Relationships between Abyssal Redox Conditions and Rock Magnetic Properties of Surficial Sediments in the Western Pacific

Reconstructing changes in deep/bottom-water redox conditions are critical for understanding the role of the deep ocean in global carbon and metals cycling; nevertheless, the quantitative relationships between redox proxies and abyssal dissolved oxygen are poorly investigated. In this work, we studie...

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Main Authors: Yanping Chen, Dong Xu, Huafeng Qin, Geng Liu, Yibing Li, Weiwei Chen, Liang Yi
Format: Article
Language:English
Published: MDPI AG 2023-05-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/11/6/1132
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author Yanping Chen
Dong Xu
Huafeng Qin
Geng Liu
Yibing Li
Weiwei Chen
Liang Yi
author_facet Yanping Chen
Dong Xu
Huafeng Qin
Geng Liu
Yibing Li
Weiwei Chen
Liang Yi
author_sort Yanping Chen
collection DOAJ
description Reconstructing changes in deep/bottom-water redox conditions are critical for understanding the role of the deep ocean in global carbon and metals cycling; nevertheless, the quantitative relationships between redox proxies and abyssal dissolved oxygen are poorly investigated. In this work, we studied the rock magnetic properties of surficial sediments in the western Pacific to investigate their relationship with regional redox conditions. Our results reveal a consistent sedimentary magnetic mineral assemblage in the western Pacific, dominated by pseudo-single-domain magnetite (Fe<sub>3</sub>O<sub>4</sub>), while the ratio of detrital and biogenic magnetite particles in different sites varies substantially. Detailed analyses identified two major magnetic-coercivity components, with modal coercivity values of 13.1 ± 1.6 mT and 54.7 ± 5.3 mT, respectively. All the magnetic parameters we measured, including both concentration-dependent and grainsize-dependent parameters, and the magnetic coercivities, are generally correlated to sedimentary redox conditions; however, the coercivities obtained by mathematical unmixing exhibit a stronger linkage, explaining about a quarter of variance of redox changes. Our findings confirm the potential of magnetic properties for tracing abyssal redox changes in the western Pacific, while the observed magnetic-redox relationships are complex and need further investigation.
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spelling doaj.art-f5d5902f642049c5a62c4066f60e29ef2023-11-18T11:06:20ZengMDPI AGJournal of Marine Science and Engineering2077-13122023-05-01116113210.3390/jmse11061132Relationships between Abyssal Redox Conditions and Rock Magnetic Properties of Surficial Sediments in the Western PacificYanping Chen0Dong Xu1Huafeng Qin2Geng Liu3Yibing Li4Weiwei Chen5Liang Yi6Zhejiang Academy of Marine Sciences, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, ChinaMNR Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, ChinaState Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaState Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaState Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, ChinaState Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, ChinaState Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, ChinaReconstructing changes in deep/bottom-water redox conditions are critical for understanding the role of the deep ocean in global carbon and metals cycling; nevertheless, the quantitative relationships between redox proxies and abyssal dissolved oxygen are poorly investigated. In this work, we studied the rock magnetic properties of surficial sediments in the western Pacific to investigate their relationship with regional redox conditions. Our results reveal a consistent sedimentary magnetic mineral assemblage in the western Pacific, dominated by pseudo-single-domain magnetite (Fe<sub>3</sub>O<sub>4</sub>), while the ratio of detrital and biogenic magnetite particles in different sites varies substantially. Detailed analyses identified two major magnetic-coercivity components, with modal coercivity values of 13.1 ± 1.6 mT and 54.7 ± 5.3 mT, respectively. All the magnetic parameters we measured, including both concentration-dependent and grainsize-dependent parameters, and the magnetic coercivities, are generally correlated to sedimentary redox conditions; however, the coercivities obtained by mathematical unmixing exhibit a stronger linkage, explaining about a quarter of variance of redox changes. Our findings confirm the potential of magnetic properties for tracing abyssal redox changes in the western Pacific, while the observed magnetic-redox relationships are complex and need further investigation.https://www.mdpi.com/2077-1312/11/6/1132deep-sea sedimentsmagnetic propertiesmagnetic coercivityredox changeswestern Pacific
spellingShingle Yanping Chen
Dong Xu
Huafeng Qin
Geng Liu
Yibing Li
Weiwei Chen
Liang Yi
Relationships between Abyssal Redox Conditions and Rock Magnetic Properties of Surficial Sediments in the Western Pacific
Journal of Marine Science and Engineering
deep-sea sediments
magnetic properties
magnetic coercivity
redox changes
western Pacific
title Relationships between Abyssal Redox Conditions and Rock Magnetic Properties of Surficial Sediments in the Western Pacific
title_full Relationships between Abyssal Redox Conditions and Rock Magnetic Properties of Surficial Sediments in the Western Pacific
title_fullStr Relationships between Abyssal Redox Conditions and Rock Magnetic Properties of Surficial Sediments in the Western Pacific
title_full_unstemmed Relationships between Abyssal Redox Conditions and Rock Magnetic Properties of Surficial Sediments in the Western Pacific
title_short Relationships between Abyssal Redox Conditions and Rock Magnetic Properties of Surficial Sediments in the Western Pacific
title_sort relationships between abyssal redox conditions and rock magnetic properties of surficial sediments in the western pacific
topic deep-sea sediments
magnetic properties
magnetic coercivity
redox changes
western Pacific
url https://www.mdpi.com/2077-1312/11/6/1132
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