Closing the Global Marine 226Ra Budget Reveals the Biological Pump as a Dominant Removal Flux in the Upper Ocean

Abstract Radium isotopes are powerful proxies in oceanography and hydrology. Radium mass balance models, including assessments of submarine groundwater discharge (SGD), often overlook particle scavenging (PS) as a pathway for dissolved radium removal from the world ocean. Here, we build a global oce...

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Main Authors: Bochao Xu, M. Bayani Cardenas, Isaac R. Santos, William C. Burnett, Matthew A. Charette, Valentí Rodellas, Sanzhong Li, Ergang Lian, Zhigang Yu
Format: Article
Language:English
Published: Wiley 2022-06-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2022GL098087
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author Bochao Xu
M. Bayani Cardenas
Isaac R. Santos
William C. Burnett
Matthew A. Charette
Valentí Rodellas
Sanzhong Li
Ergang Lian
Zhigang Yu
author_facet Bochao Xu
M. Bayani Cardenas
Isaac R. Santos
William C. Burnett
Matthew A. Charette
Valentí Rodellas
Sanzhong Li
Ergang Lian
Zhigang Yu
author_sort Bochao Xu
collection DOAJ
description Abstract Radium isotopes are powerful proxies in oceanography and hydrology. Radium mass balance models, including assessments of submarine groundwater discharge (SGD), often overlook particle scavenging (PS) as a pathway for dissolved radium removal from the world ocean. Here, we build a global ocean 226Ra mass balance model and reevaluate the potential importance of PS. We find that PS is the major 226Ra sink for the upper ocean, removing about 96% of the total input from various sources. Aside from vertical exchange with the lower ocean, SGD is the largest 226Ra source into the upper ocean. The biological pump transfers particles to the deep ocean, resulting in a major but often overlooked impact on the global 226Ra marine budget. Our findings suggest that radium mass balance models should consider PS in systems with high siliceous algae production and export fluxes and long water residence times to prevent underestimation of large‐scale SGD fluxes.
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institution Kabale University
issn 0094-8276
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language English
publishDate 2022-06-01
publisher Wiley
record_format Article
series Geophysical Research Letters
spelling doaj-art-03c8d91970d94c35929e4c26c38ec1d62025-01-22T14:38:16ZengWileyGeophysical Research Letters0094-82761944-80072022-06-014912n/an/a10.1029/2022GL098087Closing the Global Marine 226Ra Budget Reveals the Biological Pump as a Dominant Removal Flux in the Upper OceanBochao Xu0M. Bayani Cardenas1Isaac R. Santos2William C. Burnett3Matthew A. Charette4Valentí Rodellas5Sanzhong Li6Ergang Lian7Zhigang Yu8Frontiers Science Center for Deep Ocean Multispheres and Earth System Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education Ocean University of China Qingdao ChinaDepartment of Geological Sciences Jackson School of Geosciences The University of Texas at Austin Austin TX USADepartment of Marine Sciences University of Gothenburg Gothenburg SwedenDepartment of Earth, Ocean and Atmospheric Science Florida State University Tallahassee FL USADepartment of Marine Chemistry and Geochemistry Woods Hole Oceanographic Institution Woods Hole MA USAInstitut de Ciència I Tecnologia Ambientals (ICTA) Universitat Autònoma de Barcelona Catalonia SpainFrontiers Science Center for Deep Ocean Multispheres and Earth System Key Lab of Submarine Geosciences and Prospecting Techniques Ministry of Education College of Marine Geosciences Ocean University of China Qingdao ChinaState Key Laboratory of Marine Geology Tongji University Shanghai ChinaFrontiers Science Center for Deep Ocean Multispheres and Earth System Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education Ocean University of China Qingdao ChinaAbstract Radium isotopes are powerful proxies in oceanography and hydrology. Radium mass balance models, including assessments of submarine groundwater discharge (SGD), often overlook particle scavenging (PS) as a pathway for dissolved radium removal from the world ocean. Here, we build a global ocean 226Ra mass balance model and reevaluate the potential importance of PS. We find that PS is the major 226Ra sink for the upper ocean, removing about 96% of the total input from various sources. Aside from vertical exchange with the lower ocean, SGD is the largest 226Ra source into the upper ocean. The biological pump transfers particles to the deep ocean, resulting in a major but often overlooked impact on the global 226Ra marine budget. Our findings suggest that radium mass balance models should consider PS in systems with high siliceous algae production and export fluxes and long water residence times to prevent underestimation of large‐scale SGD fluxes.https://doi.org/10.1029/2022GL098087particle scavengingsubmarine groundwater dischargesiliceous algaeglobal ocean
spellingShingle Bochao Xu
M. Bayani Cardenas
Isaac R. Santos
William C. Burnett
Matthew A. Charette
Valentí Rodellas
Sanzhong Li
Ergang Lian
Zhigang Yu
Closing the Global Marine 226Ra Budget Reveals the Biological Pump as a Dominant Removal Flux in the Upper Ocean
Geophysical Research Letters
particle scavenging
submarine groundwater discharge
siliceous algae
global ocean
title Closing the Global Marine 226Ra Budget Reveals the Biological Pump as a Dominant Removal Flux in the Upper Ocean
title_full Closing the Global Marine 226Ra Budget Reveals the Biological Pump as a Dominant Removal Flux in the Upper Ocean
title_fullStr Closing the Global Marine 226Ra Budget Reveals the Biological Pump as a Dominant Removal Flux in the Upper Ocean
title_full_unstemmed Closing the Global Marine 226Ra Budget Reveals the Biological Pump as a Dominant Removal Flux in the Upper Ocean
title_short Closing the Global Marine 226Ra Budget Reveals the Biological Pump as a Dominant Removal Flux in the Upper Ocean
title_sort closing the global marine 226ra budget reveals the biological pump as a dominant removal flux in the upper ocean
topic particle scavenging
submarine groundwater discharge
siliceous algae
global ocean
url https://doi.org/10.1029/2022GL098087
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