A new species of the antiarch Microbrachius from the Middle Devonian (Givetian) of Belarus.
The original draft manuscript of this paper was written in the late 1980s by Elga Mark-Kurik. In their original form, two species of Microbrachius were erected by Mark-Kurik, one from Estonia and one from Belarus. At the time of the original draft only two species were known, the type species Microbrachius dicki Traquair, 1888 and a Chinese species Microbrachius sinensis Pan, 1984. For various reasons the manuscript was put on hold whilst Mark-Kurik pursued other projects. This article deals with one half of the original manuscript (the other half will be dealt with at a later date) and describes the Belarusian species Microbrachius kedoae n. sp. This species comes from a core from a single locality in southern Belarus (Fig 1).
HISTORY OF RESEARCH OF MICROBRACHIUS
Microbrachius is a small antiarch genus first discovered in the Middle Devonian (Givetian) Orcadian Basin of Scotland. Specimens of Microbrachius were first mentioned as a possible, new, small species of Pterichthys (now known as Pterichthyodes) by Peach (1868). He expressed that if the specimens did turn out to be new, they should be named after his friend, the fossil collector Robert Dick. It took over 20 years before Traquair (1888) published a short description (without figures) of the type species Microbrachius dicki. Later, Traquair (1904; the relevant part published in Traquair 1894-1914) figured some specimens and provided a fuller description of the species. Watson (1935) provided the first restoration in a very brief description. The first detailed description, including the individual dermal plates, was made by Hemmings (1978).
Two Chinese species have also been described. Microbrachius sinensis is dated as Eifelian, Middle Devonian and Microbrachius chuandongensis Wang & Zhang, 1999 is dated as Emsian, Early Devonian (see the discussion for more comments on these species). There are also specimens of Microbrachius found at the Essi muur (alias Essi Farm) locality in Estonia (Long et al. 2015). This species is currently under detailed investigation by the authors and others and will not be alluded to in this paper. All the specimens described in this paper are housed in the Department of Geology, Tallinn University of Technology, Estonia (GIT).
From the earliest descriptions of Microbrachius it was known that it was an antiarch although a more precise understanding of its phylogeny was not possible until the detailed description of the dermal armour was made by Hemmings (1978). Hemmings (1978) considered Microbrachius a bothriolepidoid belonging in its own family the Microbrachiidae Gross, 1965. This view was tested and confirmed by Luksevics (2001, fig. 82) in a phylogenetic analysis modified after Young (1988). More recently, the phylogeny of Microbrachius dicki has come under close scrutiny due to the discovery of male claspers (Long et al. 2015). Long et al. (2015) described Microbrachius as a small bothriolepid antiarch. Qiao et al. (2016) placed Microbrachius next to Bothriolepis in their cladistic analysis, thereby confirming the above opinions.
Suborder BOTHRIOLEPIDOIDEI Miles, 1968 Family MICROBRACHIDAE Gross, 1965 Genus Microbrachius Traquair, 1888
Type species. Microbrachius dicki Traquair, 1888.
Diagnosis (by Hemmings 1978; altered). Antiarch of small size. Head-shield relatively large and broader than it is long, between 40% and 45% of total dorsal length of dermal armour; postpineal plate drawn into pronounced point towards orbital fenestra; postpineal plate in contact with lateral plate. Dorsal wall of trunk-armour embayed anteriorly to accommodate head; tergal angle situated far forward; anterior median dorsal plate with breadth/length index between 100 and 128; pectoral articulation subcephalic; funnel pit of processes brachialis in anterior ventro-lateral very small; pars pedalis under angle to longitudinal body axis. Pectoral appendage with well-developed lateral and prominent mesial spines or enlarged denticles on both proximal and distal segments. Ornamentation of a combination of tuberculated ridges and tubercles.
Species composition. Microbrachius dicki Traquair, 1888, M. sinensis Pan, 1984, M. chuandongensis Wang & Zhang, 1999 and M. kedoae sp. n.
Microbrachius kedoae sp. n.
Etymology of name. After the late Belarus palynologist Dr Galina Kedo, Minsk.
Holotype. GIT 767-9, a right mixilateral plate housed at the Department of Geology, Tallinn University of Technology, Estonia.
