Biogenic brachiopod shell concentrations from the Hongjingshao Formation (Cambrian series 2, Stage 3) in Malong area of eastern Yunnan, South China

被引:0
作者
Chen, Feiyang [1 ,2 ,3 ,5 ,6 ]
Brock, Glenn A. [3 ]
Zhang, Zhiliang [4 ]
Topper, Timothy P. [5 ,6 ,7 ]
Zhang, Zhifei [5 ,6 ]
机构
[1] China Univ Min & Technol, Key Lab Coalbed Methane Resources & Reservoir Form, Minist Educ, Xuzhou 221116, Peoples R China
[2] China Univ Min & Technol, Sch Resources & Geosci, Xuzhou 221116, Peoples R China
[3] Macquarie Univ, Sch Nat Sci, Sydney, NSW 2109, Australia
[4] Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China
[5] Northwest Univ, State Key Lab Continental Dynam, Shaanxi Key Lab Early Life & Environm, Xian 710069, Peoples R China
[6] Northwest Univ, Dept Geol, Xian 710069, Peoples R China
[7] Swedish Museum Nat Hist, Dept Palaeobiol, SE-10405 Stockholm, Sweden
基金
中国国家自然科学基金; 瑞典研究理事会;
关键词
Biogenic shell concentration; Clustered brachiopods; Hongjingshao Formation; Cambrian Stage 3; South China; UNITED-STATES CALIFORNIA; EVOLUTIONARY PALEOECOLOGY; FOSSIL CONCENTRATIONS; IMAGE TREATMENT; RANGE PROVINCE; ORDOVICIAN; BASIN; BEDS; SOFT; LAGERSTATTE;
D O I
10.1016/j.gr.2024.07.007
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Skeletal concentrations are conspicuous taphofacies in the marine record and have been recorded from a wide range of sedimentary facies in Phanerozoic strata, providing baseline data for taphonomy, stratigraphy, sedimentology and palaeoenvironmental reconstructions. Most studied shell concentrations come from post-Cambrian deposits. Here, we document monospecific intrinsic biogenic shell concentrations formed at various stratigraphic levels by the gregarious clustering behavior of the lingulate brachiopod Palaeobolus yunnanensis (Rong, 1974) from the Cambrian Stage 3 Hongjingshao Formation in eastern Yunnan, South China, which represents the oldest-known record of an intrinsic biogenic brachiopod shell concentration in the stratigraphic record. Two types of shell concentrations are represented. Type A concentrations are composed of closely clustered (>28 individuals per square decimeter) in situ complete shells (intrinsic biogenic) buried rapidly near the sediment water interface and forming a distinctive hard pavement in the otherwise completely soft, muddy environment. Type B concentrations are composed of sharply fragmented and broken (but largely unabraded) shells affected by local low energy surface and oscillation currents over longer residence times with destruction and re-deposition exacerbated by surface bulldozing and infaunal bioturbation (extrinsic biogenic). The subsequent occurrence of intrinsic biogenic brachiopod shell concentrations across Laurentia, Siberia, NW Gondwana and South China mostly during Cambrian Stage 4 attests to the initial rise of gregarious aggregation in epifaunal brachiopods during the early Cambrian and the development of new hard substrates in the shallow marine benthos. These relatively rare early Cambrian hard substrates provided new ecospace in soft-bottom benthic communities and were the precursors to the dominant calcareous brachiopod shell concentrations which characterize shallow to deep marine substrates during the Great Ordovician Biodiversification Event. (c) 2024 The Authors. Published by Elsevier B.V. on behalf of International Association for Gondwana Research. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/ licenses/by-nc-nd/4.0/).
引用
收藏
页码:209 / 221
页数:13
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