Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron

Magnetotactic bacteria intracellularly biomineralize magnetite of an ideal grain size for recording palaeomagnetic signals. However, bacterial magnetite has only been reported in a few pre-Quaternary records because progressive burial into anoxic diagenetic environments causes its dissolution. Deep-...

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Published in:Earth and Planetary Science Letters
Main Authors: A. P. Roberts, F. Florindo, G. Villa, L. Chang, L. Jovane, S. Bohaty, J. C. Larrasoaña, D. Heslop, J. Fitz Gerald
Other Authors: Roberts, A. P., Florindo, F., Villa, G., Chang, L., Jovane, L., Bohaty, S., Larrasoaña, J. C., Heslop, D., Fitz Gerald, J.
Format: Article in Journal/Newspaper
Language:English
Published: 2011
Subjects:
Online Access:http://hdl.handle.net/11381/2368099
https://doi.org/10.1016/j.epsl.2011.08.011
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spelling ftunivparmairis:oai:air.unipr.it:11381/2368099 2024-04-21T08:12:15+00:00 Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron A. P. Roberts F. Florindo G. Villa L. Chang L. Jovane S. Bohaty J. C. Larrasoaña D. Heslop J. Fitz Gerald Roberts, A. P. Florindo, F. Villa, G. Chang, L. Jovane, L. Bohaty, S. Larrasoaña, J. C. Heslop, D. Fitz Gerald, J. 2011 http://hdl.handle.net/11381/2368099 https://doi.org/10.1016/j.epsl.2011.08.011 eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000298273500029 volume:310 firstpage:441 lastpage:452 numberofpages:12 journal:EARTH AND PLANETARY SCIENCE LETTERS http://hdl.handle.net/11381/2368099 doi:10.1016/j.epsl.2011.08.011 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-80053381935 info:eu-repo/semantics/closedAccess info:eu-repo/semantics/article 2011 ftunivparmairis https://doi.org/10.1016/j.epsl.2011.08.011 2024-03-28T01:17:50Z Magnetotactic bacteria intracellularly biomineralize magnetite of an ideal grain size for recording palaeomagnetic signals. However, bacterial magnetite has only been reported in a few pre-Quaternary records because progressive burial into anoxic diagenetic environments causes its dissolution. Deep-sea carbonate sequences provide optimal environments for preserving bacterial magnetite due to low rates of organic carbon burial and expanded pore-water redox zonations. Such sequences often do not become anoxic for tens to hundreds of metres below the seafloor. Nevertheless, the biogeochemical factors that control magnetotactic bacterial populations in such settings are not well known. We document the preservation of bacterial magnetite, which dominates the palaeomagnetic signal throughout Eocene pelagic carbonates from the southern Kerguelen Plateau, Southern Ocean. We provide evidence that iron fertilization, associated with increased aeolian dust flux, resulted in surface water eutrophication in the late Eocene that controlled bacterial magnetite abundance via export of organic carbon to the seafloor. Increased flux of aeolian ironbearing phases also delivered iron to the seafloor, some of which became bioavailable through iron reduction. Our results suggest that magnetotactic bacterial populations in pelagic settings depend crucially on particulate iron and organic carbon delivery to the seafloor. Article in Journal/Newspaper Southern Ocean Archivio della ricerca dell'Università di Parma (CINECA IRIS) Earth and Planetary Science Letters 310 3-4 441 452
institution Open Polar
collection Archivio della ricerca dell'Università di Parma (CINECA IRIS)
op_collection_id ftunivparmairis
language English
description Magnetotactic bacteria intracellularly biomineralize magnetite of an ideal grain size for recording palaeomagnetic signals. However, bacterial magnetite has only been reported in a few pre-Quaternary records because progressive burial into anoxic diagenetic environments causes its dissolution. Deep-sea carbonate sequences provide optimal environments for preserving bacterial magnetite due to low rates of organic carbon burial and expanded pore-water redox zonations. Such sequences often do not become anoxic for tens to hundreds of metres below the seafloor. Nevertheless, the biogeochemical factors that control magnetotactic bacterial populations in such settings are not well known. We document the preservation of bacterial magnetite, which dominates the palaeomagnetic signal throughout Eocene pelagic carbonates from the southern Kerguelen Plateau, Southern Ocean. We provide evidence that iron fertilization, associated with increased aeolian dust flux, resulted in surface water eutrophication in the late Eocene that controlled bacterial magnetite abundance via export of organic carbon to the seafloor. Increased flux of aeolian ironbearing phases also delivered iron to the seafloor, some of which became bioavailable through iron reduction. Our results suggest that magnetotactic bacterial populations in pelagic settings depend crucially on particulate iron and organic carbon delivery to the seafloor.
author2 Roberts, A. P.
Florindo, F.
Villa, G.
Chang, L.
Jovane, L.
Bohaty, S.
Larrasoaña, J. C.
Heslop, D.
Fitz Gerald, J.
format Article in Journal/Newspaper
author A. P. Roberts
F. Florindo
G. Villa
L. Chang
L. Jovane
S. Bohaty
J. C. Larrasoaña
D. Heslop
J. Fitz Gerald
spellingShingle A. P. Roberts
F. Florindo
G. Villa
L. Chang
L. Jovane
S. Bohaty
J. C. Larrasoaña
D. Heslop
J. Fitz Gerald
Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron
author_facet A. P. Roberts
F. Florindo
G. Villa
L. Chang
L. Jovane
S. Bohaty
J. C. Larrasoaña
D. Heslop
J. Fitz Gerald
author_sort A. P. Roberts
title Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron
title_short Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron
title_full Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron
title_fullStr Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron
title_full_unstemmed Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron
title_sort magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron
publishDate 2011
url http://hdl.handle.net/11381/2368099
https://doi.org/10.1016/j.epsl.2011.08.011
genre Southern Ocean
genre_facet Southern Ocean
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000298273500029
volume:310
firstpage:441
lastpage:452
numberofpages:12
journal:EARTH AND PLANETARY SCIENCE LETTERS
http://hdl.handle.net/11381/2368099
doi:10.1016/j.epsl.2011.08.011
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-80053381935
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1016/j.epsl.2011.08.011
container_title Earth and Planetary Science Letters
container_volume 310
container_issue 3-4
container_start_page 441
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