Material. Left lateral plates preserved viscerally: GIT 767-2, GIT 767-3 and GIT 767-17. Right lateral plate preserved dorsally: GIT 767-11. Right paranuchal plate preserved dorsally: GIT 767-7. Anterior median dorsal plates preserved viscerally: GIT 767-4, GIT 767-5, GIT 767-6 and GIT 767-23. Posterior median dorsal plate preserved viscerally: GIT 767-8. Posterior median dorsal plate preserved dorsally: GIT 767-16. Left mixilateral plate preserved viscerally: GIT 767-9. Left mixilateral plate preserved dorsally: GIT 767-10. Right anterior ventro-lateral plates preserved viscerally: GIT 767-12 and GIT 767-14. Right posterior ventro-lateral plate preserved viscerally: GIT 767-1. Left posterior ventrolateral plate preserved viscerally: GIT 767-18. Proximal pectoral appendages: GIT 767-19 and GIT 767-20. Distil pectoral appendage: GIT 767-24. Fragment of an anterior ventro-lateral plate: GIT 767-15. Fragment of bone: GIT 767-25. Figure 2 indicates the known plates and their position on the body.
Occurrence. Type locality only: Gavrilchitsy 45 borehole near the village of Gavrilchitsy, southwest of Soligorsk in southern Belarus. Material collected at a depth of 225.25-228.95 m in the Moroch Beds of the Polotsk Regional Stage, Givetian, Middle Devonian.
Diagnosis. Breadth/length index of the anterior median dorsal plate 120-128; lateral plate very long and narrow; median dorsal plate with wide lateral angles; mixilateral plate overlapped by the anterior median dorsal plate; ornamentation of widely spaced linear ridges with finely tuberculated areas between them.
Head plates. The lateral plate is fairly long and thin, being broader at the anterior end. There is a fair amount of variation in the overall morphology of the plate and the length/breadth ratio varies between about two and three times as long. The mesial edge curves strongly round the orbital fenestra and this is further reflected in the convex lateral edge. The anterior edge is convex unless worn. GIT 767-11 (Fig. 3A, B) is the only specimen known preserved dorsally. A right L plate is somewhat worn, but the ornamentation is clear, consisting of tubercles and ridges, with the ridges being more prominent posteriorly and the tubercles more prominent anteriorly. There are also three known viscerally preserved specimens, all left L plates. GIT 767-2 (Fig. 3C, D), although damaged in places, is the most informative specimen and has a distinctive rod-like crenulated anterior margin. The mesial margin runs from the preorbital angle to the postorbital angle and is hollowed dorsally by the lateropremesial depression. This depression develops lateral into the lateropremesial ridge of the head-shield. Lateral to this ridge a premedian ridge is weakly developed. The antero-lateral angle of the otico-occipital depression of the head-shield is developed as a tapering hollow entering the posterior edge.
GIT 767-7 (Fig. 4) is a very small paranuchal plate preserved in dorsal view. The mesial length of the plate is longer than the lateral length. A very faint groove of the principle section of the infraorbital sensory line (ifc1) is visible. Ornamentation consists of some few tubercles with stellated bases and a number of pits. The specimen belongs probably to a juvenile.
Trunk plates. The anterior median dorsal plate is only known in visceral view (Fig. 5). The plate is short, broad and ovoid in shape, being wider than long with a breadth/length index of 120 to 128 (compared with a breadth/length index of 100 to 120 for Microbrachius dicki and around 100 for Microbrachius sinensis and Microbrachius chuandongensis). The posterior margin is straight or slightly convex, with a pronounced posterior median process. A fairly deep, anterior ventral pit occurs on a north/south axis in the middle of the plate. There are well developed lateral corners at the points the plate overlaps the anterior dorso-lateral and the mixilateral plates. The lateral corners are level with the posterior end of the anterior ventral pit or just posterior of it. The areas where the plate overlaps the mixilateral plates are short and quite narrow. The areas where the plate overlaps the anterior dorso-lateral plates are of a similar width posteriorly but then curve strongly to form an extended indentation following the course of the postlevator thickening. This thickening forms a thin ridge that runs to lateral edges. Anterior of the postlevator thickening is the levator fossa.
