Ecosystem changes after Early Cretaceous seawater intrusion into the proto-South Atlantic Ocean

Abstract The early evolution of the South Atlantic Ocean following the Cretaceous break-up of Gondwana is extensively recorded in rift basins along the conjugate margins of Africa and Brazil. For the Brazil side, divergent views of the source and pathway of the initial seawater incursion persist due...

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Main Authors: Jian Ma, Leonardo F. Cury, Anelize M. B. Rumbelsperger, Heidi L. Albrecht, Erwin W. Adams, Joachim E. Amthor, Xingqian Cui, Antoine Crémière, Kei Sato, Kristin D. Bergmann, Roger E. Summons
Format: Article
Language:English
Published: Nature Portfolio 2025-01-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02029-2
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author Jian Ma
Leonardo F. Cury
Anelize M. B. Rumbelsperger
Heidi L. Albrecht
Erwin W. Adams
Joachim E. Amthor
Xingqian Cui
Antoine Crémière
Kei Sato
Kristin D. Bergmann
Roger E. Summons
author_facet Jian Ma
Leonardo F. Cury
Anelize M. B. Rumbelsperger
Heidi L. Albrecht
Erwin W. Adams
Joachim E. Amthor
Xingqian Cui
Antoine Crémière
Kei Sato
Kristin D. Bergmann
Roger E. Summons
author_sort Jian Ma
collection DOAJ
description Abstract The early evolution of the South Atlantic Ocean following the Cretaceous break-up of Gondwana is extensively recorded in rift basins along the conjugate margins of Africa and Brazil. For the Brazil side, divergent views of the source and pathway of the initial seawater incursion persist due to a paucity of recognized transitional sequences that document marine transgressive deposits over the continental interior. To address this, we conducted a high-resolution sedimentological and geochemical study through a core in the Campos Basin that encompasses the key lithologic switch from lacustrine carbonate to marine evaporite settings. Steroid lipid biomarkers, derived from pelagophyte marine algae, make a striking appearance in concert with a pronounced negative shift of 87Sr/86Sr ratios and coincident with the appearance of anhydrite. Importantly, the sulfur-sequestered biomarkers reveal a dynamic system where redox-stratified and anoxic conditions were amplified along with a deepening chemocline through the marine transition.
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spelling doaj-art-d4a5de1ea1134b1f870b2ad3e6f2b4a12025-01-26T12:54:07ZengNature PortfolioCommunications Earth & Environment2662-44352025-01-016111010.1038/s43247-025-02029-2Ecosystem changes after Early Cretaceous seawater intrusion into the proto-South Atlantic OceanJian Ma0Leonardo F. Cury1Anelize M. B. Rumbelsperger2Heidi L. Albrecht3Erwin W. Adams4Joachim E. Amthor5Xingqian Cui6Antoine Crémière7Kei Sato8Kristin D. Bergmann9Roger E. Summons10Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of TechnologyFederal University of Paraná, LAMIR InstituteFederal University of Paraná, LAMIR InstituteShell Exploration and Production CompanyShell Global Solutions International BVDivision of Earth Sciences and Geography, Rhine-Westphalia Technical University of AachenSchool of Oceanography, Shanghai Jiao Tong UniversityDivision of Geological and Planetary Sciences, California Institute of TechnologySão Paulo UniversityDepartment of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of TechnologyDepartment of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of TechnologyAbstract The early evolution of the South Atlantic Ocean following the Cretaceous break-up of Gondwana is extensively recorded in rift basins along the conjugate margins of Africa and Brazil. For the Brazil side, divergent views of the source and pathway of the initial seawater incursion persist due to a paucity of recognized transitional sequences that document marine transgressive deposits over the continental interior. To address this, we conducted a high-resolution sedimentological and geochemical study through a core in the Campos Basin that encompasses the key lithologic switch from lacustrine carbonate to marine evaporite settings. Steroid lipid biomarkers, derived from pelagophyte marine algae, make a striking appearance in concert with a pronounced negative shift of 87Sr/86Sr ratios and coincident with the appearance of anhydrite. Importantly, the sulfur-sequestered biomarkers reveal a dynamic system where redox-stratified and anoxic conditions were amplified along with a deepening chemocline through the marine transition.https://doi.org/10.1038/s43247-025-02029-2
spellingShingle Jian Ma
Leonardo F. Cury
Anelize M. B. Rumbelsperger
Heidi L. Albrecht
Erwin W. Adams
Joachim E. Amthor
Xingqian Cui
Antoine Crémière
Kei Sato
Kristin D. Bergmann
Roger E. Summons
Ecosystem changes after Early Cretaceous seawater intrusion into the proto-South Atlantic Ocean
Communications Earth & Environment
title Ecosystem changes after Early Cretaceous seawater intrusion into the proto-South Atlantic Ocean
title_full Ecosystem changes after Early Cretaceous seawater intrusion into the proto-South Atlantic Ocean
title_fullStr Ecosystem changes after Early Cretaceous seawater intrusion into the proto-South Atlantic Ocean
title_full_unstemmed Ecosystem changes after Early Cretaceous seawater intrusion into the proto-South Atlantic Ocean
title_short Ecosystem changes after Early Cretaceous seawater intrusion into the proto-South Atlantic Ocean
title_sort ecosystem changes after early cretaceous seawater intrusion into the proto south atlantic ocean
url https://doi.org/10.1038/s43247-025-02029-2
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