Overview of Mesozoic crocodylomorphs from the Junggar Basin, Xinjiang, Northwest China, and description of isolated crocodyliform teeth from the Late ... View Full Text


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Article Info

DATE

2010-09

AUTHORS

Oliver Wings, Daniela Schwarz-Wings, Hans-Ulrich Pfretzschner, Thomas Martin

ABSTRACT

Lacustrine and fluvial Jurassic and Cretaceous sediments in the Junggar Basin yielded at least five crocodylomorph taxa. The Middle and Late Jurassic Shishugou Formation has produced the crocodylomorph Junggarsuchus sloani, the holotype specimen of the middle-sized, amphibious goniopholidid Sunosuchus junggarensis, and remains of the shartegosuchid crocodyliform Nominosuchus matutinus. The contemporary Qigu Formation has also yielded Sunosuchus. Two crocodyliforms have been reported based on cranial and postcranial material from the Early Cretaceous Tugulu Group. The cranial material has been assigned to Edentosuchus tienshanensis, representing the geologically youngest protosuchid. In recent years, screenwashing at the Liuhuanggou locality, 40 km southwest of the city of Urumqi, has yielded a large number of isolated crocodyliform teeth in a highly fossiliferous bonebed within the Late Jurassic Qigu Formation. At least three different tooth morphologies can be distinguished at Liuhuanggou, indicating a shartegosuchid, juveniles cf. Sunosuchus and an unidentified mesoeucrocodylian. Thus, the variety in crocodyliforms known from this region is increased. The faunal composition comprises a mix of basal and derived crocodyliforms similar to that of the upper part of the Shishugou Formation and differs from contemporary European and many North American deposits. Hence, crocodyliform diversity in the Junggar Basin comprises at least two different size classes in the Junggar ecosystem: whereas the most frequently found taxon, Sunosuchus, was a larger (3 m) amphibious mesoeucrocodylian, the other taxa were smaller (<1.5 m long) and possibly more terrestrial faunal components. The combination of phylogenetically different crocodylomorphs and different ecotypes may reflect climate changes and hints towards the presence of relict faunas. More... »

PAGES

283-294

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s12549-010-0033-1

DOI

http://dx.doi.org/10.1007/s12549-010-0033-1

DIMENSIONS

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51 schema:description Lacustrine and fluvial Jurassic and Cretaceous sediments in the Junggar Basin yielded at least five crocodylomorph taxa. The Middle and Late Jurassic Shishugou Formation has produced the crocodylomorph Junggarsuchus sloani, the holotype specimen of the middle-sized, amphibious goniopholidid Sunosuchus junggarensis, and remains of the shartegosuchid crocodyliform Nominosuchus matutinus. The contemporary Qigu Formation has also yielded Sunosuchus. Two crocodyliforms have been reported based on cranial and postcranial material from the Early Cretaceous Tugulu Group. The cranial material has been assigned to Edentosuchus tienshanensis, representing the geologically youngest protosuchid. In recent years, screenwashing at the Liuhuanggou locality, 40 km southwest of the city of Urumqi, has yielded a large number of isolated crocodyliform teeth in a highly fossiliferous bonebed within the Late Jurassic Qigu Formation. At least three different tooth morphologies can be distinguished at Liuhuanggou, indicating a shartegosuchid, juveniles cf. Sunosuchus and an unidentified mesoeucrocodylian. Thus, the variety in crocodyliforms known from this region is increased. The faunal composition comprises a mix of basal and derived crocodyliforms similar to that of the upper part of the Shishugou Formation and differs from contemporary European and many North American deposits. Hence, crocodyliform diversity in the Junggar Basin comprises at least two different size classes in the Junggar ecosystem: whereas the most frequently found taxon, Sunosuchus, was a larger (3 m) amphibious mesoeucrocodylian, the other taxa were smaller (<1.5 m long) and possibly more terrestrial faunal components. The combination of phylogenetically different crocodylomorphs and different ecotypes may reflect climate changes and hints towards the presence of relict faunas.
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