Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts
Hydrogenetic ferromanganese crusts are considered a faithful record of the isotopic composition of seawater influenced by weathering processes of continental masses. Given their ubiquitous presence in all oceans of the planet at depths of 400–7000 meters, they form one of the most well-distributed a...
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ftsouthampton:oai:eprints.soton.ac.uk:449607 2023-08-27T04:11:05+02:00 Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts Josso, Pierre van Peer, Tim Horstwood, Matthew S.A. Lusty, Paul Murton, Bramley 2021-01-01 https://eprints.soton.ac.uk/449607/ English eng Josso, Pierre, van Peer, Tim, Horstwood, Matthew S.A., Lusty, Paul and Murton, Bramley (2021) Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts. Earth and Planetary Science Letters, 553, [116651]. (doi:10.1016/j.epsl.2020.116651 <http://dx.doi.org/10.1016/j.epsl.2020.116651>). Article PeerReviewed 2021 ftsouthampton https://doi.org/10.1016/j.epsl.2020.116651 2023-08-03T22:25:17Z Hydrogenetic ferromanganese crusts are considered a faithful record of the isotopic composition of seawater influenced by weathering processes of continental masses. Given their ubiquitous presence in all oceans of the planet at depths of 400–7000 meters, they form one of the most well-distributed and accessible records of water-mass mixing and climate. However, their slow accumulation rate and poor age constraints have to date limited their use to explore 100 ka paleoclimatic phenomena. Here it is shown how the Pb isotope signature and major element content of a Fe-Mn crust from the north-east Atlantic responded to changes in the intensity and geographic extent of monsoonal rainfall over West Africa, as controlled by climatic precession during the Paleocene. The studied high-spatial resolution (4 μm) laser-ablation multi-collector inductively coupled plasma mass spectrometer (LA-MC-ICP-MS) Pb isotope data is a nearly 2 order of magnitude improvement in spatial and temporal resolution compared to micro-drill subsamples. The record demonstrates cyclicity of the 206 Pb/ 204 Pb and 208, 207 Pb/ 206 Pb ratios at the scale of single Fe-Mn oxide laminae, in conjunction with variations in the Fe/Mn ratio, Al, Si and Ti content. Time-frequency analysis and astronomical tuning of the Pb isotope data demonstrates the imprint of climatic precession (∼20 ka) modulated by eccentricity (∼100 and 405 ka), yielding growth rates of 1.5–3.5 mm/Ma consistent with previous chemostratigraphic age models. In this context, boreal summer at the perihelion causes stronger insolation over West Africa, resulting in more intense and geographically extended monsoonal rainfalls compared to aphelion boreal summer conditions. This, in turn, influences the balance between the weathering endmembers feeding the north-east Atlantic basin. These results provide a new approach for calibrating Fe-Mn crust records to astronomical solutions, and allow their isotopic and chemical archive to be exploited with an improved temporal resolution of 1000–5000 ... Article in Journal/Newspaper North East Atlantic University of Southampton: e-Prints Soton Earth and Planetary Science Letters 553 116651 |
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Open Polar |
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University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
English |
description |
Hydrogenetic ferromanganese crusts are considered a faithful record of the isotopic composition of seawater influenced by weathering processes of continental masses. Given their ubiquitous presence in all oceans of the planet at depths of 400–7000 meters, they form one of the most well-distributed and accessible records of water-mass mixing and climate. However, their slow accumulation rate and poor age constraints have to date limited their use to explore 100 ka paleoclimatic phenomena. Here it is shown how the Pb isotope signature and major element content of a Fe-Mn crust from the north-east Atlantic responded to changes in the intensity and geographic extent of monsoonal rainfall over West Africa, as controlled by climatic precession during the Paleocene. The studied high-spatial resolution (4 μm) laser-ablation multi-collector inductively coupled plasma mass spectrometer (LA-MC-ICP-MS) Pb isotope data is a nearly 2 order of magnitude improvement in spatial and temporal resolution compared to micro-drill subsamples. The record demonstrates cyclicity of the 206 Pb/ 204 Pb and 208, 207 Pb/ 206 Pb ratios at the scale of single Fe-Mn oxide laminae, in conjunction with variations in the Fe/Mn ratio, Al, Si and Ti content. Time-frequency analysis and astronomical tuning of the Pb isotope data demonstrates the imprint of climatic precession (∼20 ka) modulated by eccentricity (∼100 and 405 ka), yielding growth rates of 1.5–3.5 mm/Ma consistent with previous chemostratigraphic age models. In this context, boreal summer at the perihelion causes stronger insolation over West Africa, resulting in more intense and geographically extended monsoonal rainfalls compared to aphelion boreal summer conditions. This, in turn, influences the balance between the weathering endmembers feeding the north-east Atlantic basin. These results provide a new approach for calibrating Fe-Mn crust records to astronomical solutions, and allow their isotopic and chemical archive to be exploited with an improved temporal resolution of 1000–5000 ... |
format |
Article in Journal/Newspaper |
author |
Josso, Pierre van Peer, Tim Horstwood, Matthew S.A. Lusty, Paul Murton, Bramley |
spellingShingle |
Josso, Pierre van Peer, Tim Horstwood, Matthew S.A. Lusty, Paul Murton, Bramley Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts |
author_facet |
Josso, Pierre van Peer, Tim Horstwood, Matthew S.A. Lusty, Paul Murton, Bramley |
author_sort |
Josso, Pierre |
title |
Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts |
title_short |
Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts |
title_full |
Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts |
title_fullStr |
Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts |
title_full_unstemmed |
Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts |
title_sort |
geochemical evidence of milankovitch cycles in atlantic ocean ferromanganese crusts |
publishDate |
2021 |
url |
https://eprints.soton.ac.uk/449607/ |
genre |
North East Atlantic |
genre_facet |
North East Atlantic |
op_relation |
Josso, Pierre, van Peer, Tim, Horstwood, Matthew S.A., Lusty, Paul and Murton, Bramley (2021) Geochemical evidence of Milankovitch cycles in Atlantic Ocean ferromanganese crusts. Earth and Planetary Science Letters, 553, [116651]. (doi:10.1016/j.epsl.2020.116651 <http://dx.doi.org/10.1016/j.epsl.2020.116651>). |
op_doi |
https://doi.org/10.1016/j.epsl.2020.116651 |
container_title |
Earth and Planetary Science Letters |
container_volume |
553 |
container_start_page |
116651 |
_version_ |
1775353554200952832 |