Argyriou Thodoris, Davesne Donald
UMR 7207 (MNHN-Sorbonne Université-CNRS) Centre de Recherche en Paléontologie, Museum National d'Histoire naturelle, Paris, France.
Department of Earth Sciences, University of Oxford, Oxford, UK.
PeerJ. 2021 Jan 20;9:e10676. doi: 10.7717/peerj.10676. eCollection 2021.
The fossil record of marine ray-finned fishes (Actinopterygii) from the time interval surrounding the Cretaceous-Paleogene (K-Pg) extinction is scarce at a global scale, hampering our understanding of the impact, patterns and processes of extinction and recovery in the marine realm, and its role in the evolution of modern marine ichthyofaunas. Recent fieldwork in the K-Pg interval of the Pindos Unit in Eurytania, continental Greece, shed new light on forgotten fossil assemblages and allowed for the collection of a diverse, but fragmentary sample of actinopterygians from both late Maastrichtian and Paleocene rocks. Late Maastrichtian assemblages are dominated by Aulopiformes (†Ichthyotringidae, †Enchodontidae), while †Dercetidae (also Aulopiformes), elopomorphs and additional, unidentified teleosts form minor components. Paleocene fossils include a clupeid, a stomiiform and some unidentified teleost remains. This study expands the poor record of body fossils from this critical time interval, especially for smaller sized taxa, while providing a rare, paleogeographically constrained, qualitative glimpse of open-water Tethyan ecosystems from both before and after the extinction event. Faunal similarities between the Maastrichtian of Eurytania and older Late Cretaceous faunas reveal a higher taxonomic continuum in offshore actinopterygian faunas and ecosystems spanning the entire Late Cretaceous of the Tethys. At the same time, the scarcity of Paleocene findings offers tentative clues for a depauperate state of Tethyan ichthyofaunas in the aftermath of the K-Pg Extinction.
在全球范围内,白垩纪-古近纪(K-Pg)灭绝事件前后这段时间间隔内的海洋辐鳍鱼类(Actinopterygii)化石记录非常稀少,这妨碍了我们对海洋领域灭绝和复苏的影响、模式及过程,以及它在现代海洋鱼类区系演化中所起作用的理解。最近在希腊大陆欧里塔尼亚品都斯单元的K-Pg层段开展的野外工作,为被遗忘的化石组合带来了新的认识,并使得从晚马斯特里赫特阶和古新世岩石中采集到了多样但不完整的辐鳍鱼类样本。晚马斯特里赫特阶的组合以月鱼目(†艾氏鱼科、†内齿鱼科)为主,而†德氏鱼科(也属于月鱼目)、海鲢形目鱼类以及其他未鉴定的硬骨鱼类构成次要成分。古新世化石包括一种鲱科鱼类、一种巨口鱼目鱼类以及一些未鉴定的硬骨鱼类残骸。这项研究扩展了这一关键时间间隔内身体化石的匮乏记录,特别是对于较小体型的分类群,同时提供了一个罕见的、受古地理限制的、关于灭绝事件前后特提斯洋开放水域生态系统的定性概览。欧里塔尼亚马斯特里赫特阶与更古老的晚白垩世动物群之间的动物群相似性,揭示了横跨特提斯洋整个晚白垩世的近海辐鳍鱼类动物群和生态系统中更高的分类连续性。与此同时,古新世发现的稀少为K-Pg灭绝事件后特提斯洋鱼类区系的衰退状态提供了初步线索。