Cargando…

Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago

The largest negative inorganic carbon isotope excursion in Earth’s history, namely the Ediacaran Shuram Excursion (SE), closely followed by early animal radiation, has been widely interpreted as a consequence of oceanic oxidation. However, the primary nature of the signature, source of oxidants, and...

Descripción completa

Detalles Bibliográficos
Autores principales: Wang, Haiyang, Peng, Yongbo, Li, Chao, Cao, Xiaobin, Cheng, Meng, Bao, Huiming
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10354052/
https://www.ncbi.nlm.nih.gov/pubmed/37463883
http://dx.doi.org/10.1038/s41467-023-39962-9
_version_ 1785074837320892416
author Wang, Haiyang
Peng, Yongbo
Li, Chao
Cao, Xiaobin
Cheng, Meng
Bao, Huiming
author_facet Wang, Haiyang
Peng, Yongbo
Li, Chao
Cao, Xiaobin
Cheng, Meng
Bao, Huiming
author_sort Wang, Haiyang
collection PubMed
description The largest negative inorganic carbon isotope excursion in Earth’s history, namely the Ediacaran Shuram Excursion (SE), closely followed by early animal radiation, has been widely interpreted as a consequence of oceanic oxidation. However, the primary nature of the signature, source of oxidants, and tempo of the event remain contested. Here, we show that carbonate-associated sulfate (CAS) from three different paleocontinents all have conspicuous negative (17)O anomalies (Δ′(17)O(CAS) values down to −0.53‰) during the SE. Furthermore, the Δ′(17)O(CAS) varies in correlation with its corresponding δ(34)S(CAS) and δ(18)O(CAS) as well as the carbonate δ(13)C(carb), decreasing initially followed by a recovery over the ~7-Myr SE duration. In a box-model examination, we argue for a period of sustained water-column ventilation and consequently enhanced sulfur oxidation in the SE ocean. Our findings reveal a direct involvement of mass-anomalously (17)O-depleted atmospheric O(2) in marine sulfate formation and thus a primary global oceanic oxygenation event during the SE.
format Online
Article
Text
id pubmed-10354052
institution National Center for Biotechnology Information
language English
publishDate 2023
publisher Nature Publishing Group UK
record_format MEDLINE/PubMed
spelling pubmed-103540522023-07-20 Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago Wang, Haiyang Peng, Yongbo Li, Chao Cao, Xiaobin Cheng, Meng Bao, Huiming Nat Commun Article The largest negative inorganic carbon isotope excursion in Earth’s history, namely the Ediacaran Shuram Excursion (SE), closely followed by early animal radiation, has been widely interpreted as a consequence of oceanic oxidation. However, the primary nature of the signature, source of oxidants, and tempo of the event remain contested. Here, we show that carbonate-associated sulfate (CAS) from three different paleocontinents all have conspicuous negative (17)O anomalies (Δ′(17)O(CAS) values down to −0.53‰) during the SE. Furthermore, the Δ′(17)O(CAS) varies in correlation with its corresponding δ(34)S(CAS) and δ(18)O(CAS) as well as the carbonate δ(13)C(carb), decreasing initially followed by a recovery over the ~7-Myr SE duration. In a box-model examination, we argue for a period of sustained water-column ventilation and consequently enhanced sulfur oxidation in the SE ocean. Our findings reveal a direct involvement of mass-anomalously (17)O-depleted atmospheric O(2) in marine sulfate formation and thus a primary global oceanic oxygenation event during the SE. Nature Publishing Group UK 2023-07-18 /pmc/articles/PMC10354052/ /pubmed/37463883 http://dx.doi.org/10.1038/s41467-023-39962-9 Text en © The Author(s) 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Wang, Haiyang
Peng, Yongbo
Li, Chao
Cao, Xiaobin
Cheng, Meng
Bao, Huiming
Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago
title Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago
title_full Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago
title_fullStr Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago
title_full_unstemmed Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago
title_short Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago
title_sort sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10354052/
https://www.ncbi.nlm.nih.gov/pubmed/37463883
http://dx.doi.org/10.1038/s41467-023-39962-9
work_keys_str_mv AT wanghaiyang sulfatetripleoxygenisotopeevidenceconfirmingoceanicoxygenation570millionyearsago
AT pengyongbo sulfatetripleoxygenisotopeevidenceconfirmingoceanicoxygenation570millionyearsago
AT lichao sulfatetripleoxygenisotopeevidenceconfirmingoceanicoxygenation570millionyearsago
AT caoxiaobin sulfatetripleoxygenisotopeevidenceconfirmingoceanicoxygenation570millionyearsago
AT chengmeng sulfatetripleoxygenisotopeevidenceconfirmingoceanicoxygenation570millionyearsago
AT baohuiming sulfatetripleoxygenisotopeevidenceconfirmingoceanicoxygenation570millionyearsago