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首页> 外文期刊>Palaontologische Zeitschrift >Chondrichthyans from the Lower Clayton Limestone Unit of the Midway Group (Paleocene) near Malvern, Arkansas, USA, with comments on the K/Pg boundary
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Chondrichthyans from the Lower Clayton Limestone Unit of the Midway Group (Paleocene) near Malvern, Arkansas, USA, with comments on the K/Pg boundary

机译:来自Marvern,Arkansas,Arkansas,Arkansas,Arkansas的Marvern Group(古代)下克莱顿石灰岩单位的Chondrichthyans。关于K / PG边界的评论

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摘要

The Lower Clayton Limestone Unit (LCLU) of the Midway Group (Paleocene) near Malvern, Arkansas, USA contains an assemblage of chondrichthyans recently exposed by excavation for highway stabilization. Chondrichthyan teeth in this assemblage belong to at least 12 taxa including:Ginglymostoma subafricanum,Carchariascf.whitei,Carchariassp.,Odontaspis winkleri,Palaeohypotodus rutori,Palaeogaleus vincenti,Dasyatiscf.hexagonalis,Dasyatissp.,Hypolophitessp.,Myliobatissp.,Rhinopterasp., and an indeterminate chimaerid. Locally, these chondrichthyans occur within a stratigraphic section directly above the Cretaceous-Paleogene (K/Pg) boundary that also contains chondrichthyans. This occurrence is uncommon in the global fossil record and provides an opportunity to (1) assess chondrichthyan diversity across the K/Pg boundary in the Malvern region and Gulf Coastal Plain of southwestern Arkansas and (2) evaluate the timing of marginal to shallow marine chondrichthyan faunal turnover and extinction at a proximal location approximate to 1500 km from the Chicxulub, Mexico, K/Pg impact site. Observed patterns within this K/Pg stratigraphic section indicate that changes in chondrichthyan assemblages are primarily the result of sea-level cyclicity and habitat losses that occurred across several million years.
机译:美国阿肯色州阿肯色州马尔恩(古)附近的中间克莱顿石灰岩单位(LCLU)靠近Malvern,含有最近通过挖掘公路稳定而暴露的软骨中的组合。在此组合Chondrichthyan齿属于至少12类群包括:Ginglymostoma subafricanum,Carchariascf.whitei,Carchariassp,Odontaspis winkleri,Palaeohypotodus rut​​ori,Palaeogaleus文森蒂,Dasyatiscf.hexagonalis,Dasyatissp,Hypolophitessp,Myliobatissp,Rhinopterasp和。。。不确定chimaerid。在本地,这些软骨中的本地在白垩纪古二烯(K / PG)边界上方的地层部分内发生,这也含有软骨辛基yans。在全球化石记录中,这一事件罕见,并为(1)提供了一次评估Malvern地区的K / PG边界的软骨丘脑多样性,并在西南部的西南部和(2)评估边缘到浅海池塘的时机近距离营业额和濒临灭绝,距离Chicxulub,墨西哥,K / PG撞击部位有近1500公里。该K / PG地层部分内观察到的模式表明,Chondrichthyan集会的变化主要是海平循环性和栖息地损失,在数百万年内发生。

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