中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Response of Siliceous Marine Organisms to the Permian-Triassic Climate Crisis Based on New Findings From Central Spitsbergen, Svalbard

文献类型:期刊论文

作者Foster, W. J.6; Asatryan, G.5; Rauzi, S.4; Botting, J. P.2,3; Buchwald, S. Z.6; Lazarus, D. B.5; Isson, T.4; Renaudie, J.5; Kiessling, W.1
刊名PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
出版日期2023-12-01
卷号38期号:12页码:10
ISSN号2572-4517
关键词Permian-Triassic radiolarians hexactinellids climate response thermal stress
DOI10.1029/2023PA004766
通讯作者Foster, W. J.(w.j.foster@gmx.co.uk)
英文摘要Siliceous marine ecosystems play a critical role in shaping the Earth's climate system by influencing rates of organic carbon burial and marine authigenic clay formation (i.e., reverse weathering). The ecological demise of silicifying organisms associated with the Permian-Triassic mass extinction is postulated to have elevated marine authigenic clay formation rates, resulting in a prolonged greenhouse climate during the Early Triassic. Yet, our understanding of the response of siliceous marine organisms during this critical interval is poor. Whilst radiolarians experienced the strongest diversity loss in their evolutionary history and perhaps also the greatest population decline of silica-secreting organisms during this event, only a small number of Griesbachian (post-extinction) localities that record siliceous organisms are known. Here, we report newly discovered latest Changhsingian to early Griesbachian (Clarkina meishanensis - Hindeodus parvus Zone) radiolarians and siliceous sponge spicules from Svalbard. This fauna documents the survival of a low-diversity radiolarian assemblage alongside stem-group hexactinellid sponges making this the first described account of post-extinction silica-secreting organisms from the Permian/Triassic boundary in a shallow marine shelf environment and a mid-northern paleolatitudinal setting. Our findings indicate that latitudinal diversity gradients for silica-secreting organisms following the mass extinction were significantly altered, and that silica productivity was restricted to high latitude and deep water thermal refugia. This result has potential to further shape our understanding of changes in marine dissolved silica levels and in turn rates of reverse weathering, with implications for our understanding of carbon cycle dynamics during this interval. First occurrence of siliceous sponges and radiolarians (biogenic silica) from a mid-northern paleolatitude following the mass extinctionEvidence that extinction survivors show poleward range shifts in response to thermal stressBiosiliceous productivity persisted during the Early Triassic chert gap impeding the existence of Precambrian-like marine conditions
WOS关键词MINO TERRANE ; VIKINGHOGDA FORMATION ; NORTHWEST PANGEA ; CHERT ; ROCKS ; RADIOLARIAN ; DIVERSITY ; ECOLOGY ; GROWTH ; STRATIGRAPHY
资助项目Deutsche Forschungsgemeinschaft[FO1297/1-1] ; Open Access Publication Fund of Universitat Hamburg ; Projekt DEAL
WOS研究方向Geology ; Oceanography ; Paleontology
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:001119824900001
资助机构Deutsche Forschungsgemeinschaft ; Open Access Publication Fund of Universitat Hamburg ; Projekt DEAL
源URL[http://ir.nigpas.ac.cn/handle/332004/42788]  
专题中国科学院南京地质古生物研究所
通讯作者Foster, W. J.
作者单位1.Friedrich Alexander Univ Erlangen Nurnberg, GeoZentrum Nordbayern, Dept Geog & Geosci, Erlangen, Germany
2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing, Peoples R China
3.Amgueddfa Cymru Natl Museum Wales, Dept Nat Sci, Cardiff, Wales
4.Univ Waikato Tauranga, Te Aka Matuatua, BOP, Tauranga, New Zealand
5.Leibniz Inst Evolut & Biodivers Sci, Museum Nat Kunde, Berlin, Germany
6.Univ Hamburg, Inst Geol, Ctr Erdsystemforsch & Nachhaltigkeit, Hamburg, Germany
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Foster, W. J.,Asatryan, G.,Rauzi, S.,et al. Response of Siliceous Marine Organisms to the Permian-Triassic Climate Crisis Based on New Findings From Central Spitsbergen, Svalbard[J]. PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY,2023,38(12):10.
APA Foster, W. J..,Asatryan, G..,Rauzi, S..,Botting, J. P..,Buchwald, S. Z..,...&Kiessling, W..(2023).Response of Siliceous Marine Organisms to the Permian-Triassic Climate Crisis Based on New Findings From Central Spitsbergen, Svalbard.PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY,38(12),10.
MLA Foster, W. J.,et al."Response of Siliceous Marine Organisms to the Permian-Triassic Climate Crisis Based on New Findings From Central Spitsbergen, Svalbard".PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY 38.12(2023):10.

入库方式: OAI收割

来源:南京地质古生物研究所

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