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DOI10.1016/j.palaeo.2020.109770
Polybessurus-like fossils as key contributors to Permian–Triassic boundary microbialites in South China
Zhang X.-Y.; Zheng Q.-F.; Li Y.; Yang H.-Q.; Zhang H.; Wang W.-Q.; Shen S.-Z.
发表日期2020
ISSN0031-0182
卷号552
英文摘要Massive occurrences of microbialites near the Permian–Triassic boundary have been interpreted as being due to benthic microbial proliferation in unusual marine conditions after the end-Permian mass extinction. Here, we present large populations of Polybessurus-like microfossils in the microbialites of the South China Craton to reveal their morphological structures, growth patterns, and ecological implications. These distinctive microfossils are composed of layered stalks and spherical endpoints. The spheroids, 20–40 μm in diameter, comprising external thin micritic walls and internal sparry parts, are interpreted as coccoid cyanobacteria. The stalks consist of multiple “stacked-cup” micritic envelopes consisting of micron-sized magnesian calcite/dolomite grains and are catalogued as calcified remains of coccoid cyanobacterial extracellular polymeric substances (EPS). Early microbially mediated calcification of EPS increased the preservation potential of microfossils. The microfossils stand upright as coccoid unicells supported by the highly unidirectional secretion of EPS, revealing their benthic behaviours. The successively secreted EPS lift the cells away from the substrate, expanding their ecological niches to gain more sunlight for photosynthesis in the barren marine floor. The distinctive Polybessurus-like microfossils can be viewed both in laminae of stromatolites and in spotted/digitate clots of thrombolites, suggesting their critical roles in microbe-dominated reefs in the aftermath of the end-Permian mass extinction. The morphological features and growth patterns of the Polybessurus-like fossils resemble their Proterozoic counterpart—Polybessurus bipartitus Fairchild ex Green et al. (1987). The widespread Polybessurus-like fossils in the Permian–Triassic boundary microbialites of the South China Craton suggest pervasive retrogressive ecosystems on carbonate platforms after the largest extinction event during the Earth's history. © 2020 Elsevier B.V.
英文关键词Calcified EPS; Coccoid cyanobacteria; End-Permian extinction; Microbialite; South China Craton
语种英语
scopus关键词carbonate platform; cyanobacterium; fossil record; marine environment; mass extinction; microbialite; microfacies; microfossil; morphology; Permian-Triassic boundary; Proterozoic; China; Coccoidea; Cyanobacteria
来源期刊Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/150471
作者单位CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, 164 West Xin'gang Road, Guangzhou, 510301, China; Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou, 511400, China; State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China; School of Earth Sciences and Engineering, Nanjing University, 163 Xianlin Avenue, Nanjing, 210023, China
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Zhang X.-Y.,Zheng Q.-F.,Li Y.,等. Polybessurus-like fossils as key contributors to Permian–Triassic boundary microbialites in South China[J],2020,552.
APA Zhang X.-Y..,Zheng Q.-F..,Li Y..,Yang H.-Q..,Zhang H..,...&Shen S.-Z..(2020).Polybessurus-like fossils as key contributors to Permian–Triassic boundary microbialites in South China.Palaeogeography, Palaeoclimatology, Palaeoecology,552.
MLA Zhang X.-Y.,et al."Polybessurus-like fossils as key contributors to Permian–Triassic boundary microbialites in South China".Palaeogeography, Palaeoclimatology, Palaeoecology 552(2020).
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