of significant morphological variability characteristic of Stegocornu procerum, but additional study based on the topotype material is still required to resolve the problem of taxonomic relationships between Stegocornu and Xerxespirifer.

Stegocornu procerum Durkoop, 1970

Figures 7A-H, 8; Table 3

1970 Stegocornu procerum Durkoop; p. 186; Abb. 48, text-fig. 1; pl. 18, figs 1-6.

1979 Xerxespirifer iranicus Cocks; p. 40, figs 35-39 (?non fig. 34).

2002 Stegocornu procerum Durkoop; Savage et al., fig. 708.3a-n.

Holotype. GPBIo 59, deposited in the Palaeontological Institute, Bonn, Germany, conjoined valves; Silurian, Llandovery, mid-late Aeronian, Shoroj-Sang, Dasht-e-Nawar, eastern Afghanistan.

Material. NMW 2011.11G.213 (Lv = 12.7, Ld = 11.3, W = 15.0, T = 9.9, Sw = 7.3), 252-268, CNIGR 12600/128, 129, AEU 1267-1300, articulated shells; sample K25; NMW 2011.11G.214 (Lv = 12.7, Ld = 11.3, W = 15.0, T = 9.9, Sw = 7.3), 215-251 conjoined valves; sample K28; both samples from the Boghu Mountains. CNIGR 12600/130-133, articulated shells, loose sample, vicinity of Shabdjereh. Total 94 articulated shells.

Diagnosis. See Durkoop (1970, p. 186).

Remarks. The specimens from samples K25 to K28 of the Boghu section are almost identical in morphological characters to the topotypes and considered here as conspecific. The only difference is in the presence of fine crowded concentric lamellae in the anterior half of the Iranian shells, which may be explained by partial exfoliation of the shells studied by Durkoop (1970), as is evident from the provided illustrations. Earlier Brice (1999) suggested that the majority of the shells illustrated by Cocks (1979) under the name Xerxespirifer iranicus Cocks, with the exception of the holotype, are probably conspecific to Stegocornu procerum. This synonymy is also accepted here. Delthyrial plates in S. procerum are completely merged anterior to the pedicle foramen as shown in Fig. 8A.

Stegocornu denisae sp. nov.

Figures 7I-Y, 9, 10; Tables 4, 5

1999 Stegocornu aff. procerum Durkoop; Brice, p. 7; pl. 1, figs 1-6.

Derivation of name. After Prof. Denise Brice (University of Lille) who reported for the first time on the occurrence of Stegocornu in Central Iran.

Holotype. NMW 2011.11G.269 (Lv = 13.8, Ld = 11.9, W = 18.8), conjoined valves; Llandovery, mid-late Aeronian, Niur Formation, sample S14, Derenjal Mountains, Iran.

Paratypes. NMW 2011.11G.271-326, conjoined valves; NMW 2011.11G.270, 327, 328, ventral valves; NMW 2011.11G.329, 330, dorsal valves; sample S14, Derenjal Mountains. NMW 2011.11G.336-354, AEU 1368-1475, articulated shells; NMW 2011.11G.355, ventral valve, NMW 2011.11G.357, 358, dorsal valves, sample K29; Boghu Mountains. NMW 2011.11G.331-333, conjoined valves; NMW 2011.11G.334, ventral valve; NMW 2011.11G.335, dorsal valve; sample K30, Boghu Mountains. CNIGR 12600/126, 127 conjoined valves; loose sample, vicinity of Shabdjereh. Total 184 articulated shells, five ventral and five dorsal valves.

Diagnosis. Subequally biconvex transverse shell with maximum width slightly anterior to the hinge line or at the hinge line, about 50-60% as thick as long; with a strong ventral sulcus and dorsal median fold originating at the umbonal area and occupying about 40% of maximum shell width; radial ornament with a single rib in a sulcus, two ribs on a dorsal fold and 4-7 on valve flanks; ventral median rib of equal size with ribs on valve flanks; ventral beak erect; delthyrial plates merged anterior to the elongate, submesothyrid pedicle foramen.

[FIGURE 6 OMITTED]

Description. Shell subequally biconvex, transverse, semioval in outline, about 80% as long as wide with maximum width slightly anterior to the hinge line or at hinge line and 50-60% as thick as long. Hinge line relatively wide, almost straight; anterior commissure strongly sulciplicate. Ventral valve sagittal profile moderately convex with maximum height at midlength. Beak erect to gently curved. Delthyrial plates thick, conjunct anterior to the elongate, submesothyrid pedicle foramen. Sulcus deep and narrow, with steep lateral slopes, originating at the umbonal area and terminating with a trapezoidal tongue occupying about 40% of maximum shell width. Dorsal valve moderately convex with maximum height at midlength. Dorsal median fold high, originating at the umbonal area. Radial ornament of coarse angular ribs with a single rib in the ventral sulcus, two ribs on the dorsal median fold and 4-7 ribs on flanks of the dorsal valve. Rib in the sulcus about the same size as ribs on the valve flanks. Concentric ornament of fine crowded growth lamellae covering anterior half of the shell surface and with fine, evenly spaced fila in the posterior half of the shell of the mature specimens.