The posterior median dorsal plate is known in dorsal and visceral views (Fig. 6). GIT 767-8 (Fig. 6A, B) is the only known viscerally preserved specimen but only the anterior end is preserved. The plate overlaps the anterior median dorsal plate at the anterior margin and overlaps the mixilateral plates at the lateral margins. The anterior margin has an anterior corner midline and is delimited from the lateral margin by distinct anterolateral angles. Growth lines are also visible on this specimen. GIT 767-16 (Fig. 6C, D) is the only posterior median dorsal plate preserved dorsally, but it is from a very small individual, probably a juvenile. It is near complete, although missing some of the lateral edges which would suggest in life the plate was fairly short and broad, being broadest at the lateral corners, although the breadth/length index is uncertain. The lateral corners form distinct points around two thirds down the length of the plate but due to wear it is unclear if the very ends are preserved. The posterior border is broader than the anterior border. The dorsal median ridge formed of tubercles is very clear and reaches an apex at the posterior dorsal angle where it meets an indistinct lateral ridge. This lateral ridge is formed of tubercles that run anteriorly subparallel to the lateral corners, although as stated above, it is not clear if the true lateral corners are preserved. Normally it would be expected for this lateral ridge to run to the lateral corners. The anterior angle and the posterior angle are connected by the dorsal median ridge. Two posterior--anterior ridges running parallel to the dorsal median ridge are present on the left side, the right side being worn away. A wide sensory groove runs anterior of these ridges but it is not clear if it terminates at the posterior margin of the plate as in the type species.
The mixilateral is in general short and broad with an extended posterior border. Two right mixilateral plates are known. GIT 767-9 (Fig. 7A, B) is preserved viscerally, but as most of the bone is no longer present, it is an impression of the dorsal armour that is visible. GIT 767-10 (Fig. 7C, D) is preserved dorsally, but as all the bone is gone, an impression of the visceral surface is visible. The anterior border of the plate at its intersection with the dorso-lateral ridge produces a pronounced anterior corner. It passes dorsally and ventrally by rounded corners into the dorsal and lateral margins. The dorsal lamina is larger than the lateral lamina, with the mesial border being convex and the lateral border being some-what straighter. The posterior border is slightly convex, with the dorso-lateral ridge producing a pronounced corner where it meets the border. The mesial dorsal border of GIT 767-9 has narrow overlap areas for the anterior median dorsal and posterior median dorsal plates. There are larger overlap areas for the right anterior dorso-lateral and right anterior ventro-lateral plates on the anterior border of the plate. There is a very large overlap area on the lateral border for the right posterior ventro-lateral. This results in the mixilateral plate having quite a small area exposed on the dorsal surface of the fish. The main lateral line groove is seen as a groove running posterior to anterior on the lateral lamina of the plate. The ornamentation consists of long rows of anterior--posterior running tubercles. GIT 767-10 bears a well-developed, quite thick, crista transversalis interna posterior near the posterior border.
Only right anterior ventro-lateral plates in visceral aspect are known, with GIT 767-12 (Fig. 8A, B) being the best preserved. However, it is missing most of the posterior lateral edges and the antero-lateral corner. From what can be seen, the posterior margin of the plate is concave and extended to the ventro-lateral corner. Parallel to the antero-dorsal margin and in front of the crista transversalis interna anterior, a crista postbranchialis is developed. The foramen axillare is round and quite large, although it may be somewhat eroded. The plate overlaps the right posterior ventro-lateral plate at the posterior margin, but only a small part of this area is preserved. The plate also overlaps the right anterior dorso-lateral plate on the dorsal margin, but once again only a small part of this area is preserved.
Only right posterior ventro-lateral plates in ventral and visceral aspect are known. GIT 767-1 (Fig. 9A, B) is preserved in ventral view, but most of the bone is now missing, and so mostly a cast of the visceral surface is visible. This makes specific features difficult to discern. GIT 767-18 (Fig. 9C) is preserved in visceral view, but as all the bone is missing, a cast of the ventral surface is preserved. Also, the lateral part of the plate is mostly missing. However, between GIT 767-1 and GIT 767-18 a fairly complete restoration of the morphology of the dorsal surface of the plate is possible (Fig. 9D). The anterior and posterior portions are about the same length, with the posterior portion being about half as broad as the anterior portion. The lateral margin of the posterior portion continues anteriorly as the ventro-lateral ridge. This ridge continues to the area where the plate is overlapped by the right anterior ventro-lateral plate. This area stretches the entire breadth of the anterior border and is broadest where it meets the ventro-lateral ridge. The ornament consists of prominent tubercles arranged in ridges. Towards the anterior end they are fairly evenly spaced in an anterior--posterior direction. They become more convoluted where the left posterior ventro-lateral plate overlaps the plate before straightening up again. The left posterior ventro-lateral plate overlaps the plate midway along the length being longer than broad. At its broadest point a ridge runs laterally, similar to that seen in Pterichthyodes (Hemmings 1978, fig. 13A).
