首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >The Mesozoic return of Paleozoic faunal constituents: A decoupling of taxonomic and ecological dominance during the recovery from the end-Permian mass extinction
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The Mesozoic return of Paleozoic faunal constituents: A decoupling of taxonomic and ecological dominance during the recovery from the end-Permian mass extinction

机译:古生代动物区系的中生代回归:二叠纪末大灭绝恢复过程中的分类学和生态优势的分离

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Phanerozoic diversity curves illustrate that the transition from taxonomic dominance of the Paleozoic Fauna to taxonomic dominance of the Modern Fauna is coincident with the Permo-Triassic boundary. Although a corresponding transition in ecological dominance must have occurred, its timing is unclear. One way to assess ecological dominance during the Early-Middle Triassic recovery interval is through the study of bioclastic accumulations. Bioclastic accumulations from the Early Triassic are largely dominated by constituents of the Modern Fauna. In this study, we examined bioclastic accumulations from the Middle Triassic, the interval after the environmental stress associated with the end-Permian extinction abated.Bioclastic accumulations from Panthalassan deposits (Ladinian portion of the Liard Formation at Williston Lake, Ca?ada) and Tethyan deposits (Anisian-Ladinian Muschelkalk Group, Germany) were examined. Although the most common shell bed-producer differed between the two sites (bivalves, constituents of the Modern Fauna, in Germany and brachiopods, constituents of the Paleozoic Fauna, in Ca?ada), both sites, though geographically disparate, contained significant crinoidal bioclastic accumulations (encrinites).Crinoids, like many constituents of the Paleozoic Fauna, suffered drastic diversity losses at the end-Permian mass extinction and maintained relatively low diversity through the Middle Triassic. Despite reduced diversity, bioclastic accumulations show that crinoids regained some measure of ecologic dominance in the Middle Triassic. In addition, brachiopods, another constituent of the Paleozoic Fauna that suffered severe diversity losses at the end-Permian extinction, regained at minimum local ecological dominance in the Middle Triassic of Panthalassa. These data demonstrate that the transition to Modern faunal taxonomic dominance was decoupled from the transition to Modern faunal ecological dominance.
机译:生代多样性曲线表明,从古生代动物区系的分类优势到现代动物区系的分类优势的过渡与二叠纪—三叠纪界线是一致的。尽管必然发生了生态优势的相应转变,但其时机尚不清楚。评估中三叠世早期恢复时期的生态优势的一种方法是通过研究生物碎屑堆积。三叠纪早期的生物碎屑堆积主要由现代动物区系的成分所控制。在这项研究中,我们研究了中三叠纪的生物碎屑积累,即环境压力与二叠纪末期灭绝相关的时间间隔减弱之后,来自Panthalassan矿床(卡萨达州Williston湖Liard组的拉丁区部分)和Tethyan的生物碎屑积累。对矿床(Anisian-Ladinian Muschelkalk集团,德国)进行了检查。尽管最常见的贝壳床生产者在两个地点之间不同(双壳类动物,现代动物的组成部分,德国和腕足动物,古生动物的组成部分,加利福尼亚州),但两个地点虽然地理位置不同,但都含有大量的贝壳状生物碎屑与古生代动物区系的许多成分一样,类古生物在二叠纪末期生物大灭绝时遭受了急剧的多样性丧失,并且在中三叠纪一直保持相对较低的多样性。尽管减少了多样性,但生物碎屑堆积表明,在中三叠纪,海百合恢复了某种程度的生态优势。此外,腕足类是古生代动物区系的另一个组成部分,在二叠纪末期灭绝时遭受了严重的多样性丧失,在潘塔拉萨中三叠世恢复了最小的局部生态优势。这些数据表明,向现代动物分类优势的过渡与向现代动物生态优势的过渡是分离的。

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