Magnetic analyses of ODP Hole 119-738B sediments ...
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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ftdatacite:10.1594/pangaea.788624 2024-09-15T18:37:14+00:00 Magnetic analyses of ODP Hole 119-738B sediments ... Roberts, Andrew P Florindo, Fabio Villa, Giuliana Chang, Liao Jovane, Luigi Bohaty, Steven M Larrasoaña, Juan C Heslop, David Fitz Gerald, John D 2011 application/zip https://dx.doi.org/10.1594/pangaea.788624 https://doi.pangaea.de/10.1594/PANGAEA.788624 en eng PANGAEA https://dx.doi.org/10.1016/j.epsl.2011.08.011 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2011 ftdatacite https://doi.org/10.1594/pangaea.78862410.1016/j.epsl.2011.08.011 2024-08-01T10:57:37Z 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 ... : Supplement to: Roberts, Andrew P; Florindo, Fabio; Villa, Giuliana; Chang, Liao; Jovane, Luigi; Bohaty, Steven M; Larrasoaña, Juan C; Heslop, David; Fitz Gerald, John D (2011): Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron. Earth and Planetary Science Letters, 310(3-4), 441-452 ... Article in Journal/Newspaper Southern Ocean DataCite |
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Open Polar |
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ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP Roberts, Andrew P Florindo, Fabio Villa, Giuliana Chang, Liao Jovane, Luigi Bohaty, Steven M Larrasoaña, Juan C Heslop, David Fitz Gerald, John D Magnetic analyses of ODP Hole 119-738B sediments ... |
topic_facet |
Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP |
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 ... : Supplement to: Roberts, Andrew P; Florindo, Fabio; Villa, Giuliana; Chang, Liao; Jovane, Luigi; Bohaty, Steven M; Larrasoaña, Juan C; Heslop, David; Fitz Gerald, John D (2011): Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron. Earth and Planetary Science Letters, 310(3-4), 441-452 ... |
format |
Article in Journal/Newspaper |
author |
Roberts, Andrew P Florindo, Fabio Villa, Giuliana Chang, Liao Jovane, Luigi Bohaty, Steven M Larrasoaña, Juan C Heslop, David Fitz Gerald, John D |
author_facet |
Roberts, Andrew P Florindo, Fabio Villa, Giuliana Chang, Liao Jovane, Luigi Bohaty, Steven M Larrasoaña, Juan C Heslop, David Fitz Gerald, John D |
author_sort |
Roberts, Andrew P |
title |
Magnetic analyses of ODP Hole 119-738B sediments ... |
title_short |
Magnetic analyses of ODP Hole 119-738B sediments ... |
title_full |
Magnetic analyses of ODP Hole 119-738B sediments ... |
title_fullStr |
Magnetic analyses of ODP Hole 119-738B sediments ... |
title_full_unstemmed |
Magnetic analyses of ODP Hole 119-738B sediments ... |
title_sort |
magnetic analyses of odp hole 119-738b sediments ... |
publisher |
PANGAEA |
publishDate |
2011 |
url |
https://dx.doi.org/10.1594/pangaea.788624 https://doi.pangaea.de/10.1594/PANGAEA.788624 |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
https://dx.doi.org/10.1016/j.epsl.2011.08.011 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.78862410.1016/j.epsl.2011.08.011 |
_version_ |
1810481594609172480 |