Two main components of the pectoral appendages are preserved, being the proximal and distal segments. The proximal segments are box-like and fairly long and slender. GIT 767-19 (Fig. 10A, B) has the socket exposed but it is badly eroded and so its original shape is hard to discern. The ornamentation consists of long rows of tubercles forming ridges. GIT 767-20 (Fig. 10C, E) shows this ornamentation quite well along with elongated pits. GIT 767-24 (Fig. 11) is the only distal segment known. The segment is very small and it is difficult to determine the ornamentation except at the edges. The lateral edge has fairly blunt, small tubercles. The mesial edge has large, fairly blunt, conical denticles.
Microbrachius kedoae compares well with the type species Microbrachius dicki which was described in detail by Hemmings (1978). Many of the dermal plates of M. dicki are quite variable and the dermal plates of M. kedoae fall into this variability for the most part. However, there are some striking morphological differences between the two species. The most obvious difference is that the mixilateral plate is overlapped by the anterior median dorsal plate in M. kedoae rather than the mixilateral plate overlapping the anterior median dorsal plate in M. dicki (see Hemmings 1978, fig. 30B, F). Also, the anterior ventro-lateral plate in M. kedoae has a crista postbranchialis developed unlike M. dicki. Another difference is the narrowness of the lateral plates in M. kedoae which are quite broad in M. dicki. Finally, another difference is that M. kedoae has denticles on the mesial edge of the distal segment of the pectoral appendage which are fairly blunt of the bothriolepid norm, whereas in M. dicki there are large, strongly recurved spines (Hemmings 1978). Long et al. (2015) speculated that these large spines allowed greater purchase in the internal fertilization process. How this relates to M. kedoae is uncertain.
Two Chinese Microbrachius species are also known. Microbrachius sinensis was erected on a limited number of isolated dermal plates. This species is found in the upper part of the Qujing Formation, near Qujing, Yunnan Province in southern China and is dated Late Eifelian (Pan 1984). It is therefore earlier than M. dicki and M. kedoae. Microbrachius kedoae differs from M. sinensis in that M. sinensis does not have well-developed lateral corners on the anterior median dorsal plate. Another difference is that the ornamentation of M. sinensis consists of tubercles fused into distinct lines without the isolated tubercles seen in M. kedoae. Also, a number of anterior median dorsal plates are known in M. sinensis, which show a fairly consistent breadth/length ratio of 100 which is considerably lower than in M. kedoae. Further detailed comparison of the diagnostic characters of M. kedoae with M. sinensis is hampered by the lack of material in M. sinensis. Unfortunately the anterior ventro-lateral plates in M. sinensis are not well enough preserved to show if a crista postbranchialis is developed or not. Also, there are no mixilateral plates, lateral plates or distal segments of the pectoral appendage known of M. sinensis.
The other Chinese species, Microbrachius chuandongensis was erected on articulated specimens that are not particularly well preserved. Microbrachius chuandongensis is found in the Chuandong Formation, near Qujing and is dated as Late Emsian, thus making it the oldest known Microbrachius species. It differs from M. kedoae in a number of important characters, including the mixilateral plate overlapping the anterior median dorsal plate rather than the other way round. Also, the anterior median dorsal plate does not have an anterior ventral pit as is the case in M. kedoae and the breadth/length ratio of this plate is around 100, so considerably less than in M. kedoae. The lateral plates are also much wider in M. chuandongensis than in M. kedoae. Other M. kedoae diagnostic characters we cannot compare with M. chuandongensis as viscerally preserved anterior ventro-lateral plates or distal segments of the pectoral appendages are unknown in the Chinese species. However, the most conspicuous character of M. chuandongensis is the very short posterior median dorsal plate which is much shorter and smaller than the anterior median dorsal plate. This also distinguished it from M. dicki and we have our doubts the species actually belongs in Microbrachius.
