KMS Nanjing Institute of Geology and Palaeonotology,CAS
Primary or secondary? A dichotomy of the strontium isotope anomalies in the Ediacaran carbonates of Saudi Arabia | |
Cui, Huan (崔欢)1,2,3; Kaufman, Alan J.4,5; Zou, Haibo6; Kattan, Fayek H.7; Trusler, Peter8; Smith, Jeff8; Ivantsov, Andrey Yu8,9; Rich, Thomas H.8,10,11; Al Qubsani, Ashraf7; Yazedi, Abdullah7 | |
2020-07-01 | |
发表期刊 | PRECAMBRIAN RESEARCH |
ISSN | 0301-9268 |
卷号 | 343页码:24 |
摘要 | Secular variation of Sr-87/Sr-86 in carbonate strata has been widely used in regional and global chemostratigraphic correlations. Typically, diagenesis results in higher Sr-87/Sr-86 signals relative to their primary composition due to the alteration by Rb-rich fluids and radiogenic decay of Rb-87 to Sr-87. Surprisingly, Sr-87/Sr-86 values in the Ediacaran limestones from Saudi Arabia (from 0.7029 to 0.7059) are significantly lower than typical Ediacaran seawater values (mostly from 0.7080 to 0.7090) based on a global compilation. Understanding the origin of these anomalies is important insofar as early macrofossils are preserved in these strata. Two hypotheses have been independently evaluated in this study. The first hypothesis shows a low temperature scenario with isolated oceans or lakes in proximity to a mafic source. The second hypothesis is characterized by a high temperature scenario with profound overprints by juvenile hydrothermal fluids. Integrated Sr and Nd isotope data reveal that the Sr-87/Sr-86 anomalies are closely coupled with positive epsilon Nd(t = 560 Ma) values (up to +4.1). Clear covariations between Sr-87/Sr-86, epsilon Nd, TOC, delta C-13(carb), delta C-13(org), and delta O-13(carb) were found. Based on multiple lines of petrographic, field, and geochemical evidence, the second hypothesis (i.e., hydrothermal alteration by juvenile fluids) is preferred in this study. Thermogenic breakdown of organic matter in host sediments may have caused the increasingly low TOC abundance and high delta C-13(org) signals of the residual organic matter. We argue that the concept that the Ediacaran biotic radiation took place in an isolated lake environment should be treated with caution. These remarkably low Sr-87/Sr-86 signals have neither temporal nor biogeochemical significance. Sr isotope chemostratigraphy in this particular region may not be a reliable tool for stratigraphic correlations. |
关键词 | Strontium isotopes Neodymium isotopes Ediacaran Early macroorganisms Hydrothermal alteration Chemostratigraphy Diagenesis Geobiology Saudi Arabia |
DOI | 10.1016/j.precamres.2020.105720 |
收录类别 | SCI |
语种 | 英语 |
关键词[WOS] | RARE-EARTH-ELEMENTS ; NUBIAN SHIELD ; TRACE-ELEMENT ; SM-ND ; DOUSHANTUO FORMATION ; JIBALAH GROUP ; BLACK SHALE ; EVOLUTION ; SR ; SEAWATER |
资助项目 | Saudi Geological Survey ; Australian International Geoscience Program (IGCP) Committee ; UNESCO IGCP Board[IGCP587] ; National Geographic Society ; Geological Society of America (GSA) graduate student research grant ; FESD grant[NSF-EAR 13-38810] ; Belgian Science Policy (BELSPO) ; Research Foundation -Flanders (FWO) ; VUB strategic program ; State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000532835600012 |
项目资助者 | Saudi Geological Survey ; Australian International Geoscience Program (IGCP) Committee ; UNESCO IGCP Board ; National Geographic Society ; Geological Society of America (GSA) graduate student research grant ; FESD grant ; Belgian Science Policy (BELSPO) ; Research Foundation -Flanders (FWO) ; VUB strategic program ; State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences |
出版者 | ELSEVIER |
文献类型 | 期刊论文 |
条目标识符 | http://ir.nigpas.ac.cn/handle/332004/31903 |
专题 | 中国科学院南京地质古生物研究所 |
通讯作者 | Cui, Huan (崔欢) |
作者单位 | 1.Vrije Univ Brussel, Div Earth Syst Sci, Analyt Environm & Geochem Grp, Brussels, Belgium 2.ET HOME Evolut & Tracers Habitabil Mars & Earth A, Brussels, Belgium 3.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China 4.Univ Maryland, Dept Geol, College Pk, MD 20742 USA 5.Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA 6.Auburn Univ, Dept Geosci, Auburn, AL 36849 USA 7.Saudi Geol Survey, Jeddah, Saudi Arabia 8.Monash Univ, Sch Earth Atmosphere & Environm, Melbourne, Vic, Australia 9.Russian Acad Sci, Paleontol Inst, Moscow, Russia 10.Museum Victoria, Palaeontol Dept, Melbourne, Vic, Australia |
第一作者单位 | 中国科学院南京地质古生物研究所 |
通讯作者单位 | 中国科学院南京地质古生物研究所 |
推荐引用方式 GB/T 7714 | Cui, Huan ,Kaufman, Alan J.,Zou, Haibo,et al. Primary or secondary? A dichotomy of the strontium isotope anomalies in the Ediacaran carbonates of Saudi Arabia[J]. PRECAMBRIAN RESEARCH,2020,343:24. |
APA | Cui, Huan .,Kaufman, Alan J..,Zou, Haibo.,Kattan, Fayek H..,Trusler, Peter.,...&Vickers-Rich, Patricia.(2020).Primary or secondary? A dichotomy of the strontium isotope anomalies in the Ediacaran carbonates of Saudi Arabia.PRECAMBRIAN RESEARCH,343,24. |
MLA | Cui, Huan ,et al."Primary or secondary? A dichotomy of the strontium isotope anomalies in the Ediacaran carbonates of Saudi Arabia".PRECAMBRIAN RESEARCH 343(2020):24. |
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