Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals
The distribution of dissolved iodine in seawater is sensitive to multiple biogeochemical cycles, including those of nitrogen and oxygen. The iodine-to-calcium ratio (I/Ca) of marine carbonates, such as bulk carbonate or foraminifera, has emerged as a potential proxy for changes in past seawater oxyg...
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ftdoajarticles:oai:doaj.org/article:27cde835d55740d88cbf05752e9f9963 2023-12-10T09:51:42+01:00 Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals Yun-Ju Sun Laura F. Robinson Ian J. Parkinson Joseph A. Stewart Wanyi Lu Dalton S. Hardisty Qian Liu James Kershaw Michèle LaVigne Tristan J. Horner 2023-11-01T00:00:00Z https://doi.org/10.3389/fmars.2023.1264380 https://doaj.org/article/27cde835d55740d88cbf05752e9f9963 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fmars.2023.1264380/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2023.1264380 https://doaj.org/article/27cde835d55740d88cbf05752e9f9963 Frontiers in Marine Science, Vol 10 (2023) biogenic carbonate iodate incorporation seawater oxygenation proxy dissolved oxygen marine redox state Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2023 ftdoajarticles https://doi.org/10.3389/fmars.2023.1264380 2023-11-12T01:39:42Z The distribution of dissolved iodine in seawater is sensitive to multiple biogeochemical cycles, including those of nitrogen and oxygen. The iodine-to-calcium ratio (I/Ca) of marine carbonates, such as bulk carbonate or foraminifera, has emerged as a potential proxy for changes in past seawater oxygenation. However, the utility of the I/Ca proxy in deep-sea corals, natural archives of seawater chemistry with wide spatial coverage and radiometric dating potential, remains unexplored. Here, we present the first I/Ca data obtained from modern deep-sea corals, specifically scleractinian and bamboo corals, collected from the Atlantic, Eastern Pacific, and Southern Oceans, encompassing a wide range of seawater oxygen concentrations (10–280 μmol/kg). In contrast to thermodynamic predictions, we observe higher I/Ca ratios in aragonitic corals (scleractinian) compared to calcitic corals (bamboo). This observation suggests a strong biological control during iodate incorporation into deep-sea coral skeletons. For the majority of scleractinian corals, I/Ca exhibits a covariation with local seawater iodate concentrations, which is closely related to seawater oxygen content. Scleractinian corals also exhibit notably lower I/Ca below a seawater oxygen threshold of approximately 160 μmol/kg. In contrast, no significant differences in I/Ca are found among bamboo corals across the range of oxygen concentrations encountered (15–240 μmol/kg). In the North Atlantic, several hydrographic factors, such as temperature and/or salinity, may additionally affect coral I/Ca. Our results highlight the potential of I/Ca ratios in deep-sea scleractinian corals to serve as an indicator of past seawater iodate concentrations, providing valuable insights into historical seawater oxygen levels. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Pacific Frontiers in Marine Science 10 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
biogenic carbonate iodate incorporation seawater oxygenation proxy dissolved oxygen marine redox state Science Q General. Including nature conservation geographical distribution QH1-199.5 |
spellingShingle |
biogenic carbonate iodate incorporation seawater oxygenation proxy dissolved oxygen marine redox state Science Q General. Including nature conservation geographical distribution QH1-199.5 Yun-Ju Sun Laura F. Robinson Ian J. Parkinson Joseph A. Stewart Wanyi Lu Dalton S. Hardisty Qian Liu James Kershaw Michèle LaVigne Tristan J. Horner Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals |
topic_facet |
biogenic carbonate iodate incorporation seawater oxygenation proxy dissolved oxygen marine redox state Science Q General. Including nature conservation geographical distribution QH1-199.5 |
description |
The distribution of dissolved iodine in seawater is sensitive to multiple biogeochemical cycles, including those of nitrogen and oxygen. The iodine-to-calcium ratio (I/Ca) of marine carbonates, such as bulk carbonate or foraminifera, has emerged as a potential proxy for changes in past seawater oxygenation. However, the utility of the I/Ca proxy in deep-sea corals, natural archives of seawater chemistry with wide spatial coverage and radiometric dating potential, remains unexplored. Here, we present the first I/Ca data obtained from modern deep-sea corals, specifically scleractinian and bamboo corals, collected from the Atlantic, Eastern Pacific, and Southern Oceans, encompassing a wide range of seawater oxygen concentrations (10–280 μmol/kg). In contrast to thermodynamic predictions, we observe higher I/Ca ratios in aragonitic corals (scleractinian) compared to calcitic corals (bamboo). This observation suggests a strong biological control during iodate incorporation into deep-sea coral skeletons. For the majority of scleractinian corals, I/Ca exhibits a covariation with local seawater iodate concentrations, which is closely related to seawater oxygen content. Scleractinian corals also exhibit notably lower I/Ca below a seawater oxygen threshold of approximately 160 μmol/kg. In contrast, no significant differences in I/Ca are found among bamboo corals across the range of oxygen concentrations encountered (15–240 μmol/kg). In the North Atlantic, several hydrographic factors, such as temperature and/or salinity, may additionally affect coral I/Ca. Our results highlight the potential of I/Ca ratios in deep-sea scleractinian corals to serve as an indicator of past seawater iodate concentrations, providing valuable insights into historical seawater oxygen levels. |
format |
Article in Journal/Newspaper |
author |
Yun-Ju Sun Laura F. Robinson Ian J. Parkinson Joseph A. Stewart Wanyi Lu Dalton S. Hardisty Qian Liu James Kershaw Michèle LaVigne Tristan J. Horner |
author_facet |
Yun-Ju Sun Laura F. Robinson Ian J. Parkinson Joseph A. Stewart Wanyi Lu Dalton S. Hardisty Qian Liu James Kershaw Michèle LaVigne Tristan J. Horner |
author_sort |
Yun-Ju Sun |
title |
Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals |
title_short |
Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals |
title_full |
Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals |
title_fullStr |
Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals |
title_full_unstemmed |
Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals |
title_sort |
iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals |
publisher |
Frontiers Media S.A. |
publishDate |
2023 |
url |
https://doi.org/10.3389/fmars.2023.1264380 https://doaj.org/article/27cde835d55740d88cbf05752e9f9963 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Frontiers in Marine Science, Vol 10 (2023) |
op_relation |
https://www.frontiersin.org/articles/10.3389/fmars.2023.1264380/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2023.1264380 https://doaj.org/article/27cde835d55740d88cbf05752e9f9963 |
op_doi |
https://doi.org/10.3389/fmars.2023.1264380 |
container_title |
Frontiers in Marine Science |
container_volume |
10 |
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1784897465053347840 |