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首页> 外文期刊>Acta Palaeontologica Polonica >New protoceratopsid specimens improve the age correlation of the Upper Cretaceous Gobi Desert strata
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New protoceratopsid specimens improve the age correlation of the Upper Cretaceous Gobi Desert strata

机译:新的ProtoceraTapid标本改善了上白垩纪戈壁沙漠地层的年龄相关性

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摘要

New protoceratopsid (Dinosauria: Ceratopsia) specimens from two Late Cretaceous Mongolian localities with problematic stratigraphy are described. A specimen of Protoceratops andrewsi from the Zamyn Khond locality enables its correlation with other sites of the Djadokhta Formation. P. andrewsi is also abundant in the Uuden Sair locality, variously assigned to the Djadokhta or Baruungoyot formations. However, one new specimen from that site exhibits a fused nasal horn and a sharp buccal crest of the dentary. With these apomorphic features, it resembles Bagaceratops rozhdestvenskyi, known from the Baruungoyot and Bayan Mandahu formations. It may be an evidence for: sympatric evolution of B. rozhdestvenskyi and P. andrewsi; a dispersal of Bagaceratops to Uuden Sair; hybridization between the two parapatric taxa; or the anagenetic evolutionary transition from P. andrewsi to Bagaceratops. The anagenetic explanation appears to be most strongly supported by given data. This new record advocates for the age of the sediments from the Uuden Sair locality being intermediate between the Djadokhta and Baruungoyot formations. The observed changes in the frequency of the apomorphic features within protoceratopsid samples from various Late Cretaceous sites of the Gobi Desert potentially enable their correlations and chronological ordering.
机译:描述了新的Protocerapopsid(Dinosauria:Ceratopsia)来自两个晚餐蒙古地区的标本,具有有问题的地层的蒙古地区。来自Zamyn Khond Localitial的Protoceraps Andrewsi标本能够与Djadokhta形成的其他网站相关。 P. Andrewsi在Uuden Sair途中也丰富,各种分配给Djadokhta或Baruengoyot地层。然而,来自该网站的一项新标本展示了一个融合的鼻角和伪心的尖锐的颊嵴。凭借这些制导特征,它类似于Baruengoyot和Bayan Mandahu的组织,从Bagaceratops Rozhdestvenskyi。它可能是一种证据:B. Rozhdestvenskyi和P. Andrewsi的SympaTric演变;对Uuden Sair的Bagaceratops分散;两个帕拉奇毒素之间的杂交;或者从P. Andrewsi到Bagaceratops的Anagenetic进化过渡。对给定数据来说,似乎是最强烈的支持。这种新的纪录倡导沉积物的年龄来自uuden坐在的沉积物的年龄是Djadokhta和Baruengoyot地层之间的中间。观察到戈壁沙漠的各种晚期白垩纪位点的经过细胞凋落体样品中静脉凋落性样本频率的变化可能使其相关性和按时间顺序排列。

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