DOI: 10.1016/j.earscirev.2018.09.007
论文题名: Marine sulfur cycle evidence for upwelling and eutrophic stresses during Early Triassic cooling events
作者: Stebbins A. ; Algeo T.J. ; Krystyn L. ; Rowe H. ; Brookfield M. ; Williams J. ; Nye Jr S.W. ; Hannigan R.
刊名: Earth Science Reviews
ISSN: 00128252
出版年: 2019
卷: 195 起始页码: 68
结束页码: 82
语种: 英语
中文关键词: Carbonate-associated sulfate
; Microbial sulfate reduction
; Neo-Tethys Ocean
; Pyrite
; Spiti Valley
; Sulfur isotopes
英文关键词: carbonate
; cooling
; eutrophication
; marine environment
; paleoceanography
; pyrite
; sulfate
; sulfur cycle
; sulfur isotope
; Triassic
; upwelling
; Himachal Pradesh
; India
; Spiti Valley
英文摘要: Perturbations to the global carbon and sulfur cycles recurred episodically throughout the ~5-Myr-long Early Triassic, in the aftermath of the end-Permian mass extinction, the largest biocrisis in Earth's history. In this study, analyses of carbonate-associated sulfate (CAS) sulfur, CAS oxygen, and pyrite sulfur-isotope ratios in a continental shelf section from the southern Neo-Tethys Ocean (Spiti Valley, India) provide new insights into the Early Triassic marine sulfur cycle. Secular variation in CAS sulfur-isotope values at Spiti is similar to that in South China, suggesting that CAS was a robust recorder of a global seawater sulfate signal. The Spiti CAS and pyrite δ34S profiles show that the highest rates of pyrite burial coincided with cooler sea-surface temperatures. We infer that climatic cooling steepened equator-to-pole temperature gradients, invigorating thermohaline overturning circulation, and enhancing upwelling of nutrients that stimulated marine productivity and organic carbon sinking fluxes. Enhanced productivity fueled and sustained microbial respiration, increased oxygen demand, and, within the southern Neo-Tethys, caused the zone of microbial sulfate reduction to migrate upwards and become more connected to the water column. Microbial sulfate reduction, under these conditions, was no longer limited by organic matter or sulfate availability, leading to burial of more 34S-depleted pyrite and 34S- and 18O-enrichment of the oceanic sulfate pool. This environmental scenario suggests possible environmental stresses related to eutrophication during positive carbon-isotope excursions around the Griesbachian-Dienerian, Dienerian-Smithian, and Smithian-Spathian boundaries. Additionally, the difference between CAS and pyrite sulfur-isotope values, Δ34SCAS-pyr, slowly rose through the Early Triassic, reflecting a slow increase in seawater sulfate concentrations following a minimum close to the Permian-Triassic boundary. © 2018 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165933
Appears in Collections: 气候变化与战略
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作者单位: School for the Environment, University of Massachusetts Boston, Boston, MA 02125, United States; Department of Geology, University of Cincinnati, Cincinnati, OH 45221, United States; State Key Laboratories of BGEG and GPMR, China University of Geosciences, Wuhan, 430074, China; Institute for Paleontology, Vienna University, Althanstrasse 14, Vienna, 1090, Austria; Bureau of Economic Geology, The University of Texas at Austin, Austin, TX 78758, United States; Department of Geology, Kent State University, Kent, OH 44242, United States
Recommended Citation:
Stebbins A.,Algeo T.J.,Krystyn L.,et al. Marine sulfur cycle evidence for upwelling and eutrophic stresses during Early Triassic cooling events[J]. Earth Science Reviews,2019-01-01,195