Ventral interior with strong, oblique teeth supported by the rudimentary dental plates mainly fused to the valve walls. Ventral muscle field strongly impressed with adductor scars completely enclosed by larger diductor scars. Strongly thickened pedicle callist mainly occupying a bottom of the small delthyrial cavity. Dorsal interior with massive united hinge plates and a small septalium supported by a very short median septum. Cardinal process septiform. Crura faint, radulifer, gently curved dorsolaterally.

Remarks. Stegocornu denisae sp. nov. in the Boghu section succeeds the type species Stegocornu procerum Durkoop in the stratigraphical sequence. It differs from the former in having a more dorso-laterally compressed shell (only 50-60% as thick as long against 75% in S. procerum), a narrow median fold and dorsal sulcus (on average 40% as wide as the shell against 50% in S. procerum) and an erect ventral beak. The median rib in the ventral sulcus in S. denisae is of about equal size to the ribs on the valve flanks, whereas in S. procerum it is considerably smaller. The number of ribs on the flanks overlaps significantly in both species, however, in S. procerum specimens with four ribs on flanks of the dorsal valve are the most common and the number of ribs does not exceed six, whereas in S. denisae specimens with 5-6 ribs are the most characteristic and shells with seven ribs do occasionally occur. Unlike S. procerum shells of S. denisae are transverse suboval, with maximum width slightly anterior of the hinge line or at the hinge line, and may be slightly alate.

Subfamily LEPIDOCYCLINAE Cooper, 1956

Genus Rhytidorhachis Jin & Caldwell, 1990

Type species. Rhytidorhachis hudsonensis Jin & Caldwell, 1990; Silurian, Llandovery, Ekwan River Formation, Hudson Bay Lowlands, Canada.

Rhytidorhachis? sp.

Figure 6A-D

Material. NMW 2011.11G.2 (Lv = 10.0, Ld = 8.0, W = 10.3, T = 5.7, Sw = 5.0), articulated shell, sample S14, Derenjal Mountains.

Description. Shell rostrate, subtriangular, subequally biconvex almost as long as wide; hinge line very narrow, curved. Anterior commissure uniplicate. Ventral valve with an erect, acuminate beak. Pedicle foramen large, submesothyridid. Delthyrium covered by thick deltidial plates merged distally. Ventral sulcus originating at the umbo, narrow and deep, with steep lateral slopes terminating in a semioval tongue. Dorsal valve evenly convex with a narrow fold originating at the umbo. Radial ornament with six subangular ribs on flanks. Ventral sulcus with a single costa in the umbonal area and a pair of smaller ribs intercalating at about midlength. Dorsal median fold with two costae bifurcating anteriorly. Concentric ornament of prominent, regular growth lamellae about 3 per 1 mm forming a characteristic zig-zag pattern on the rib crests. Interior of both valves unknown.

[FIGURE 7 OMITTED]

[FIGURE 8 OMITTED]

[FIGURE 9 OMITTED]

[FIGURE 10 OMITTED]

Remarks. Lack of data on the interior of both valves makes the generic affiliation of the specimen tentative. It is assigned provisionally to Rhytidorhachis because it has a rostrate shell with a delthyrium covered by thick medially conjunct deltidial plates and prominent concentric ornament. It differs from the type species R. hudsonensis Jin & Caldwell, 1990 from the Silurian, Llandovery, Ekwan River Formation of Hudson Bay Lowlands, Canada, in having a single rib in the ventral sulcus and two ribs on the dorsal fold posterior to midlength and coarse concentric growth lamellae. The Iranian shell differs from Rhytidorhachis diodonta (Dalman, 1828) from the Silurian Klintberg Beds (upper Wenlock-lower Ludlow) of Gotland in having finer radial ornament with up to six ribs on flanks and a pair of additional costellae originating in the ventral sulcus and a dorsal median fold anterior to midlength.

Genus Stegerhynchus Foerste, 1909

Type species. Rhynchonella (Stegerhynchus) whittiipraecursor (= Stegerhynchus praecursor) Foerste, 1909. Silurian, Llandovery, Aeronian. Clinton Beds, Clinton, Tennessee, USA.

Stegerhynchus? sp.

Figure 6K-M

Material. NMW 2011.11G.372 (Ld = 12.7, W = 13.7, T = 6.7, Sw = 7.6), articulated shell; sample S14, Derenjal Mountains.

