Article (Scientific journals)
An authigenic response to Ediacaran surface oxidation: Remarkable micron-scale isotopic heterogeneity revealed by SIMS
Cui, Huan; Kitajima, Kouki; Orland, Ian J. et al.
2022In Precambrian Research, 377, p. 106676
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Keywords :
Anaerobic oxidation of methane; Authigenic carbonate; Carbon isotopes; Deep-time carbon cycle; Microbial sulfate reduction; Secondary ion mass spectrometry; Shuram excursion; Geology; Geochemistry and Petrology
Abstract :
[en] The Ediacaran Shuram excursion (SE) records a global decrease in carbonate carbon isotope (δ13Ccarb) values from +6‰ down to ca. –10‰, representing the largest δ13Ccarb negative anomaly in Earth history. While the SE is widely recorded in the upper Doushantuo Formation of South China, it shows highly variable δ13Ccarb profiles among correlative sections. This inconsistent expression of the SE challenges the conventional view of a homogeneous marine dissolved inorganic carbon (DIC) reservoir. A potential process that could explain δ13Ccarb variability is local mineralization of isotopically distinct authigenic carbonates near the sediment–water interface during early diagenesis. However, a direct test of such authigenic carbonates is still limited. Here, following a recent study on the SE in an intra-shelf environment, we revisited an outer-shelf section, identified and analyzed μm-scale, syn-depositional authigenic calcite cements via integrated cathodoluminescence (CL), micro-X-ray fluorescence (μXRF), scanning electron microscope (SEM), energy-dispersive spectroscopy (EDS), and secondary ion mass spectrometry (SIMS). Our new SIMS results reveal remarkable micron-scale heterogeneity of δ13Ccarb in authigenic calcite cements, including extremely negative values down to –37.5‰ (VPDB). We interpret these calcite cements as methane-derived authigenic calcite (MDAC) resulting from microbial sulfate reduction (MSR) and anaerobic oxidation of methane (AOM) during early diagenesis. Based on the new results, we propose that the heterogeneous SE in South China — manifest on micrometer, centimeter, and basinal scales — was modulated by methane oxidation under variable local redox and water depth conditions. The SE, therefore, was coupled with different degrees of methane oxidation in individual basins, and globally triggered by enhanced seawater sulfate during an atmospheric oxygenation event. In light of this study, the potential role of redox variability in methane oxidation during the SE may have been underestimated. Our study demonstrates that integrated SIMS-SEM analysis can distinguish different generations of isotopically distinct carbonates otherwise undetected by conventional analysis, and is thus an effective approach to assess the origin and diagenetic history of δ13Ccarb anomalies in the sedimentary record.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Cui, Huan;  Equipe Géomicrobiologie, Institut de Physique du Globe de Paris (IPGP), université Paris Cité, Paris, France ; Stable Isotope Laboratory, Department of Earth Sciences, University of Toronto, Toronto, Canada ; NASA Astrobiology Institute, University of Wisconsin–Madison, Madison, United States ; Department of Geoscience, University of Wisconsin–Madison, Madison, United States
Kitajima, Kouki;  Department of Geoscience, University of Wisconsin–Madison, Madison, United States
Orland, Ian J.;  Department of Geoscience, University of Wisconsin–Madison, Madison, United States ; Wisconsin Geological and Natural History Survey, University of Wisconsin–Madison, Madison, United States
Baele, Jean-Marc  ;  Université de Mons - UMONS
Xiao, Shuhai;  Department of Geosciences, Virginia Tech, Blacksburg, United States
Kaufman, Alan J.;  Department of Geology and Earth System Science Interdisciplinary Center, University of Maryland, College Park, United States
Denny, Adam;  Department of Geoscience, University of Wisconsin–Madison, Madison, United States ; Pacific Northwest National Laboratory, Richland, United States
Spicuzza, Michael J.;  Department of Geoscience, University of Wisconsin–Madison, Madison, United States
Fournelle, John H.;  Department of Geoscience, University of Wisconsin–Madison, Madison, United States
Valley, John W.;  NASA Astrobiology Institute, University of Wisconsin–Madison, Madison, United States ; Department of Geoscience, University of Wisconsin–Madison, Madison, United States
Language :
English
Title :
An authigenic response to Ediacaran surface oxidation: Remarkable micron-scale isotopic heterogeneity revealed by SIMS
Publication date :
August 2022
Journal title :
Precambrian Research
ISSN :
0301-9268
Publisher :
Elsevier B.V.
Volume :
377
Pages :
106676
Peer reviewed :
Peer Reviewed verified by ORBi
Development Goals :
13. Climate action
Research unit :
F401 - Géologie fondamentale et appliquée
Research institute :
R400 - Institut de Recherche en Science et Ingénierie des Matériaux
Funding text :
This study was supported by the NASA Astrobiology Institute (NNA13AA94A) at UW–Madison. The WiscSIMS Lab is supported by NSF (EAR–1355590, –1658823, –2004618) and UW–Madison. JWV was also supported by NSF (EAR–1524336) and DOE (DE–FG02–93ER14389). SX was supported by NASA Exobiology Program (80NSSC18K1086). HC is grateful for joint support from CIFAR (Canadian Institute for Advanced Research) “Earth 4D: Subsurface Science and Exploration” program at Université Paris Cité and University of Toronto. This paper is dedicated to Yiheng Wu and toddler Ruogu Cui, for the love, peace, and joy during the pandemic in Paris.HC wants to thank Prof. Jianbo Liu (Peking University), who introduced HC the conventional carbon cycle model in his class when HC was a graduate student in Beijing back to over 10 years ago. It was Prof. Liu's course Biogeochemistry and Biomineralization that inspired HC to pursue a Ph.D. in geobiology and biogeochemistry abroad. The authors thank Bil Schneider for assistance in the SEM laboratory at UW-Madison; Brian Hess, Noriko Kita, James Kern, and Maciej Śliwiński for assistance in sample preparation and SIMS analysis at UW-Madison; Huifang Xu for assistance in the microscope laboratory at UW-Madison; Steven Goderis, Niels J. de Winter, and Pim Kaskes for guidance in the μXRF laboratory at VUB; Yiheng Wu for assistance in compiling supplemental materials; Chuanming Zhou (NIGPAS) for field assistance and constructive comments; Ganqing Jiang (UNLV) and Magali Ader (IPGP) for kind discussion. This paper was handled by Frances Westall (CNRS, Orléans) and benefits from constructive reviews by James Busch (Dartmouth), Thomas Algeo (Cincinnati), and three anonymous reviewers. This study was supported by the NASA Astrobiology Institute (NNA13AA94A) at UW–Madison. The WiscSIMS Lab is supported by NSF (EAR–1355590, –1658823, –2004618) and UW–Madison. JWV was also supported by NSF (EAR–1524336) and DOE (DE–FG02–93ER14389). SX was supported by NASA Exobiology Program (80NSSC18K1086). HC is grateful for joint support from CIFAR (Canadian Institute for Advanced Research) “Earth 4D: Subsurface Science and Exploration” program at Université Paris Cité and University of Toronto. This paper is dedicated to Yiheng Wu and toddler Ruogu Cui, for the love, peace, and joy during the pandemic in Paris.
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