中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Coupled evolution of nitrogen cycling and redoxcline dynamics on the Yangtze Block across the Ediacaran-Cambrian transition

文献类型:期刊论文

作者Chen, Yan1,2,3,4; Diamond, Charles W.2; Stueken, Eva E.5,6; Cai, Chunfang1,3,4; Gill, Benjamin C.7; Zhang, Feifei8; Bates, Steve M.2; Chu, Xuelei3,4; Ding, Yi1,3,4; Lyons, Timothy W.2
刊名GEOCHIMICA ET COSMOCHIMICA ACTA
出版日期2019-07-15
卷号257页码:243-265
ISSN号0016-7037
关键词Ediacaran Cambrian Yangtze Block Nitrogen cycling Redoxcline Ammonium
DOI10.1016/j.gca.2019.05.017
英文摘要The Ediacaran-Cambrian transition is characterized by the evolution of complex eukaryotes and rapid diversification of metazoans. However, linkages between environmental triggers and evolutionary patterns remain unclear. Here, we present high-resolution records of carbon and nitrogen isotopic data (delta C-13, delta N-15) for a drill core extending from the early Ediacaran Doushantuo Formation to the early Cambrian Jiumenchong Formation, located on the slope of the Yangtze Block. Our data show that sedimentary bulk nitrogen isotope values (delta N-15(bulk)) decrease progressively from the early Ediacaran to the early Cambrian, broadly concurrent with nitrogen isotope data from other sections throughout the Yangtze Block. During the early Ediacaran, however, delta N-15 bulk values from our study are higher (maximum 11.2%e) compared to those from more restricted coeval sections, suggesting a higher degree of denitrification in our slope section. The early Ediacaran delta N-15(bulk) data from the Yangtze Block may thus provide indirect evidence for an upwelling system that led to a shallower redoxcline in slope environments of the Upper Yangtze region. Widespread light delta N-15 bulk values from the early Cambrian (minimum -7.5%e) paired with excess silicate-bound nitrogen throughout much of the Yangtze Block are most parsimoniously interpreted as non-quantitative assimilation of ammonium (NH4-) with relatively high concentrations of NH4+ accumulating in the deep basin. Overall, the spatial and temporal trends in nitrogen cycling across the Yangtze Block suggest that fixed nitrogen was more bioavailable in the Ediacaran-Cambrian Yangtze Basin compared to previously studied Mesoproterozoic sections, although nitrogen speciation in the photic zone may have varied with time. Environmental factors such as oxygen levels and nitrogen bioavailability may have shaped the evolutionary trajectory of life on the Yangtze Block and potentially elsewhere across the Ediacaran-Cambrian transition. (C) 2019 Elsevier Ltd. All rights reserved.
WOS关键词SOUTH CHINA IMPLICATIONS ; ORGANIC-CARBON ISOTOPE ; ATMOSPHERIC OXYGEN ; TRACE-ELEMENTS ; METASEDIMENTARY ROCKS ; DOUSHANTUO FORMATION ; OCEANIC OXYGENATION ; SINKING PARTICLES ; ANAMMOX BACTERIA ; STABLE NITROGEN
资助项目NSF FESD program ; Earth-Life Transitions program ; NASA Astrobiology Institute[NNA15BB03A] ; key project of the Natural Science Foundation of China[41730424] ; program of China Scholarships Council[201504910582] ; Virginia Tech
WOS研究方向Geochemistry & Geophysics
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000470830800016
资助机构NSF FESD program ; NSF FESD program ; NSF FESD program ; NSF FESD program ; Earth-Life Transitions program ; Earth-Life Transitions program ; Earth-Life Transitions program ; Earth-Life Transitions program ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; program of China Scholarships Council ; program of China Scholarships Council ; program of China Scholarships Council ; program of China Scholarships Council ; Virginia Tech ; Virginia Tech ; Virginia Tech ; Virginia Tech ; NSF FESD program ; NSF FESD program ; NSF FESD program ; NSF FESD program ; Earth-Life Transitions program ; Earth-Life Transitions program ; Earth-Life Transitions program ; Earth-Life Transitions program ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; program of China Scholarships Council ; program of China Scholarships Council ; program of China Scholarships Council ; program of China Scholarships Council ; Virginia Tech ; Virginia Tech ; Virginia Tech ; Virginia Tech ; NSF FESD program ; NSF FESD program ; NSF FESD program ; NSF FESD program ; Earth-Life Transitions program ; Earth-Life Transitions program ; Earth-Life Transitions program ; Earth-Life Transitions program ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; program of China Scholarships Council ; program of China Scholarships Council ; program of China Scholarships Council ; program of China Scholarships Council ; Virginia Tech ; Virginia Tech ; Virginia Tech ; Virginia Tech ; NSF FESD program ; NSF FESD program ; NSF FESD program ; NSF FESD program ; Earth-Life Transitions program ; Earth-Life Transitions program ; Earth-Life Transitions program ; Earth-Life Transitions program ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; key project of the Natural Science Foundation of China ; program of China Scholarships Council ; program of China Scholarships Council ; program of China Scholarships Council ; program of China Scholarships Council ; Virginia Tech ; Virginia Tech ; Virginia Tech ; Virginia Tech
源URL[http://ir.iggcas.ac.cn/handle/132A11/92270]  
专题地质与地球物理研究所_中国科学院油气资源研究重点实验室
通讯作者Cai, Chunfang; Lyons, Timothy W.
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resource Res, Beijing 100029, Peoples R China
2.Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USA
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
5.Univ St Andrews, Sch Earth & Environm Sci, St Andrews KY16 9AL, Fife, Scotland
6.NASA, Astrobiol Inst, Virtual Planetary Lab, Seattle, WA 98195 USA
7.Virginia Polytech Inst & State Univ, Dept Geosci, Blacksburg, VA 24061 USA
8.Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA
推荐引用方式
GB/T 7714
Chen, Yan,Diamond, Charles W.,Stueken, Eva E.,et al. Coupled evolution of nitrogen cycling and redoxcline dynamics on the Yangtze Block across the Ediacaran-Cambrian transition[J]. GEOCHIMICA ET COSMOCHIMICA ACTA,2019,257:243-265.
APA Chen, Yan.,Diamond, Charles W..,Stueken, Eva E..,Cai, Chunfang.,Gill, Benjamin C..,...&Lyons, Timothy W..(2019).Coupled evolution of nitrogen cycling and redoxcline dynamics on the Yangtze Block across the Ediacaran-Cambrian transition.GEOCHIMICA ET COSMOCHIMICA ACTA,257,243-265.
MLA Chen, Yan,et al."Coupled evolution of nitrogen cycling and redoxcline dynamics on the Yangtze Block across the Ediacaran-Cambrian transition".GEOCHIMICA ET COSMOCHIMICA ACTA 257(2019):243-265.

入库方式: OAI收割

来源:地质与地球物理研究所

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