首页> 外文期刊>Carnets de Geologie: Notebooks of geology >Temporal and latitudinal trends in the biodiversity of European Atlantic Cenozoic gastropod (Mollusca) faunas. A base for the history of biogeographic provinces
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Temporal and latitudinal trends in the biodiversity of European Atlantic Cenozoic gastropod (Mollusca) faunas. A base for the history of biogeographic provinces

机译:欧洲大西洋新生代腹足动物(软体动物)动物群生物多样性的时空和纬度趋势。生物地理省历史的基础

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A general overview of the biodiversity of the marine fauna during the Tertiary period is developed in the context of the biogeographical evolution of the European realm. This study combines a reappraisal of the literature with a unique first-hand source of data on the richest marine group (the gastropods) from over a 25 million year period (Early Oligocene to Late Miocene). In total the French deposits have yielded more than 10,000 species from the Eocene to the Upper Miocene. Evidence of significant bias in the fossil record is pointed out for the Palaeocene (Danian) and Upper Eocene (Priabonian). For the period considered (Palaeocene to Late Miocene, ca 50 million years) the second highest diversity is reported in the Late Oligocene. This study reveals also the importance of pre-Miocene extinctions of genera. The Oligocene was when the latitudinal differentiation of the faunas was greatest. The local generic gastropod richness ranges from 59 (Rupelian of Belgium) to 494 (Chattian of Aquitaine). A clear trend towards homogenization appears in the Late Oligocene which leads to the development of a vast biogeographical region named Euro-West Africa. This faunal evolutionary pattern has never been demonstrated before and is a novel feature of the biogeography of the Eastern-Atlantic region.
机译:在欧洲范围的生物地理演化的背景下,对第三纪时期海洋动物的生物多样性进行了总体概述。这项研究结合了对文献的重新评估以及独特的第一手资料,这些资料来自超过2500万年的时期(早渐新世至中新世)最丰富的海洋群(腹足动物)。从始新世到中新世上层,法国矿床总共产生了10,000多种物种。指出了古新世(达尼安)和上新世(上新世)在化石记录中存在明显偏差的证据。在所考虑的时期(古新世至晚中新世,约5000万年),晚渐新世的多样性第二高。这项研究还揭示了中新世前灭绝的重要性。渐新世是动物区系的横向差异最大的时期。当地普通腹足动物的丰富度从59(比利时的Rupelian)到494(阿基坦的查特)。渐新世出现了明显的均质化趋势,这导致了一个广阔的生物地理区域的发展,这个区域被称为欧洲西非。这种动物的进化模式以前从未被证明过,并且是东大西洋地区生物地理学的一个新颖特征。

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