Remarks. A single specimen from the Niur Formation of the Derenjal Mountains occurs in association with the shell referred to Hercotrema sp. It also has three ribs in the ventral sulcus, four ribs in the dorsal fold, but differs in having angular ribs, a subrectangular, not semioval tongue, a more strongly dorsibiconvex shell with a dorsal valve profile having maximum height close to the anterior margin. Without knowing the characters of the cardinalia the generic affiliation of this shell is uncertain, but it is more likely not congeneric with Hercotrema sp. from the same locality. In general shell shape and characters of radial ornament, the specimen resembles Stegerhynchus peneborealis (Twenhofel, 1928), as revised by Jin & Copper (2004), but differs in its slightly larger size and less transverse shell outline.

Family TRIGONIRCHYNCHIDAE Schmidt, 1965

Subfamily ROSTRICELLULINAE Rozman, 1969

Genus Hercotrema Jin, 1989

Type species. Hercotrema bulbicostatum Jin, 1989; Silurian, Llandovery, Jupiter Formation, Anticosti Island, Quebec, Canada.

Hercotrema sp.

Figure 6E-J

Material. NMW 2011.11G.3 (Lv = 9.0, Ld = 8.6, W = 10.7, T = 5.0, Sw = 5.7), 4, 5 (Lv = 12.9, Ld = 12.2, W = 13.3, T = 7.5, Sw = 7.2), articulated shells, sample S14, Derenjal Mountains.

Description. Shell slightly dorsibiconvex, subpentagonal in outline, slightly wider than long and about three fifths as high as long. Anterior commissure uniplicate. Ventral valve lateral profile moderately convex with maximum height at about one third valve length from the umbo. Delthyrium open, narrow, triangular. Ventral median sulcus originating at about 3-4 mm from the umbo, gently deepening anteriorly and terminating in a low, semioval tongue slightly wider than half the maximum shell width. Dorsal valve lateral profile moderately and unevenly convex with maximum height at about one third valve length from the anterior margin. Dorsal median fold low, evenly convex in transverse profile, originating slightly posteriorly to the midvalve. Radial ornament with simple rounded costae, with three ribs in the ventral sulcus, four ribs in the dorsal median fold and 5-6 ribs on flanks. Concentric ornament of very fine, evenly spaced fila.

Ventral interior with delicate teeth and thin, short dental plates. Dorsal interior with a short, narrow septalium supported by a short median septum. Cardinal process absent (Fig. 6H, I).

Remarks. The shells from the Niur Formation show strong simple ribs, a ventral sulcus and dorsal median fold originating at some distance from the beak, rudimentary dental plates and a small cruralium lacking a cardinal process, all suggesting affiliation to Hercotrema Jin, 1989. They differ from the type species Hercotrema bulbicostatum in having three ribs in the ventral sulcus and four ribs on the dorsal median fold.

Order SPIRIFERIDA Waagen, 1883

Suborder SPIRIFERIDINA Waagen, 1883

Superfamily CYRTIOIDEA Frederiks, 1924

Family CYRTIOIDAE Frederiks, 1924

Subfamily EOSPIRIFERINAE Schuchert, 1929

Genus Striispirifer Cooper & Muir-Wood, 1951

Type species. Delthyris niagarensis Conrad, 1842; Silurian, Wenlock, Niagara Group, Lockport, New York, USA.

Striispirifer? ocissimus sp. nov.

Figures 6R-T, 11

Derivation of name. After Latin ocissimus, appearing, occurring earliest.

Holotype. NMW 2011.11G.365 (Lv = 11.0, Ld = 9.2, T = 7.9, W = 15.2, Sw = 3.9), conjoined valves, Llandovery, mid-late Aeronian, Niur Formation, sample S14, Derenjal Mountains, Iran.

Material. NMW 2011.11G.359 (L = 15.5, W = 23.2, T = 14.2), conjoined valves; NMW 2011.11G.360 (L = 10.2, W = 14.0, Sw = 4.9), ventral valve; sample K30. NMW 2011.11G.361.1, 2, disarticulated conjoined valves; NMW 2011.11G.364 (Lv = 9.1, Ld = 7.9, T = 6.9, W = 12.1, Sw = 3.2), 366 (Lv = 9.2, Ld = 7.0, W = 11.5, T = 6.7, Sw = 3.4), 367 (Lv = 7.8, Ld = 6.1, T = 6.6, W = 11.6, Sw = 3.1), 368 (Lv = 7.3, Ld = 6.8, W = 15.2, T = 5.6), conjoined valves; NMW 2011.11G.363, 369, ventral valves; NMW 2011.11G.362, dorsal valve; sample S14, Derenjal Mountains. Total eight articulated shells, three ventral valves and one dorsal valve.

