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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Brachiopod miniaturization and its possible causes during the Permian-Triassic crisis in deep water environments, South China
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Brachiopod miniaturization and its possible causes during the Permian-Triassic crisis in deep water environments, South China

机译:中国南方深水环境中的二叠纪-三叠纪危机期间腕足动物小型化及其可能原因

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Brachiopod miniaturization is both the reduction in size of individuals of a species over time, and where one brachiopod fauna dominated by larger individuals was replaced by a brachiopod fauna dominated by smaller individuals over time. This paper investigates this phenomenon prior to and during the end-Permian crisis in a deep water setting in South China, based on precise measurements of brachiopod body size and on the abundance and diversity of brachiopod species. The process of miniaturization near the Permian-Triassic boundary in deep water environments is characterized by: (1) Larger species, including Martirria sp., Costattamulus dongpanensis, and Anidanthus mucronata, reduced in average body size and abundance over time towards the end-Permian brachiopod extinction event. (2) Small species, including Attenuatella mengi and Spinomarginifera semicircridge, showed a mixed response with either no size change, or a reduction in average body size, while these species increased in abundance over time, indicating they were less sensitive to the stressed environmental setting. (3) Both the total abundance and the diversity of this brachiopod fauna decreased over time towards the end-Permian crisis. Regression, an increased input of terrestrial material and productivity decline are considered to all have contributed to brachiopod miniaturization, based on the biotic replacement and changes in sea-water chemistry. Among these factors, the fall in sea level is perhaps the primary factor, and led to a decline in productivity and an increased input of terrestrial material into the marine setting. (C) 2007 Published by Elsevier B.V.
机译:腕足动物小型化既是物种个体随时间推移的减小,又是一种由较大个体主导的腕足动物群被随时间推移较小个体主导的腕足动物群所取代。本文基于腕足动物体的精确测量以及腕足动物的丰富度和多样性,研究了在华南深水环境中二叠纪末危机发生之前和之中的这一现象。在深水环境中,二叠纪-三叠纪边界附近的小型化过程具有以下特征:(1)较大的物种,包括Martirria sp。,Costattamulus dongpanensis和Anidanthus mucronata,随着到二叠纪末期的平均体形和丰度的降低腕足动物灭绝事件。 (2)小物种,包括孟氏Attenuatella mengi和Spinomarginifera semicircridges,表现出混合的反应,没有大小变化或平均体型减小,而这些物种随着时间的流逝而增加,这表明它们对压力环境的敏感性较低。 。 (3)随着二叠纪末危机的来临,腕足动物的总数量和多样性都随着时间而下降。基于生物替代和海水化学变化,回归,陆地物质输入增加和生产力下降都被认为有助于腕足动物的小型化。在这些因素中,海平面下降可能是主要因素,导致生产力下降和陆生材料向海洋环境的投入增加。 (C)2007由Elsevier B.V.发布

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