Cargando…

The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions

In modern environments, pore water geochemistry and modelling simulations allow the study of methane (CH(4)) sources and sinks at any geographic location. However, reconstructing CH(4) dynamics in geological records is challenging. Here, we show that the benthic foraminiferal δ(34)S can be used to r...

Descripción completa

Detalles Bibliográficos
Autores principales: Borrelli, C., Gabitov, R. I., Liu, M.-C., Hertwig, A. T., Panieri, G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6987089/
https://www.ncbi.nlm.nih.gov/pubmed/31992778
http://dx.doi.org/10.1038/s41598-020-58353-4
_version_ 1783492073161228288
author Borrelli, C.
Gabitov, R. I.
Liu, M.-C.
Hertwig, A. T.
Panieri, G.
author_facet Borrelli, C.
Gabitov, R. I.
Liu, M.-C.
Hertwig, A. T.
Panieri, G.
author_sort Borrelli, C.
collection PubMed
description In modern environments, pore water geochemistry and modelling simulations allow the study of methane (CH(4)) sources and sinks at any geographic location. However, reconstructing CH(4) dynamics in geological records is challenging. Here, we show that the benthic foraminiferal δ(34)S can be used to reconstruct the flux (i.e., diffusive vs. advective) and timing of CH(4) emissions in fossil records. We measured the δ(34)S of Cassidulina neoteretis specimens from selected samples collected at Vestnesa Ridge, a methane cold seep site in the Arctic Ocean. Our results show lower benthic foraminiferal δ(34)S values (∼20‰) in the sample characterized by seawater conditions, whereas higher values (∼25–27‰) were measured in deeper samples as a consequence of the presence of past sulphate-methane transition zones. The correlation between δ(34)S and the bulk benthic foraminiferal δ(13)C supports this interpretation, whereas the foraminiferal δ(18)O-δ(34)S correlation indicates CH(4) advection at the studied site during the Early Holocene and the Younger-Dryas – post-Bølling. This study highlights the potential of the benthic foraminiferal δ(34)S as a novel tool to reconstruct the flux of CH(4) emissions in geological records and to indirectly date fossil seeps.
format Online
Article
Text
id pubmed-6987089
institution National Center for Biotechnology Information
language English
publishDate 2020
publisher Nature Publishing Group UK
record_format MEDLINE/PubMed
spelling pubmed-69870892020-01-31 The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions Borrelli, C. Gabitov, R. I. Liu, M.-C. Hertwig, A. T. Panieri, G. Sci Rep Article In modern environments, pore water geochemistry and modelling simulations allow the study of methane (CH(4)) sources and sinks at any geographic location. However, reconstructing CH(4) dynamics in geological records is challenging. Here, we show that the benthic foraminiferal δ(34)S can be used to reconstruct the flux (i.e., diffusive vs. advective) and timing of CH(4) emissions in fossil records. We measured the δ(34)S of Cassidulina neoteretis specimens from selected samples collected at Vestnesa Ridge, a methane cold seep site in the Arctic Ocean. Our results show lower benthic foraminiferal δ(34)S values (∼20‰) in the sample characterized by seawater conditions, whereas higher values (∼25–27‰) were measured in deeper samples as a consequence of the presence of past sulphate-methane transition zones. The correlation between δ(34)S and the bulk benthic foraminiferal δ(13)C supports this interpretation, whereas the foraminiferal δ(18)O-δ(34)S correlation indicates CH(4) advection at the studied site during the Early Holocene and the Younger-Dryas – post-Bølling. This study highlights the potential of the benthic foraminiferal δ(34)S as a novel tool to reconstruct the flux of CH(4) emissions in geological records and to indirectly date fossil seeps. Nature Publishing Group UK 2020-01-28 /pmc/articles/PMC6987089/ /pubmed/31992778 http://dx.doi.org/10.1038/s41598-020-58353-4 Text en © The Author(s) 2020 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 license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license 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 license, visit http://creativecommons.org/licenses/by/4.0/.
spellingShingle Article
Borrelli, C.
Gabitov, R. I.
Liu, M.-C.
Hertwig, A. T.
Panieri, G.
The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions
title The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions
title_full The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions
title_fullStr The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions
title_full_unstemmed The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions
title_short The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions
title_sort benthic foraminiferal δ(34)s records flux and timing of paleo methane emissions
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6987089/
https://www.ncbi.nlm.nih.gov/pubmed/31992778
http://dx.doi.org/10.1038/s41598-020-58353-4
work_keys_str_mv AT borrellic thebenthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT gabitovri thebenthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT liumc thebenthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT hertwigat thebenthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT panierig thebenthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT borrellic benthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT gabitovri benthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT liumc benthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT hertwigat benthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions
AT panierig benthicforaminiferald34srecordsfluxandtimingofpaleomethaneemissions