Diagnosis. Shell strongly ventribiconvex, transverse, subtrapezoidal and about three quarters as long as wide, with maximum width slightly anterior to the hinge line; cardinal extremities obtuse; ventral sulcus and dorsal median fold narrow, flattened, slightly more than one quarter as wide as the shell; dorsal median fold bisected by a fine groove; radial ornament of 5-7 plications on flanks and superimposed very fine striae, about 9-11 per 1 mm; dental plates sulcus-bounding, cardinal process smooth.

Description. Shell ventribiconvex, strongly transverse, subtrapezoidal in outline, about three quarters as long as wide, with maximum width slightly anterior to the hinge line, and about three quarters as thick as long. Cardinal extremities obtuse; anterior commissure uniplicate. Ventral valve lateral profile strongly convex with maximum height above the hinge line. Ventral interarea high, curved, apsacline with an open, narrow triangular delthyrium. Ventral sulcus narrow, strongly curved, originating at the umbo and terminating in a subtrapezoidal tongue about 25-30% valve width. Dorsal valve moderately and evenly convex with a low, anacline interarea and a narrow, flattened median fold originating at the umbo and often bisected by a fine groove. Radial ornament with 5-6 strong, rounded plications on the flanks of the dorsal valve and 6-7 plications on the flanks of the ventral valve, separated by broad, U-shaped interspaces. Microornament of very fine, striae about 10-12 per 1 mm. Concentric ornament of fine, evenly spaced fila.

[FIGURE 11 OMITTED]

Ventral interior with rounded, long, slightly divergent, sulcus-bounding dental plates. Dorsal interior with thin, short, slightly divergent crural plates, straight, short rod-like crura (Fig. 11O), and a smooth cardinal process.

Discussion. The Iranian shells are provisionally assigned to the genus, because they have broad, rounded in cross section interspaces between the ribs and a flattened dorsal median fold, unlike other species of Striispirifer (e.g. Boucot 1963; Rong et al. 1974; Rong & Yang 1978).

Rounded in cross section interspaces between the ribs are considered as diagnostic for Macropleura (Boucot 1963). However, Iranian shells differ from other species assigned to this genus in having sulcus-bounding, not distinctly extrasinal, dental plates and a relatively narrow dorsal median fold bisected by a faint groove. In addition, they differ from the type species Macropleura macropleura (Conrad, 1840) in having more plications (up to 7) on the lateral sides of the valves and a high, apsacline, not strongly curved ventral interarea.

doi: 10.3176/earth.2012.2.02

Acknowledgements. This paper benefited from conodont identifications and ages of the brachiopod-bearing horizons, provided by Peep Mannik (Tallinn University of Technology, Estonia) and C. Giles Miller (Natural History Museum, London). We are grateful to Koorosh Rashidi (Open University of Ardakan), Hasan Hejazi (Azad University of Khorasgan, Esfahan, Iran) and Amir Akbari (Esfahan) for assistance in fieldworks. VH acknowledges financial support from Islamic Azad University, Khorasgan Branch (project No. 51753871117003). The research of Mansoureh Ghobadi Pour was supported by Golestan University. Leonid Popov acknowledges logistical support from the National Museum of Wales. We are grateful to Arthur Boucot (University of Oregon) for valuable comments on the earlier version of the paper. Robin Cocks (Natural History Museum, London) and Rong Jia-Yu (Nanjing Institute of Geology and Palaeontology) provided helpful reviews of the manuscript.

REFERENCES

Alavi, M. 1991. Tectonic Map of the Middle East, Scale 1:5,000,000. Geological Survey of Iran, Tehran.

Alvarez, F. & Rong, J. Y. 2002. Order Athyridida. In Treatise on Invertebrate Paleontology. Part H, Brachiopoda (Revised) (Kaesler, R. L., ed.), pp. 1475-1614. Geological Society of America and the University of Kansas Press, Boulder and Lawrence.

Barrande, J. 1879. Systeme Silurien du centre de la Boheme. Premiere partie Recherches paleontologiques 5, Classe des Mollusques, Ordre des Brachiopodes. Published by the author, Paris, 226 pp.

Bassett, M. G. 1972. The articulate brachiopods from the Wenlock Series of the Welsh Borderland and South Wales, part 2. Monograph of the Palaeontographical Society, 126(532), 27-78.

Berberian, M. & King, G. C. P. 1981. Towards a paleogeography and tectonic evolution of Iran. Canadian Journal of Earth Science, 18, 210-265.

Boucot, A. J. 1963. The Eospiriferidae. Palaeontology, 5, 682-711.

Boucot, A. J. & Blodgett, R. B. 2001. Silurian-Devonian biogeography. In Brachiopods Past and Present (Brunton, C. H. C., Cocks, L. R. M. & Long, S. L., eds), pp. 335-344. Taylor and Francis, London.

