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Oxygenation in carbonate microbialites and associated facies after the end-Permian mass extinction: Problems and potential solutions
Kershaw, Stephen1; Tang, Hao2; Li, Yue (李越)3; Guo, Li4
2018
发表期刊JOURNAL OF PALAEOGEOGRAPHY-ENGLISH
ISSN2095-3836
卷号7期号:1页码:32-47
摘要

Carbonate sediments deposited in normally-oxygenated shallow ocean waters of the latest Permian period, immediately prior to the end-Permian mass extinction, contain well-developed diverse shelly faunas. After the extinction of these skeletal metazoans, the sediments commonly comprise microbialites (regarded by most authors as benthic) and associated facies bearing evidence interpreted by many authors to indicate reduced oxygenation of the shallow ocean waters. However, the evidence of oxygenation state is inconsistent and the sequences have gaps, indicated in the following 5 points: 1) Shelly fossils occur commonly in post-extinction shallow marine limestones, and likely to have been aerated in contact with the atmosphere. Nevertheless, although the largest mass extinction in Earth history may have caused reduced body size in shelly organisms, such reduction is arguably due to environmental stress of lowered oxygenation. Discriminating between these controls remains a challenge. 2) Abundant pyrite framboids in many post-extinction limestones are interpreted by several authors as indicating dysoxic contemporaneous waters, so the organisms that lived there, now shelly fossils, were dysaerobic. However, verification is problematic because pyrite framboids scattered amongst shelly fossils cannot have formed amongst living organisms, which need at least some oxygen; synsedimentary framboid formation requires anoxic conditions in the redox boundary where sulphate-reducing processes work. Thus, framboids and shelly fossils found together means taphonomic mixing of sediments, destroying original depositional relationships so that it is not possible to determine whether the shells were aerobic or dysaerobic prior to sediment mixing. Furthermore, diagenetic growth of framboids is possible, as is import of previously-formed framboids from deeper water during upwelling. Thus, there is no proof of an environmental link between framboid size and occurrence, and contemporaneous oxygenation in these post-extinction shallow water facies, so we question the validity of this model in those facies, but consider that the model is valid for deeper water facies. 3) Some publications provide evidence of oxygenation, from redox-sensitive elements in post-extinction limestones, while others indicate low oxygen conditions. Redox-sensitive geochemistry requires further work to explore this issue at higher resolution of sampling than has been so far applied. 4) Biomarkers recorded in some post-extinction facies contain evidence of anoxic conditions (including green sulphur bacteria) but other examples lack these, which may be indicate fluctuations of water oxygenation. However, a key issue that has not yet been resolved is determination of whether biomarkers were imported into the sites of deposition, for example by upwelling currents, or formed where they are found. Thus, there is currently no verification that biomarkers of low oxygen organisms in shallow water settings actually formed in the places where they are sampled. 5) The common occurrence of small erosion surfaces and stylolites represents loss of evidence, and must be accounted for in future studies. The oxygenation state of post-end-Permian extinction shallow marine facies continues to present a challenge of interpretation, and requires high-resolution sampling and careful attention to small-scale changes, as well as loss of rock through pressure solution, as the next step to resolve the issue.

关键词Stromatolite Thrombolite Microbialite Permian-triassic Boundary Pyrite Anoxia
DOI10.1016/j.jop.2017.10.001
语种英语
关键词[WOS]Earliest Triassic Microbialites ; Photic-zone Euxinia ; South China ; Nanpanjiang Basin ; Ecological Crisis ; Framboidal Pyrite ; Sichuan Province ; Redox Conditions ; Sulfur Isotopes ; Boundary Crisis
资助项目National Scientific and Technology Major Project[2016ZX05004002-001] ; National Natural Science Foundation of China[41602166]
WOS研究方向Geology ; Paleontology
WOS类目Geosciences, Multidisciplinary ; Paleontology
WOS记录号WOS:000428753900003
项目资助者National Scientific and Technology Major Project ; National Natural Science Foundation of China
出版者SCIENCE PRESS
文献类型期刊论文
条目标识符http://ir.nigpas.ac.cn/handle/332004/18882
专题中国科学院南京地质古生物研究所
其他
通讯作者Kershaw, Stephen
作者单位1.Brunel Univ, Dept Life Sci, Kingston Lane, Uxbridge UB8 3PH, Middx, England
2.Southwest Petr Univ, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610500, Sichuan, Peoples R China
3.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, CAS Key Lab Econ Stratig & Palaeogeog, Nanjing 210008, Jiangsu, Peoples R China
4.Univ Cambridge, Dept Earth Sci, CASP, Cambridge CB3 0UD, England
推荐引用方式
GB/T 7714
Kershaw, Stephen,Tang, Hao,Li, Yue ,et al. Oxygenation in carbonate microbialites and associated facies after the end-Permian mass extinction: Problems and potential solutions[J]. JOURNAL OF PALAEOGEOGRAPHY-ENGLISH,2018,7(1):32-47.
APA Kershaw, Stephen,Tang, Hao,Li, Yue ,&Guo, Li.(2018).Oxygenation in carbonate microbialites and associated facies after the end-Permian mass extinction: Problems and potential solutions.JOURNAL OF PALAEOGEOGRAPHY-ENGLISH,7(1),32-47.
MLA Kershaw, Stephen,et al."Oxygenation in carbonate microbialites and associated facies after the end-Permian mass extinction: Problems and potential solutions".JOURNAL OF PALAEOGEOGRAPHY-ENGLISH 7.1(2018):32-47.
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