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来自俄罗斯欧洲部分的海鳄形超目鳄形类,以及对中真鳄齿龙科牙齿锯齿进化及其古纬度分布的新认识。

Thalattosuchian crocodylomorphs from European Russia, and new insights into metriorhynchid tooth serration evolution and their palaeolatitudinal distribution.

机构信息

School of GeoSciences, University of Edinburgh, Edinburgh, United Kingdom.

LWL-Museum für Naturkunde, Münster, Germany.

出版信息

PeerJ. 2023 Aug 11;11:e15781. doi: 10.7717/peerj.15781. eCollection 2023.

DOI:10.7717/peerj.15781
PMID:37583913
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10424675/
Abstract

From the Middle Jurassic to the Early Cretaceous, metriorhynchid crocodylomorphs inhabited marine ecosystems across the European archipelago. Unfortunately, European metriorhynchids are only well known from Germany, France, and the UK, with the Eastern European fossil record being especially poor. This hinders our understanding of metriorhynchid biodiversity across these continuous seaways, and our ability to investigate provincialism. Here we describe eleven isolated tooth crowns and six vertebrae referable to Metriorhynchidae from the Callovian, Oxfordian, Volgian (Tithonian), and Ryazanian (Berriasian) or Valanginian of European Russia. We also describe an indeterminate thalattosuchian tooth from the lower Bajocian of the Volgograd Oblast, the first discovery of a marine reptile from the Bajocian strata of European Russia. These rare fossils, along with previous reports of Russian thalattosuchians, indicate that thalattosuchians have been common in the Middle Russian Sea since it was formed. Palaeolatitude calculations for worldwide metriorhynchid-bearing localities demonstrate that the occurrences in European Russia are the most northern, located mainly between 44-50 degrees north. However, metriorhynchids appear to be rare at these palaeolatitudes, and are absent from palaeolatitudes higher than 50°. These observations support the hypothesis that metriorhynchids evolved an elevated metabolism but were not endo-homeothermic, especially as endo-homeothermic marine reptiles (ichthyosaurs and plesiosaurs) remained abundant at much higher palaeolatitudes.

摘要

从中侏罗世到早白垩世,短吻鳄形类鳄形超目动物栖息在整个欧洲群岛的海洋生态系统中。不幸的是,欧洲的短吻鳄形类动物仅在德国、法国和英国有很好的记录,东欧的化石记录尤其匮乏。这阻碍了我们对这些连续海峡中短吻鳄形类动物生物多样性的理解,也阻碍了我们对地方特有性进行调查的能力。在这里,我们描述了来自俄罗斯欧洲部分的中侏罗统、牛津统、沃尔冈统(白垩纪)和里阿斯统(贝里亚期)或凡蓝今统的 11 颗孤立的牙冠和 6 节脊椎,这些都可归入短吻鳄科。我们还描述了来自伏尔加格勒州下白垩统的一个未定的海生鳄类牙齿,这是在俄罗斯欧洲部分的白垩纪地层中首次发现海洋爬行动物。这些罕见的化石,以及以前对俄罗斯海生鳄类的报道,表明自从形成以来,中俄罗斯海就一直有海生鳄类存在。对全世界有短吻鳄类化石的地点的古纬度计算表明,俄罗斯欧洲部分的短吻鳄类化石的地理位置最北,主要位于北纬 44-50 度之间。然而,在这些古纬度上,短吻鳄类似乎非常稀少,并且在古纬度高于 50 度的地方没有发现。这些观察结果支持了这样一种假说,即短吻鳄类进化出了较高的新陈代谢,但不是内温动物,尤其是因为内温海洋爬行动物(鱼龙和蛇颈龙)在更高的古纬度上仍然大量存在。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/fd40af1588d5/peerj-11-15781-g012.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/2e9473a970b9/peerj-11-15781-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/93ec7ade2804/peerj-11-15781-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/118c821c1759/peerj-11-15781-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/8bcd66b855f0/peerj-11-15781-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/77dd57ba0899/peerj-11-15781-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/8c7547e217ac/peerj-11-15781-g010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/4b7524931a09/peerj-11-15781-g011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/fd40af1588d5/peerj-11-15781-g012.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/91aa42a5d34c/peerj-11-15781-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/450b36a58fb8/peerj-11-15781-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/3dfa7d7fa558/peerj-11-15781-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/0510e3db3643/peerj-11-15781-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/2e9473a970b9/peerj-11-15781-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/93ec7ade2804/peerj-11-15781-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/118c821c1759/peerj-11-15781-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/8bcd66b855f0/peerj-11-15781-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/77dd57ba0899/peerj-11-15781-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/8c7547e217ac/peerj-11-15781-g010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/4b7524931a09/peerj-11-15781-g011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/07e9/10424675/fd40af1588d5/peerj-11-15781-g012.jpg

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