Boucot, A. J., Johnson, J. G. & Walmsley, V. G. 1965. Revision of the Rhipidomellidae (Brachiopoda) and the affinities of Mendacella and Dalejina. Journal of Paleontology, 39, 331-340.

Brice, D. 1999. Middle(?) Silurian rhynchonellid and spiriferid brachiopod faunas from eastern central Iran. Annales de la Societe geologique du Nord, 7, 5-12.

Bruton, D. L., Wright, A. J. & Hamedi, M. A. 2004. Ordovician trilobites of Iran. Palaeontographica, A271, 111-149.

Carter, J. L., Johnson, J. G., Gourvennec, R. & Hou, H. 1994. A revised classification of the spiriferid brachiopods. Annals of the Carnegie Museum, 63, 327-374.

Caster, K. E. 1939. A Devonian fauna from Colombia. Bulletin of American Paleontology, 24(83), 1-218.

Cocks, L. R. M. 1967. Llandovery stropheodontids from the Welsh Borderland. Palaeontology, 10, 245-265.

Cocks, L. R. M. 1979. A silicified brachiopod fauna from the Silurian of Iran. Bulletin of the British Museum (Natural History), Geology, 32, 25-42.

Conrad, T. A. 1840. Third Annual Report, Palaeontological Department, Geological Survey of New York, Albany, 4, 199-207.

Conrad, T. A. 1842. Observations on the Silurian and Devonian Systems of the United States, with descriptions of new organic remains. Journal of the Academy of Natural Sciences of Philadelphia, 8(2), 228-280.

Cooper, G. A. 1956. Chazyan and related brachiopods. Smithsonian Miscellaneous Collections, 127, 1-1245.

Cooper, G. A. & Muir-Wood, H. M. 1951. Brachiopod homonyms. Journal of Washington Academy of Sciences, 41(6), 195-196.

Dalman, J. W. 1828. Uppstallning och Beskrifning af de i Sverige funne Terebratuliter. Kungliga Vetenskapsakademiens Handlingar, Stockholm, 1827, 85-155.

Durkoop, A. 1970. Brachiopoden aus dem Silur, Devon und Karbon in Afghanistan. Palaeontographica, Series A, 134, 153-225.

Foerste, A. F. 1909. Fossils from the Silurian formations of Tennessee, Indiana and Kentucky. Bulletin of the Denison University Scientific Laboratory, 14, 61-116.

Flugel, H. W. & Saleh, H. 1970. Die palaeozoischen Korallenfaunen Ost-Irans. 1. Rugose Korallen der Niur Formation (Silur). Jahrbuch der Geologischen Bundesanstalt, 113, 267-302.

Frederiks, G. N. 1924. Paleontologicheskie etyudy. 2. O verkhnekamenougol'nykh spiriferidakh Urala [Paleontological studies. 2. On Upper Carboniferous spiriferids from the Urals]. Izvestiya Geologicheskogo Komiteta, 38(3), 295-324. (Volume 38 for 1919 was published in 1924) [in Russian].

Ghobadi Pour, M., Williams, M., Vannier, J., Meidla, T. & Popov, L. E. 2006. Ordovician ostracods from east Central Iran. Acta Palaeontologica Polonica, 51, 551-560.

[GSI] Geological Survey of Iran. 2001a. Geological Map of Quadrangle Kashmar, 1 : 100 000. Geological Survey of Iran, Tehran.

[GSI] Geological Survey of Iran. 2001b. Geological Map of Quadrangle Robat-e-Qarehbil, 1 : 100 000. Geological Survey of Iran, Tehran.

Hairapetian, V., Blom, H. & Miller, C. G. 2008. Silurian thelodonts from the Niur Formation, central Iran. Acta Palaeontologica Polonica, 53, 85-95.

Hairapetian, V., Mohibullah, M., Tilley, L. J., Williams, M., Miller, C. G., Afzal, J., Ghobadi Pour, M. & Hejazi, S. H. 2011. Early Silurian carbonate platform ostracods from Iran: a peri-Gondwanan fauna with strong Laurentian affinities. Gondwana Research, 20, 645-653.

Harper, D. & Boucot, A. 1978. The Stropheodontacea, Part I (Leptostrophiidae, Eostropheodontidae, and Strophonellidae). Palaeontographica, Series A, 161, 55-118.

Havlicek, V. 1953. O nekolika novych ramenonozcich ceskeho a moravskeho stfedniho devonu [On some new brachiopods of the Czech and Moravian Middle Devonian]. Vestnik Ustfedniho Ustavu Geologickeho, 28, 4-9 [in Czech].

Jin, J. 1989. Late Ordovician-Early Silurian rhynchonellid brachiopods from Anticosti Island, Quebec. Biostratigraphie du Paleozoique, 10, 1-127.