The Gavrilchitsy 45 core was taken by A. Fursenko in 1954 near the village of Gavrilchitsy southwest of the town of Soligorsk in southern Belarus. The M. kedoae remains were recovered from a single siltstone sample from a depth of 225.25 to 228.95 m along with unidentifiable osteolepid remains (D. Plax pers. comm. 2017). The siltstone is part of the Moroch Beds of the Polotsk Regional Stage (Plax 2008a, 2008b) which has recently been dated to the Givetian (Kruchek et al. 2010). This is significant as originally this part of the core was thought to be in the higher Lan Regional Stage. Mark-Kurik (2000, fig. 2) correlated the Moroch Beds with the Abava Member of the Burtnieki Formation in Estonia, which also contains remains of Microbrachius sp. (Long et al. 2015). The Abava Member has been correlated with the Eday Flagstone Formation of Scotland (Mark-Kurik & Poldvere 2012, fig. 3) where Microbrachius dicki is found. This means that Microbrachius could act as a zone fossil between Scotland, Estonia and Belarus.
Microbrachius kedoae is closely related to M. dicki with only a number of minor differences. The two Chinese species are morphologically quite different. The fact that Microbrachius is found at the same horizon in Scotland, Estonia and Belarus is highly significant for biostratigraphy. Also of note were Burrow et al. (2016) reporting the Orcadian Basin acanthodian, Diplacanthus crassisimus Duff 1842 in the Moroch Beds. However, by the Eday Flagstone Formation, acanthodians have become extinct in the Orcadian Basin. It is hoped that continued investigation of the Belarusian, Estonian and Scottish fauna will further refine the biostratigraphy between these areas.
Acknowledgements. We would like to thank Valentina Karatajute-Talimaa for allowing the senior author to study the Belarus collection and Dmitry Plax (Belarusian Research Geological Exploration Institute) for information and advice on the biostratigraphy of Belarus. We would also like to thank Gennadi Baranov (Department of Geology, Tallinn University of Technology) for photographic services and the digitalization of Elga Mark-Kurik's original drawings. Finally, we would also like to thank the two reviewers, John Long (Flinders University) and Dmitry Plax (Belarusian National Technical University) for insightful and useful comments that greatly improved the final version of this manuscript. This is a contribution to IGCP596: Climate change and biodiversity patterns in the mid-Palaeozoic (Early Devonian to Late Carboniferous). The publication costs of this article were covered by the Estonian Academy of Sciences.
Burrow, C. J., den Blaauwen, J. L., Newman, M. J. & Davidson, R. G. 2016. The diplacanthid fishes (Acanthodii, Diplacanthiformes, Diplacanthidae) from the Middle Devonian of Scotland. Palaeontologica Electronica, 19, 1-83.
Duff, P. 1842. Geology of Moray. Forsyth and Young, Elgin, 72 pp.
Gross, W. 1965. Uber die Placodermen-Gattungen Asterolepis und Tiaraspis aus dem Devon Belgiens und einen fraglichen Tiaraspis-rest aus dem Devon Spitzbergens. Institut Royal des Sciences Naturelles de Belgique, Bulletin, 41, 1-19.
Hemmings, S. K. 1978. The Old Red Sandstone antiarchs of Scotland: Pterichthyodes and Microbrachius. Palaeontographical Society Monographs, Publication, 131, 1-64.
Kruchek, S. A., Matveyev, A. V., Yakubovskaya, T. V., Naidenkov, I. V., Veretennikov, N. V., Obukhovskaya, T. G., Sanko, A. F. & Plax, D. P. (eds). 2010. Strati-graphic Charts of Precambrian and Phanerozoic Deposits of Belarus: Explanatory Notes. Belarusian Research Geological Exploration Institute, Minsk, 282 pp. [in Belarusian, with English introduction].
Long, J. A., Mark-Kurik, E., Johanson, Z., Lee, M. S. Y., Young, G. C., Zhu, M., Ahlberg, P. E., Newman, M., Jones, R., den Blaauwen, J., Choo, B. & Trinajstic, K. 2015. Copulation in antiarch placoderms and the origin of gnathostome internal fertilization. Nature, 517, 196-199.
Luksevics, E. 2001. Bothriolepid antiarchs (Vertebrata, Placodermi) from the Devonian of the north-western part of the East European Platform. Geodiversitas, 23, 489-609.
Mark-Kurik, E. 2000. The Middle Devonian fishes of the Baltic States (Estonia, Latvia) and Belarus. Courier Forschungsinstitut Senckenberg, 223, 309-324. Mark-Kurik, E. & Poldvere, A. 2012. Devonian stratigraphy in Estonia: current state and problems. Estonian Journal of Earth Sciences, 61, 33-47.
Miles, R. S. 1968. The Old Red Sandstone antiarchs of Scotland: Family Bothriolepididae. Palaeontographical Society Monographs, Publication, 122, 1-130.
