Biogeochemical cycling of copper in the Northeast Pacific Ocean : role of marine heterotrophic bacteria

Copper (Cu) is important in regulating microbial activity in the ocean, as it can act both as a limiting nutrient and a toxic inhibitor depending on its concentration. Yet, our knowledge of its biogeochemical cycle is limited in many oceanic regions including the subarctic Northeast (NE) Pacific, as...

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Main Author: Posacka, Anna
Format: Thesis
Language:English
Published: University of British Columbia 2017
Subjects:
Online Access:http://hdl.handle.net/2429/62937
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spelling ftunivbritcolcir:oai:circle.library.ubc.ca:2429/62937 2023-05-15T18:28:23+02:00 Biogeochemical cycling of copper in the Northeast Pacific Ocean : role of marine heterotrophic bacteria Posacka, Anna 2017 http://hdl.handle.net/2429/62937 eng eng University of British Columbia Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ CC-BY-NC-ND Text Thesis/Dissertation 2017 ftunivbritcolcir 2019-10-15T18:23:57Z Copper (Cu) is important in regulating microbial activity in the ocean, as it can act both as a limiting nutrient and a toxic inhibitor depending on its concentration. Yet, our knowledge of its biogeochemical cycle is limited in many oceanic regions including the subarctic Northeast (NE) Pacific, as is our knowledge of Cu nutrition in marine heterotrophic bacteria. To address this, I investigated Cu biogeochemical cycling along a coastal‒oceanic transect, Line P, in the subarctic NE Pacific (Chapter 2). I also explored physiological responses to varying Cu availability (limiting to sufficient) of taxonomically diverse heterotrophic bacteria, which include isolates from surface waters of the Line P transect (Flavobacteriia member: Dokdonia sp. Dokd-P16, and Gammaproteobacteria members Pseudoalteromonas sp. strain PAlt-P2 [coastal] and PAlt-P26 [oceanic]), and a member of the marine Roseobacter clade within class Alphaproteobacteria (Ruegeria pomeroyi DSS-3). Several important processes were identified to moderate dissolved Cu along Line P. These include fluvial and sedimentary inputs (near the coast), upwelling of deep, Cu-rich waters in the Alaskan gyre (offshore), atmospheric inputs (offshore), as well as scavenging within the intermediate waters of the Oxygen Minimum Zone (OMZ) across the transect. Bacterial responses to changing Cu availability were diverse. Flavobacteriia member Dokd-P16 reduced its growth rate, carbon metabolism, and Cu quota (Cu:P) under Cu limitation, but enhanced its Mn quota. In contrast, both Pseudoalteromonas spp. were mostly unaffected by different Cu levels. Ruegeria pomeroyi maintained constant growth rates but moderated quotas of several metals (under low Cu: decreased Cu and Co, but increased Mn and Fe quotas), and some aspects of its C metabolism. These findings illuminate on the role of Cu in shaping bacterial species composition in the ocean, and the bacterially-mediated cycles of carbon and bioactive metals (i.e. Fe, Zn, Mn, Co). Copper quotas of heterotrophic bacteria are similar to those of cultured marine phytoplankton. Estimates of Cu partitioning between these planktonic groups in the euphotic zone of the NE Pacific revealed that up to 50% of biogenic Cu could be associated with bacterial biomass. Therefore, marine heterotrophic bacteria should not be overlooked in studies of Cu biogeochemical cycling. Science, Faculty of Earth, Ocean and Atmospheric Sciences, Department of Graduate Thesis Subarctic University of British Columbia: cIRcle - UBC's Information Repository Pacific
institution Open Polar
collection University of British Columbia: cIRcle - UBC's Information Repository
op_collection_id ftunivbritcolcir
language English
description Copper (Cu) is important in regulating microbial activity in the ocean, as it can act both as a limiting nutrient and a toxic inhibitor depending on its concentration. Yet, our knowledge of its biogeochemical cycle is limited in many oceanic regions including the subarctic Northeast (NE) Pacific, as is our knowledge of Cu nutrition in marine heterotrophic bacteria. To address this, I investigated Cu biogeochemical cycling along a coastal‒oceanic transect, Line P, in the subarctic NE Pacific (Chapter 2). I also explored physiological responses to varying Cu availability (limiting to sufficient) of taxonomically diverse heterotrophic bacteria, which include isolates from surface waters of the Line P transect (Flavobacteriia member: Dokdonia sp. Dokd-P16, and Gammaproteobacteria members Pseudoalteromonas sp. strain PAlt-P2 [coastal] and PAlt-P26 [oceanic]), and a member of the marine Roseobacter clade within class Alphaproteobacteria (Ruegeria pomeroyi DSS-3). Several important processes were identified to moderate dissolved Cu along Line P. These include fluvial and sedimentary inputs (near the coast), upwelling of deep, Cu-rich waters in the Alaskan gyre (offshore), atmospheric inputs (offshore), as well as scavenging within the intermediate waters of the Oxygen Minimum Zone (OMZ) across the transect. Bacterial responses to changing Cu availability were diverse. Flavobacteriia member Dokd-P16 reduced its growth rate, carbon metabolism, and Cu quota (Cu:P) under Cu limitation, but enhanced its Mn quota. In contrast, both Pseudoalteromonas spp. were mostly unaffected by different Cu levels. Ruegeria pomeroyi maintained constant growth rates but moderated quotas of several metals (under low Cu: decreased Cu and Co, but increased Mn and Fe quotas), and some aspects of its C metabolism. These findings illuminate on the role of Cu in shaping bacterial species composition in the ocean, and the bacterially-mediated cycles of carbon and bioactive metals (i.e. Fe, Zn, Mn, Co). Copper quotas of heterotrophic bacteria are similar to those of cultured marine phytoplankton. Estimates of Cu partitioning between these planktonic groups in the euphotic zone of the NE Pacific revealed that up to 50% of biogenic Cu could be associated with bacterial biomass. Therefore, marine heterotrophic bacteria should not be overlooked in studies of Cu biogeochemical cycling. Science, Faculty of Earth, Ocean and Atmospheric Sciences, Department of Graduate
format Thesis
author Posacka, Anna
spellingShingle Posacka, Anna
Biogeochemical cycling of copper in the Northeast Pacific Ocean : role of marine heterotrophic bacteria
author_facet Posacka, Anna
author_sort Posacka, Anna
title Biogeochemical cycling of copper in the Northeast Pacific Ocean : role of marine heterotrophic bacteria
title_short Biogeochemical cycling of copper in the Northeast Pacific Ocean : role of marine heterotrophic bacteria
title_full Biogeochemical cycling of copper in the Northeast Pacific Ocean : role of marine heterotrophic bacteria
title_fullStr Biogeochemical cycling of copper in the Northeast Pacific Ocean : role of marine heterotrophic bacteria
title_full_unstemmed Biogeochemical cycling of copper in the Northeast Pacific Ocean : role of marine heterotrophic bacteria
title_sort biogeochemical cycling of copper in the northeast pacific ocean : role of marine heterotrophic bacteria
publisher University of British Columbia
publishDate 2017
url http://hdl.handle.net/2429/62937
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_rights Attribution-NonCommercial-NoDerivatives 4.0 International
http://creativecommons.org/licenses/by-nc-nd/4.0/
op_rightsnorm CC-BY-NC-ND
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