Jin, J. & Caldwell, G. E. 1990. Rhytidorhachis, a new Silurian rhynchonellid brachiopod from Gotland, Sweden and Hudson Bay Lowlands, Canada. Institut Royal des Sciences Naturelles de Belgique, Bulletin (Sciences de la Terre), 60, 29-41.

Jin, J. & Copper, P. 2004. Evolution of the Early Silurian rhynchonellid brachiopod Stegerhynchus, Anticosti Island, eastern Canada. Journal of Paleontology, 78, 866-883.

King, W. 1846. Remarks on certain genera belonging to the class Palliobranchiata. Annals and Magazine of Natural History (Series 1), 18(117), 26-42, 83-94.

Kuhn, O. 1949. Lehrbuch der Palaozoologie. E. Schweizer bartsche Verlagsbuchhandlung, Stuttgart, 326 pp.

Kozlowski, R. 1929. Les brachiopodes gotlandiens de la Podolie polonaise. Palaeontologia Polonica, 1, I-XIII+1-254.

Laurie, J. R. 1991. Articulate brachiopods from the Ordovician and Lower Silurian of Tasmania. Memoir of the Association of Australasian Palaeontologists, 11, 1-106.

Li, R. & Copper, P. 2006. Early Silurian (Llandovery) orthide brachiopods from Anticosti Island, eastern Canada: the O/S extinction recovery fauna. Special Papers in Palaeontology, 76, 1-71.

Lindenberg, H. G., Groler, K., Jacobshagen, V. & Ibbeken, H. 1984. Post-Paleozoic stratigraphy, structure and orogenetic evolution of the southern Sabzevar zone and the Taknar block. Neues Jahrbuch fur Geologie und Palaontologie, Abhandlungen, 168, 287-326.

Mannik, P. 1994. Conodonts from the Pusku Quarry, lower Llandovery, Estonia. Proceedings of the Estonian Academy of Sciences, Geology, 43, 183-191.

Moore, R. C. 1952. Brachiopods. In Invertebrate Fossils (Moore, R. C., Lalicker, C. G. & Fischer, A. G., eds), pp. 197-267. McGraw-Hill. New York.

Opik, A. 1934. Uber Klitamboniten. Acta and Commentationes Universitatis Tartuensis (Dorpatensis), Series A, 26(5), 4-239.

Paeckelman, W. & Sieverts, H. 1932. Obersilurische und devonische Faunen der Prinzeninseln, Bithyniens und Thraziens. Abhandlungen der Preussischen Geologischen Landesanstalt, Berlin (New Series), 142, 1-79.

Ramezani, J. & Tucker, R. D. 2003. The Saghand region, central Iran: U-Pb geochronology, petrogenesis and implications for Gondwana tectonics. American Journal of Science, 303, 622-665.

Rozman, Kh. S. 1969. Pozdneordovikskie brakhiopody Sibirskoj platformy [Late Ordovician brachiopods of the Siberian Platform]. Paleontologicheskij Zhurnal, 1969(3), 86-108.

Rong, J. & Yang, X. 1978. Silurian spiriferoids from southwest China with special reference to their stratigraphical significance. Acta Palaeontologica Sinica, 17, 357-386 [in Chinese, with English summary].

Rong, J., Xu, H. & Yang, X. 1974. Brachiopoda (Silurian). In A Handbook of the Stratigraphy and Palaeontology in Southwest China, pp. 195-208, pls 92-96. Science Press, Beijing.

Rubel, M. 1963. Silurian orthide brachiopods of Estonia. Eesti NSV Teaduste Akadeemia Geoloogia Instituudi Uurimused, 13, 109-160 [in Russian, with English summary].

Ruttner, A., Nabavi, M. & Hajian, J. 1968. Geology of the Shirgesht area (Tabas area, East Iran). Reports of the Geological Survey of Iran, 4, 1-133.

Rzhonsnitskaya, M. A. 1956. Nadsemeistvo Pentameracea M'Coy, 1844. In Materialy po paleontologii, novye semeistva i rody [Palaeontological Material, New Families and Genera] (Kiparisova, L. D., Markovskij, B. P. & Radchenko, G. P., eds), Trudy Vsesoyuznogo Nauchno-Issledovatel'skogo Geologicheskogo Instituta (VSEGEI) (New Series), 12, 49-50 [in Russian].

Savage, N. M., Mancenido, M. O., Owen, E. F., Carlson, S. J., Grant, R. E., Dagys, A. S. & Sun, D. 2002. Rhynchonellida. In Treatise on Invertebrate Paleontology, Part H, Brachiopoda, (Revised), 4, Rhynchonelliformea (Part) (Kaesler, R. L., ed.), pp. 1027-1376. Geological Society of America, Denver and University of Kansas Press, Lawrence.