Pan, J. 1984. A new species of Microbrachius from the Middle Devonian of Yunnan. Vertebrata PalAsiatica, 22, 8-13 [in Chinese, with English summary].
Peach, C. W. 1868. On fossil fishes of the Old Red Sandstone of Caithness and Sutherland, with notices of some new to those counties. Report of the Thirty-Seventh Meeting of the British Association for the Advancement of Science Held at Dundee in September 1867, Transaction of Sections, Geology, 72.
Plax, D. P. 2008a. Devonian fish fauna of Belarus. Lithosphere, 2(29), 66-92 [in Russian, with Belarusian and English summaries].
Plax, D. P. 2008b. Introduction of vertebrate zonal scales into the stratigraphic chart of Devonian deposits of Belarus. Reports of the National Academy of Sciences of Belarus, 52, 83-88 [in Belarusian, with English summary].
Qiao T., King, B., Long, J. A., Ahlberg, P. E. & Zhu, M. 2016. Early gnathostome phylogeny revisited: multiple method consensus. PLoS ONE, 11, 1-23.
Traquair, R. H. 1888. Notes on the nomenclature of the fishes of the Old Red Sandstone of Great Britain. Geological Magazine, 5, 507-517.
Traquair, R. H. 1894-1914. A monograph of the fishes of the Old Red Sandstone of Britain. Part 2. The Asterolepidae. Palaeontographical Society Monographs, 48, 63-134.
Wang, J.-Q. & Zang, G. R. 1999. New material of Microbrachius from Lower Devonian of Qujing, Yunnan,
China. Vertebrata PalAsiatica, 37, 200-211 [in Chinese, with English summary].
Watson, D. M. S. 1935. Fossil fishes of the Orcadian Old Red Sandstone. In The Geology of the Orkneys (Wilson, G. V., Edwards, W., Knox, J., Jones, R. C. B. & Stephens, S. J. V., eds), pp. 157-169. Memoirs of the Geological Survey, Scotland, HMSO, Edinburgh.
Young, G. C. 1988. Antiarchs (Placoderm fishes) from the Devonian Aztec Siltstone, Southern Victoria Land, Antarctica. Palaeontographica, 202(A), 1-125.
Antiarhi Microbrachius'e uus liik Valgevene Kesk-Devonist (Givet' lade)
Elga Mark-Kurik, Michael J. Newman, Ursula Toom ja Jan L. den Blaauwen
Antiarhi uus liik Microbrachius kedoae n. sp. on kirjeldatud Valgevene Kesk-Devonist (Givet' lade). Liik pohineb uksikutel nahaplaatidel, mis on leitud Gavriltsitso puursudamikust 25 km Soligorski linnast edelas. M. kedoae on hasti vorreldav selle perekonna tuupliigiga Microbrachius dicki Sotimaalt, kuid erineb nii sellest kui ka teistest perekonna Microbrachius'e liikidest erineva mixilateraalplaadi poolest. Viimane on kaetud anteriormediaan-dorsaalplaadiga, mille kulgedel on nurgad. Microbrachius'e samaaegne esinemine Sotimaal ja Valgevenes tugevdab arusaama, et nende piirkondade fauna oli Kesk-Devonis seotud.
Elga Mark-Kurik[dagger], Michael J. Newman (a), Ursula Toom (b) and Jan L. den Blaauwen (c)
(a) Vine Lodge, Vine Road, Johnston, Haverfordwest, Pembrokeshire, SA62 3NZ, UK; firstname.lastname@example.org
(b) Department of Geology, School of Science, Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; email@example.com
(c) University of Amsterdam, Science Park 904, 1098 XH, Amsterdam, Netherlands; J.L.denBlaauwen@uva.nl
Received 30 May 2017, accepted 12 August 2017, available online 19 December 2017
|Printer friendly Cite/link Email Feedback|
|Author:||Mark-Kurik, Elga; Newman, Michael J.; Toom, Ursula; den Blaauwen, Jan L.|
|Publication:||Estonian Journal of Earth Sciences|
|Date:||Mar 1, 2018|
|Previous Article:||Good traditions deserve to be continued and supported.|
|Next Article:||Elgaecrinus uralicus gen. et sp. nov., a new crotalocrinitid (Crinoidea, Echinodermata) from the Lower Devonian (Lochkovian) of the Middle Urals.|