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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Published in:Frontiers in Marine Science
Main Authors: Sun, Yun-Ju, Robinson, Laura F, Parkinson, Ian J, Stewart, Joseph A, Lu, Wanyi, Hardisty, Dalton S, Liu, Qian, Kershaw, James, LaVigne, Michèle, Horner, Tristan J
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://hdl.handle.net/1983/1bac35c3-4b3d-4e69-919f-fb3022ce4fd4
https://research-information.bris.ac.uk/en/publications/1bac35c3-4b3d-4e69-919f-fb3022ce4fd4
https://doi.org/10.3389/fmars.2023.1264380
https://bris.idm.oclc.org/login?url=https://www.proquest.com/scholarly-journals/iodine-calcium-ratios-deep-sea-scleractinian/docview/2886738384/se-2?accountid=9730
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https://bris.on.worldcat.org/atoztitles/link?sid=ProQ:&issn=&volume=&issue=&title=Frontiers+in+Marine+Science&spage=&date=2023-11-07&atitle=Iodine-to-calcium+ratios+in+deep-sea+scleractinian+and+bamboo+corals&au=Sun,+Yun-Ju%3BRobinson,+Laura+F%3BParkinson,+Ian+J%3BStewart,+Joseph+A%3BLu,+Wanyi%3BHardisty,+Dalton+S%3BLiu,+Qian%3BKershaw,+James%3BLaVigne,+Mich%C3%A8le%3BHorner,+Tristan+J&id=doi:10.3389%2Ffmars.2023.1264380
id ftubristolcris:oai:research-information.bris.ac.uk:publications/1bac35c3-4b3d-4e69-919f-fb3022ce4fd4
record_format openpolar
institution Open Polar
collection University of Bristol: Bristol Research
op_collection_id ftubristolcris
language English
topic Earth Sciences--Oceanography
Seawater oxygen1
Iodine2
Deep-sea coral3
Scleractinian coral4
Bamboo coral5
Deep sea
Corals
Seawater
Biogeochemistry
Biological control
Deep water
Geochemistry
Hypoxia
Oxygenation
Archives
Mineralogy
Iodates
Oceans
Museums
Foraminifera
Radiometric dating
Carbonates
Calcium
Iodine
Biogeochemical cycles
Marine invertebrates
Oxidation
Oxygen
Archives & records
Biogeochemical cycle
Southern Ocean
spellingShingle Earth Sciences--Oceanography
Seawater oxygen1
Iodine2
Deep-sea coral3
Scleractinian coral4
Bamboo coral5
Deep sea
Corals
Seawater
Biogeochemistry
Biological control
Deep water
Geochemistry
Hypoxia
Oxygenation
Archives
Mineralogy
Iodates
Oceans
Museums
Foraminifera
Radiometric dating
Carbonates
Calcium
Iodine
Biogeochemical cycles
Marine invertebrates
Oxidation
Oxygen
Archives & records
Biogeochemical cycle
Southern Ocean
Sun, Yun-Ju
Robinson, Laura F
Parkinson, Ian J
Stewart, Joseph A
Lu, Wanyi
Hardisty, Dalton S
Liu, Qian
Kershaw, James
LaVigne, Michèle
Horner, Tristan J
Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals
topic_facet Earth Sciences--Oceanography
Seawater oxygen1
Iodine2
Deep-sea coral3
Scleractinian coral4
Bamboo coral5
Deep sea
Corals
Seawater
Biogeochemistry
Biological control
Deep water
Geochemistry
Hypoxia
Oxygenation
Archives
Mineralogy
Iodates
Oceans
Museums
Foraminifera
Radiometric dating
Carbonates
Calcium
Iodine
Biogeochemical cycles
Marine invertebrates
Oxidation
Oxygen
Archives & records
Biogeochemical cycle
Southern Ocean
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 Sun, Yun-Ju
Robinson, Laura F
Parkinson, Ian J
Stewart, Joseph A
Lu, Wanyi
Hardisty, Dalton S
Liu, Qian
Kershaw, James
LaVigne, Michèle
Horner, Tristan J
author_facet Sun, Yun-Ju
Robinson, Laura F
Parkinson, Ian J
Stewart, Joseph A
Lu, Wanyi
Hardisty, Dalton S
Liu, Qian
Kershaw, James
LaVigne, Michèle
Horner, Tristan J
author_sort Sun, Yun-Ju
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
publishDate 2023
url https://hdl.handle.net/1983/1bac35c3-4b3d-4e69-919f-fb3022ce4fd4
https://research-information.bris.ac.uk/en/publications/1bac35c3-4b3d-4e69-919f-fb3022ce4fd4
https://doi.org/10.3389/fmars.2023.1264380