Schmidt, H. 1965. Paleozoic Rhynchonellacea [part]. In Treatise on Invertebrate Paleontology. Part H, Brachiopoda (Moore, R. C., ed.), pp. 552-597. Geological Society of America & University of Kansas Press, New York & Lawrence.

Schuchert, C. 1913. Class 2. Brachiopoda. In Text-book of Palaeontology, Vol. 1, Part 1, 2nd Ed. (von Zittel, K. A., translated and edited by Eastman, C. R.), pp. 355-420, figs 526-636. MacMillan & Co., Ltd. London.

Schuchert, C. 1929. Classification of brachiopod genera, fossil and recent. In Brachiopoda (Generum et Genotyporum Index et Bibliographia) (Schuchert, C. & LeVene, C. M.), Fossilium Catalogus I: Animalia, 42, 10-25. W. Junk, Berlin.

Schuchert, C. & Cooper, G. A. 1931. Synopsis of the brachiopod genera of the suborders Orthoidea and Pentameroidea, with notes on the Telotremata. American Journal of Science (Series 5), 22, 241-255.

Schuchert, C. & Cooper, G. A. 1932. Brachiopod genera of the suborders Orthoidea and Pentameroidea. Memoirs of the Peabody Museum of Natural History, 4(1), 1-270.

Sowerby, J. de C. 1839. Mollusca and Conchifers. In The Silurian System, Part 2. Organic remains (Murchison, R. I.), pp. 577-768. John Murray, London.

Sowerby, J. de C. 1840-1846. The Mineral Conchology of Great Britain, Vol. 7. Published by the author, London, 80 pp.

Strusz, D. L. 2002. Brachiopods of the Orders Protorthida and Orthida from the Silurian of the Yass Syncline, southern New South Wales. Alcheringa, 26, 49-86.

Twenhofel, W. H. 1928. Geology of Anticosti Island. Geological Survey of Canada, Memoir, 154, 1-351.

Waagen, W. H. 1883. Salt-Range fossils, vol. I, Part 4, Productus Limestone fossils, Brachiopoda. Memoirs of the Geological Survey of India, Palaeontologia Indica (Series 13), fasc. 2, 391-546.

Walliser, O. H. 1964. Conodonten des Silurs. Abhandlungen des Hessischen Landesamtes fur Bodenforschung, 41, 1-106.

Walmsley, V. G. 1966. Silurian brachiopods and gastropods of southern New Brunswick. Geological Survey of Canada, Bulletin, 140, 1-45.

Walmsley, V. G. & Boucot, A. J. 1975. The phylogeny, taxonomy and biogeography of Silurian and Early to Mid Devonian Isorthinae (Brachiopoda). Palaeontographica, 148A, 34-108.

Williams, A. 1951. Llandovery brachiopods from Wales with special reference to the Llandovery district. Quarterly Journal of the Geological Society of London, 107, 85-136.

Williams, A. & Harper, D. A. T. 2000. Orthida. In Treatise on Invertebrate Paleontology, Volume H, Brachiopoda (Revised), 3 (Kaesler, R. L., ed.), pp. 714-782. Geological Society of America and University of Kansas Press, Boulder and Lawrence.

Zhang, N. 1989. Wenlockian (Silurian) brachiopods of the Cape Phillips Formation, Baillie Hamilton Island, Arctic Canada: Part I. Palaeontographica (Abt. A), 206, 46-97.

Vachik Hairapetian (a), Mansoureh Ghobadi Pour (b), Leonid E. Popov (c) and Tatiana L. Modzalevskaya (d)

(a) Department of Geology, Khorasgan (Isfahan) Branch, Islamic Azad University, PO Box 81595-158, Isfahan, Iran; vacMk@khuisf.ac.ir

(b) Department of Geology, Faculty of Sciences, Golestan University, Gorgan 49138-15739, Iran; mghobadipour@yahoo.co.uk, m.ghobadipour@gu.ac.ir

(c) Department of Geology, National Museum of Wales, Cathays Park, Cardiff CF10 3NP, United Kingdom; leonid.popov@museumwales.ac.uk

(d) Department of Stratigraphy and Palaeontology, Russian Geological Research Institute (VSEGEI), 74 Sredniy prospect, 199106 St. Petersburg, Russia; Tatiana_Modzalevskaya@vsegei.ru

Received 18 October 2011, accepted 13 December 2011
Table 1. Basic statistics of 20 ventral valves of Isorthis
(Ovalella) inflata sp. nov.; Llandovery, mid-late Aeronian, Niur
Formation, sample S14, Derenjal Mountains

S14         Lv         W        Iw         T        Ml

N           20        19        17        19        15
X           8.4       10        8.2      3.18       4.8
S          1.61      1.84      1.73       0.8      0.91
Min         5.5       6.7       5.6       2.0       3.7
Max        11.9      14.8      12.2       5.0       7.2

