Ostracods after the end-Permian extinction in South China: insights into non-microbial survival

IF 1.3 4区 地球科学 Q3 PALEONTOLOGY Micropaleontology Pub Date : 2020-09-01 DOI:10.47894/mpal.66.5.02
M. Forel, A. Bercovici, Jianxin Yu
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引用次数: 4

Abstract

The taxonomy of ostracods from one deep-water, one shallow shelf and three paralic sections spanning the end-Permian extinction in South China (Guizhou and Yunnan) is summarized and discussed.We report on the occurrence of nine species, including mass occurrences of Hollinella panxiensis Wang, on the surface of these clastic Permian-Triassic transitional beds. The preservation of the material allows for the description of the central muscle scar field of Langdaia suboblonga Wang, which is the first observation of this character for the genus. These firstly described assemblages differ from those from post-extinction microbial deposits in being dominated by Palaeocopida. They illustrate survival without recovery after the end-Permian crisis, as none of the reported taxa participated in the subsequent Triassic diversification. We relate this phenomenon to clastic input and show that the patchy survival of benthic faunas following the crisis is an interplay between environments and adaptive potential. The persistence of Palaeocopida as a function of their depth distribution is discussed with the illustration of short-term survival of Hollinellidae in shallow areas, as opposed to the survival of Kirkbyidae in deep-marine waters until, at least, the Late Triassic.
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中国南方二叠纪末灭绝后的介形类:对非微生物生存的洞察
对华南(贵州和云南)二叠纪末灭绝的一个深水、一个浅陆架和三个平行剖面的介形虫分类进行了总结和讨论。我们报道了在这些碎屑二叠纪-三叠纪过渡层的表面上出现的9个物种,包括大规模出现的潘氏Hollinella Wang。该材料的保存使人们能够描述王的中央肌肉瘢痕区,这是该属首次观察到这一特征。这些首次描述的组合与灭绝后微生物沉积物的不同之处在于,它们以古生物门为主。它们说明了二叠纪末危机后没有恢复的生存,因为没有一个报告的分类群参与了随后的三叠纪多样化。我们将这一现象与碎屑输入联系起来,并表明危机后海底动物群的不稳定生存是环境和适应潜力之间的相互作用。Paleocopida的持久性与其深度分布的函数进行了讨论,并举例说明了Hollinelidae在浅水区的短期生存,而Kirkbyidae至少在三叠纪晚期之前在深海中的生存。
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来源期刊
Micropaleontology
Micropaleontology 地学-古生物学
CiteScore
3.20
自引率
6.70%
发文量
18
审稿时长
>12 weeks
期刊介绍: The Journal of Micropalaeontology (JM) is an established international journal covering all aspects of microfossils and their application to both applied studies and basic research. In particular we welcome submissions relating to microfossils and their application to palaeoceanography, palaeoclimatology, palaeobiology, evolution, taxonomy, environmental change and molecular phylogeny. Owned by The Micropalaeontological Society, the scope of the journal is broad, demonstrating the application of microfossils to solving broad geoscience issues.
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