首页> 外文期刊>Journal of vertebrate paleontology >Regional to global patterns in Late Cretaceous selachian (Chondrichthyes, Euselachii) diversity
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Regional to global patterns in Late Cretaceous selachian (Chondrichthyes, Euselachii) diversity

机译:晚白垩世selachian(Chondrichthyes,Euselachii)多样性的区域到全球格局

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Although selachian fossil remains have been studied for nearly three centuries, little is known about their evolutionary history. Recent studies have suggested different timings of early diversification events in the Late Triassic, Jurassic, and Early Cretaceous. However, Late Cretaceous selachian diversity has remained little explored despite numerous and diversified selachian assemblages known from this time interval. Sampling standardization, origination/extinction rates, and raw ordinal diversity were examined based on taxonomic occurrences in three data sets representing distinct geographical areas (Anglo-Paris Basin, northwestern Europe, and Western Interior Seaway) spanning the Cenomanian-Campanian interval. This examination allowed the identification of regional diversity events, previously reported for some invertebrate groups, but presented for the first time for a marine vertebrate group. The local mid-Cenomanian diversity drop (Anglo-Paris Basin) is interpreted as a possible consequence of changes in bottom seawater conditions related to the rapid mid-Cenomanian transgression. The Cenomanian/Turonian faunal turnover is likely to be due to various sampling biases (Anglo-Paris Basin and northwestern Europe), but a genuine extinction in the Western Interior Seaway cannot be excluded. The Santonian diversity peak synchronous with a marked global increase in seawater temperatures contrasts with the rapid temperature decrease linked with low diversity in the early Campanian. SUPPLEMENTAL DATA - Supplemental materials are available for this article for free at www.tandfonline.com/UJVP
机译:尽管塞拉奇人化石的遗迹已经研究了近三个世纪,但对其演化历史知之甚少。最近的研究表明,三叠纪晚期,侏罗纪和白垩纪早期发生多样化事件的时机不同。然而,尽管从这个时间间隔已知了许多和多样化的塞拉契亚组合,但白垩纪晚期塞拉奇兰的多样性仍然很少被探索。根据分类学上出现的样本标准化,起源/灭绝率和原始序数多样性,对三个数据集进行了分类,这些数据集代表了跨越Cenomanian-Campanian区间的不同地理区域(Anglo-Paris盆地,西北欧洲和Western Interior Seaway)。这项检查可以识别以前曾报道过的一些无脊椎动物群体的区域多样性事件,但首次出现在海洋脊椎动物群体中。本地的西诺曼尼亚中期生物多样性下降(昂洛-巴黎盆地)被解释为与快速的西诺曼尼亚中期海侵有关的底部海水状况变化的可能结果。西诺曼尼亚/突尼斯的动物区系更新可能是由于各种采样偏差(安格洛-巴黎盆地和西北欧洲)引起的,但不能排除西部内陆海域的真正灭绝。 Santonian多样性峰与全球海水温度显着升高同步,而温度快速下降与Campanian早期的低多样性相关。补充数据-可在www.tandfonline.com/UJVP上免费获得本文的补充材料

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