S14         Mw       Lv/W      Iw/W      T/Lv      Ml/Lv

N           15        19        17        19        15
X           3.1      85.3%     81.8%     37.2%     55.6%
S          0.79       3.8       6.1       2.5       4.5
Min         1.8      76.6%     71.4%     31.9%     48.8%
Max         5.2      91.7%     95.1%     42.0%     66.7%

Table 2. Basic statistics of 21 dorsal valves of Isorthis
(Ovalella) inflata sp. nov.; Llandovery, mid-late Aeronian, Niur
Formation, sample S14, Derenjal Mountains

S14       Ld         W          Iw         T          Ml

N         21         21         18         17         16
X        9.0        10.7       9.5        2.9        4.9
S        1.67       1.58       1.26       0.66       1.00
Min      6.0        7.6        7.4        1.9        3.4
Max      12.6       13.9       12.3       4.2        7.0

S14       Mw        Lv/W       Ld/W       T/Lv      Ml/Lv

N         15         21         18         17         16
X        3.7       83.6%      87.0%      30.9%      56.0%
S        0.85       5.7        5.6        4.4        5.1
Min      2.4       73.9%      74.7%      21.8%      43.5%
Max      5.8       94.4%      93.7%      41.3%      64.1%

Table 3. Basic statistics of 24 shells of Stegocornu procerum
Durkoop, 1970; Llandovery, mid-late Aeronian, Niur Formation,
sample K28, Boghu Mountains

K28         Lv          Ld           W           T          Sw

N           24          24          24          24          22
X          14.0        12.7        17.7        10.4         8.8
S          0.87        0.85        0.97        1.13        0.95
Min        12.8         11         15.8         7.5         7.2
Max        16.5        14.1        19.2         12         10.5

K28         St         Lv/W        Ld/W        T/Lv        Sw/W

N           18          18          18          18          18
X           7.9        79.3%       71.9%       74.2%       50.0%
S          1.21         5.6         4.7         7.1        5.0%
Min         5.9        70.3%       64.8%       58.6%       41.0%
Max         9.9        89.0%       84.1%       85.8%       59.1%

Table 4. Basic statistics of 10 shells of Stegocornu denisae sp.
nov.; Llandovery, mid-late Aeronian, Niur Formation, sample K29,
Boghu Mountains

K29        Lv          Ld           W           T          Sw

N          10          10          10          10          10
X         15.3        14.3        20.6         9.3         8.3
S         1.49        1.36        2.33        1.79        1.30
Min       12.7        11.8         17          6.3         6.4
Max       17.4        16.2        24.2        12.5         9.7

K29        St         Lv/W        Ld/W        T/Lv        Sw/W

N           9          10          10          10          10
X          5.9        74.6%       69.9%       60.2%       40.3%
S         1.23         5.8         6.4         7.6         4.3
Min        4.5        67.4%       60.5%       49.6%       35.2%
Max        8.1        82.9%       81.8%       75.3%       49.2%

Table 5. Basic statistics of 28 shells of Stegocornu denisae sp.
nov.; Llandovery, mid-late Aeronian, Niur Formation, sample S14,
Derenjal Mountains

S14        Lv          Ld           W           T          Sw

N          28          28          29          29          26
X         11.1         9.9        14.2         5.5         5.8
S         1.88        1.66        2.60        1.15        1.23
Min        7.7         7.0         9.7         3.2         3.8
Max       15.9        14.2        20.2         7.9         8.8

S14        St         Lv/W        Ld/W        T/Lv        Sw/W

N          26          28          28          28          26
X          4.1        79.4%       69.8%       49.7%       41.3%
S         1.55         8.3         5.7         7.7         7.2
Min        2.2        67.8%       59.2%       39.8%       22.8%
Max        8.9       100.0%       77.9%       60.0%       53.1%
COPYRIGHT 2012 Estonian Academy Publishers
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 2012 Gale, Cengage Learning. All rights reserved.

Article Details
Printer friendly Cite/link Email Feedback
Author:Hairapetian, Vachik; Pour, Mansoureh Ghobadi; Popov, Leonid E.; Modzalevskaya, Tatiana L.
Publication:Estonian Journal of Earth Sciences
Article Type:Report
Geographic Code:7IRAN
Date:Jun 1, 2012
Words:9076
Previous Article:Hirnantia sagittifera (Brachiopoda) and Mucronaspis mucronata s.l. (Trilobita) in the Upper Ordovician of the East Baltic: taxonomy and...
Next Article:Anniversaries provoke interest in lessons gained from history.
Topics:

Terms of use | Copyright © 2018 Farlex, Inc. | Feedback | For webmasters