https://bris.idm.oclc.org/login?url=https://www.proquest.com/scholarly-journals/iodine-calcium-ratios-deep-sea-scleractinian/docview/2886738384/se-2?accountid=9730
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geographic Pacific
Southern Ocean
geographic_facet Pacific
Southern Ocean
genre North Atlantic
Southern Ocean
genre_facet North Atlantic
Southern Ocean
op_source Sun , Y-J , Robinson , L F , Parkinson , I J , Stewart , J A , Lu , W , Hardisty , D S , Liu , Q , Kershaw , J , LaVigne , M & Horner , T J 2023 , ' Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals ' , Frontiers in Marine Science , vol. 10 , 1264380 . https://doi.org/10.3389/fmars.2023.1264380
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.3389/fmars.2023.1264380
container_title Frontiers in Marine Science
container_volume 10
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spelling ftubristolcris:oai:research-information.bris.ac.uk:publications/1bac35c3-4b3d-4e69-919f-fb3022ce4fd4 2024-02-11T10:06:46+01:00 Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals Sun, Yun-Ju Robinson, Laura F Parkinson, Ian J Stewart, Joseph A Lu, Wanyi Hardisty, Dalton S Liu, Qian Kershaw, James LaVigne, Michèle Horner, Tristan J 2023-12-07 https://hdl.handle.net/1983/1bac35c3-4b3d-4e69-919f-fb3022ce4fd4 https://research-information.bris.ac.uk/en/publications/1bac35c3-4b3d-4e69-919f-fb3022ce4fd4 https://doi.org/10.3389/fmars.2023.1264380 https://bris.idm.oclc.org/login?url=https://www.proquest.com/scholarly-journals/iodine-calcium-ratios-deep-sea-scleractinian/docview/2886738384/se-2?accountid=9730 https://media.proquest.com/media/hms/PFT/1/oxIAW?_a=ChgyMDI0MDExNjExNDA0ODMzMzo0NjY3MzESBjEwNzY4NxoKT05FX1NFQVJDSCIOMTM3LjIyMi4yMjkuMTcqBzIwNDk1MzgyCjI4ODY3MzgzODQ6DURvY3VtZW50SW1hZ2VCATBSBk9ubGluZVoCRlRiA1BGVGoKMjAyMy8xMS8wN3IKMjAyMy8xMS8wN3oAggEgUC0xMDA5MjQwLTk3MzAtRlJFRS1udWxsLTY1MDc5ODmSAQZPbmxpbmXKAXVNb3ppbGxhLzUuMCAoTWFjaW50b3NoOyBJbnRlbCBNYWMgT1MgWCAxMF8xNV83KSBBcHBsZVdlYktpdC81MzcuMzYgKEtIVE1MLCBsaWtlIEdlY2tvKSBDaHJvbWUvMTIwLjAuMC4wIFNhZmFyaS81MzcuMzbSARJTY2hvbGFybHkgSm91cm5hbHOaAgdQcmVQYWlkqgIrT1M6RU1TLU1lZGlhTGlua3NTZXJ2aWNlLWdldE1lZGlhVXJsRm9ySXRlbcoCD0FydGljbGV8RmVhdHVyZdICAVnyAgD6AgFZggMDV2ViigMcQ0lEOjIwMjQwMTE2MTE0MDQ4MzMzOjg5MDExMA%3D%3D&_s=3TTSC4bXE4FtjrhIe38nKF3UZKU%3D https://bris.on.worldcat.org/atoztitles/link?sid=ProQ:&issn=&volume=&issue=&title=Frontiers+in+Marine+Science&spage=&date=2023-11-07&atitle=Iodine-to-calcium+ratios+in+deep-sea+scleractinian+and+bamboo+corals&au=Sun,+Yun-Ju%3BRobinson,+Laura+F%3BParkinson,+Ian+J%3BStewart,+Joseph+A%3BLu,+Wanyi%3BHardisty,+Dalton+S%3BLiu,+Qian%3BKershaw,+James%3BLaVigne,+Mich%C3%A8le%3BHorner,+Tristan+J&id=doi:10.3389%2Ffmars.2023.1264380 eng eng info:eu-repo/semantics/restrictedAccess Sun , Y-J , Robinson , L F , Parkinson , I J , Stewart , J A , Lu , W , Hardisty , D S , Liu , Q , Kershaw , J , LaVigne , M & Horner , T J 2023 , ' Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals ' , Frontiers in Marine Science , vol. 10 , 1264380 . https://doi.org/10.3389/fmars.2023.1264380 Earth Sciences--Oceanography Seawater oxygen1 Iodine2 Deep-sea coral3 Scleractinian coral4 Bamboo coral5 Deep sea Corals Seawater Biogeochemistry Biological control Deep water Geochemistry Hypoxia Oxygenation Archives Mineralogy Iodates Oceans Museums Foraminifera Radiometric dating Carbonates Calcium Iodine Biogeochemical cycles Marine invertebrates Oxidation Oxygen Archives & records Biogeochemical cycle Southern Ocean article 2023 ftubristolcris https://doi.org/10.3389/fmars.2023.1264380 2024-01-25T23:33:23Z 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 Southern Ocean University of Bristol: Bristol Research Pacific Southern Ocean Frontiers in Marine Science 10