Organic matter in an Ocean Continent Transitions of present-day magma-poor rifted margins: the examples of Iberia and Newfoundland

Abstract: Serpentinisation and concomitant reduction of CO2 to methane at modern hydrothermal vents has been observed to support methanotrophic biosystems at mid-ocean ridges. Exhumation of mantle within ocean regions and its subsequent serpentinisation is a common occurrence. It is possible that me...

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Main Authors: Mateeva, Tsvetomila, Wolff, George A., J. Kusznir, Nick J., Manatschal, Gianreto, Holtvoeth, Jens
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
ODP
Online Access:https://zenodo.org/record/4515471
https://doi.org/10.5281/zenodo.4515471
id ftzenodo:oai:zenodo.org:4515471
record_format openpolar
spelling ftzenodo:oai:zenodo.org:4515471 2023-06-06T11:56:41+02:00 Organic matter in an Ocean Continent Transitions of present-day magma-poor rifted margins: the examples of Iberia and Newfoundland Mateeva, Tsvetomila Wolff, George A. J. Kusznir, Nick J. Manatschal, Gianreto Holtvoeth, Jens 2021-02-07 https://zenodo.org/record/4515471 https://doi.org/10.5281/zenodo.4515471 eng eng doi:10.5281/zenodo.4515470 https://zenodo.org/record/4515471 https://doi.org/10.5281/zenodo.4515471 oai:zenodo.org:4515471 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode serpentinization Iberian margin Newfoundland margin GDGTs ODP methanotroph. Leg 210 leg 149 leg 170 info:eu-repo/semantics/article publication-article 2021 ftzenodo https://doi.org/10.5281/zenodo.451547110.5281/zenodo.4515470 2023-04-13T21:44:42Z Abstract: Serpentinisation and concomitant reduction of CO2 to methane at modern hydrothermal vents has been observed to support methanotrophic biosystems at mid-ocean ridges. Exhumation of mantle within ocean regions and its subsequent serpentinisation is a common occurrence. It is possible that methanotrophy is not restricted to hydrothermal vents systems alone and could be pervasive within serpentinised exhumed oceanic mantle. The ocean-continent transition (OCT) of magma-poor rifted continental margins provides an opportunity to investigate this. Serpentinite, intrusive magmatic rocks and overlying sediments collected as part of the Ocean Drilling Program (ODP) from the Iberian and Newfoundland margin, were analysed to find evidence of methanotrophic archaea related to the serpentinisation process. Samples from the OCT of Newfoundland (ODP Leg 210) contain n-alkanes, PAHs and isoprenoids (pristane, phytane) while those from the OCT of Iberian (ODP Legs 149 and 173) also contained detectable steranes and hopanes. However, the distribution and composition of hydrocarbons suggest that the OM may not be indigenous to the rocks. The only clear evidence of Archaea was provided from GDGTs (0 – 3), crenarchaeol and isomers from one sediment sample at the Iberian Margin and these were likely derived from overlying oceanic waters. Hydrocarbon fingerprinting using polar plots suggests that any organic compounds in the igneous and metamorphic rocks were probably introduced from the drilling mud. All data and raw files available on simple demand. Manuscript and data presented on a conference but never published except in a thesis. Article in Journal/Newspaper Newfoundland Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic serpentinization
Iberian margin
Newfoundland margin
GDGTs
ODP
methanotroph. Leg 210
leg 149
leg 170
spellingShingle serpentinization
Iberian margin
Newfoundland margin
GDGTs
ODP
methanotroph. Leg 210
leg 149
leg 170
Mateeva, Tsvetomila
Wolff, George A.
J. Kusznir, Nick J.
Manatschal, Gianreto
Holtvoeth, Jens
Organic matter in an Ocean Continent Transitions of present-day magma-poor rifted margins: the examples of Iberia and Newfoundland
topic_facet serpentinization
Iberian margin
Newfoundland margin
GDGTs
ODP
methanotroph. Leg 210
leg 149
leg 170
description Abstract: Serpentinisation and concomitant reduction of CO2 to methane at modern hydrothermal vents has been observed to support methanotrophic biosystems at mid-ocean ridges. Exhumation of mantle within ocean regions and its subsequent serpentinisation is a common occurrence. It is possible that methanotrophy is not restricted to hydrothermal vents systems alone and could be pervasive within serpentinised exhumed oceanic mantle. The ocean-continent transition (OCT) of magma-poor rifted continental margins provides an opportunity to investigate this. Serpentinite, intrusive magmatic rocks and overlying sediments collected as part of the Ocean Drilling Program (ODP) from the Iberian and Newfoundland margin, were analysed to find evidence of methanotrophic archaea related to the serpentinisation process. Samples from the OCT of Newfoundland (ODP Leg 210) contain n-alkanes, PAHs and isoprenoids (pristane, phytane) while those from the OCT of Iberian (ODP Legs 149 and 173) also contained detectable steranes and hopanes. However, the distribution and composition of hydrocarbons suggest that the OM may not be indigenous to the rocks. The only clear evidence of Archaea was provided from GDGTs (0 – 3), crenarchaeol and isomers from one sediment sample at the Iberian Margin and these were likely derived from overlying oceanic waters. Hydrocarbon fingerprinting using polar plots suggests that any organic compounds in the igneous and metamorphic rocks were probably introduced from the drilling mud. All data and raw files available on simple demand. Manuscript and data presented on a conference but never published except in a thesis.
format Article in Journal/Newspaper
author Mateeva, Tsvetomila
Wolff, George A.
J. Kusznir, Nick J.
Manatschal, Gianreto
Holtvoeth, Jens
author_facet Mateeva, Tsvetomila
Wolff, George A.
J. Kusznir, Nick J.
Manatschal, Gianreto
Holtvoeth, Jens
author_sort Mateeva, Tsvetomila
title Organic matter in an Ocean Continent Transitions of present-day magma-poor rifted margins: the examples of Iberia and Newfoundland
title_short Organic matter in an Ocean Continent Transitions of present-day magma-poor rifted margins: the examples of Iberia and Newfoundland
title_full Organic matter in an Ocean Continent Transitions of present-day magma-poor rifted margins: the examples of Iberia and Newfoundland
title_fullStr Organic matter in an Ocean Continent Transitions of present-day magma-poor rifted margins: the examples of Iberia and Newfoundland
title_full_unstemmed Organic matter in an Ocean Continent Transitions of present-day magma-poor rifted margins: the examples of Iberia and Newfoundland
title_sort organic matter in an ocean continent transitions of present-day magma-poor rifted margins: the examples of iberia and newfoundland
publishDate 2021
url https://zenodo.org/record/4515471
https://doi.org/10.5281/zenodo.4515471
genre Newfoundland
genre_facet Newfoundland
op_relation doi:10.5281/zenodo.4515470
https://zenodo.org/record/4515471
https://doi.org/10.5281/zenodo.4515471
oai:zenodo.org:4515471
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.451547110.5281/zenodo.4515470
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