Distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean

Cobalt is a necessary nutrient for many marine phytoplankton, but its hybrid-type nature results in small marine inventories that make it one of the scarcest bioactive trace metals in the oceans. This study examines the marine dissolved cobalt cycle in two regions: the Pacific Ocean and Antarctic co...

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Main Author: Chmiel, Rebecca Jane
Other Authors: Saito, Makoto A., Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Thesis
Language:unknown
Published: Massachusetts Institute of Technology 2023
Subjects:
Online Access:https://hdl.handle.net/1721.1/150086
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spelling ftmit:oai:dspace.mit.edu:1721.1/150086 2023-06-11T04:06:25+02:00 Distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean Chmiel, Rebecca Jane Saito, Makoto A. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences 2023-03-01T13:49:41.039Z application/pdf https://hdl.handle.net/1721.1/150086 unknown Massachusetts Institute of Technology https://hdl.handle.net/1721.1/150086 orcid:0000-0003-1461-8744 In Copyright - Educational Use Permitted Copyright retained by author(s) https://rightsstatements.org/page/InC-EDU/1.0/ Thesis 2023 ftmit 2023-05-29T08:43:01Z Cobalt is a necessary nutrient for many marine phytoplankton, but its hybrid-type nature results in small marine inventories that make it one of the scarcest bioactive trace metals in the oceans. This study examines the marine dissolved cobalt cycle in two regions: the Pacific Ocean and Antarctic coastal seas. In the North Pacific, elevated cobalt stoichiometries among phytoplankton were linked to nitrogen, iron and phosphate stress protein biomarkers at the boundaries of oceanographic provinces and upwelling zones, providing insight into the flexibility of cobalt stoichiometry. In both regions, perturbations to the marine cobalt cycle were either predicted or observed; in the equatorial Pacific, the dissolved cobalt inventory was predicted to increase by up to 28% due to the expansion of oxygen minimum zones in a warmer ocean, while in the Antarctic, melting ice shelves have the potential to shift the nutrient regime from iron limitation towards zinc and vitamin B12 limitation, resulting in higher cobalt demand and a lower dissolved cobalt inventory. When the global cobalt cycle was estimated throughout four of Earth’s systems (the lithosphere, biosphere, hydrosphere and the anthroposphere – the human environment), it was determined that the scale of the cobalt flux through the anthroposphere is only one order of magnitude lower than the inventory of the entire hydrosphere (10⁹ mol Co yr⁻¹ and 10¹⁰ mol Co, respectively), revealing a vulnerability to anthropogenic perturbation of the marine cobalt inventory through human mining, use and disposal of cobalt if appropriate pollution abatement, disposal and recycling infrastructure is not established. In light of observed and predicted changes to cobalt biogeochemistry, this research suggests that the marine cobalt cycle is particularly vulnerable to anthropogenic perturbation from both global climate change and pollution due to its low ocean inventory and interconnection to other nutrient biogeochemical cycles. Ph.D. Thesis Antarc* Antarctic Ice Shelves DSpace@MIT (Massachusetts Institute of Technology) Antarctic The Antarctic Pacific
institution Open Polar
collection DSpace@MIT (Massachusetts Institute of Technology)
op_collection_id ftmit
language unknown
description Cobalt is a necessary nutrient for many marine phytoplankton, but its hybrid-type nature results in small marine inventories that make it one of the scarcest bioactive trace metals in the oceans. This study examines the marine dissolved cobalt cycle in two regions: the Pacific Ocean and Antarctic coastal seas. In the North Pacific, elevated cobalt stoichiometries among phytoplankton were linked to nitrogen, iron and phosphate stress protein biomarkers at the boundaries of oceanographic provinces and upwelling zones, providing insight into the flexibility of cobalt stoichiometry. In both regions, perturbations to the marine cobalt cycle were either predicted or observed; in the equatorial Pacific, the dissolved cobalt inventory was predicted to increase by up to 28% due to the expansion of oxygen minimum zones in a warmer ocean, while in the Antarctic, melting ice shelves have the potential to shift the nutrient regime from iron limitation towards zinc and vitamin B12 limitation, resulting in higher cobalt demand and a lower dissolved cobalt inventory. When the global cobalt cycle was estimated throughout four of Earth’s systems (the lithosphere, biosphere, hydrosphere and the anthroposphere – the human environment), it was determined that the scale of the cobalt flux through the anthroposphere is only one order of magnitude lower than the inventory of the entire hydrosphere (10⁹ mol Co yr⁻¹ and 10¹⁰ mol Co, respectively), revealing a vulnerability to anthropogenic perturbation of the marine cobalt inventory through human mining, use and disposal of cobalt if appropriate pollution abatement, disposal and recycling infrastructure is not established. In light of observed and predicted changes to cobalt biogeochemistry, this research suggests that the marine cobalt cycle is particularly vulnerable to anthropogenic perturbation from both global climate change and pollution due to its low ocean inventory and interconnection to other nutrient biogeochemical cycles. Ph.D.
author2 Saito, Makoto A.
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
format Thesis
author Chmiel, Rebecca Jane
spellingShingle Chmiel, Rebecca Jane
Distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean
author_facet Chmiel, Rebecca Jane
author_sort Chmiel, Rebecca Jane
title Distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean
title_short Distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean
title_full Distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean
title_fullStr Distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean
title_full_unstemmed Distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean
title_sort distributions and perturbations of the marine dissolved cobalt cycle in a changing ocean
publisher Massachusetts Institute of Technology
publishDate 2023
url https://hdl.handle.net/1721.1/150086
geographic Antarctic
The Antarctic
Pacific
geographic_facet Antarctic
The Antarctic
Pacific
genre Antarc*
Antarctic
Ice Shelves
genre_facet Antarc*
Antarctic
Ice Shelves
op_relation https://hdl.handle.net/1721.1/150086
orcid:0000-0003-1461-8744
op_rights In Copyright - Educational Use Permitted
Copyright retained by author(s)
https://rightsstatements.org/page/InC-EDU/1.0/
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