Potential Interactions Between Diatoms and Bacteria are Shaped by Trace Element Gradients in the Southern Ocean

The growth of diatoms in the Southern Ocean, especially the region surrounding the West Antarctic Peninsula, is frequently constrained by low dissolved iron and other trace metal concentrations. This challenge may be overcome by mutualisms between diatoms and co-occurring associated bacteria, in whi...

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Published in:Frontiers in Marine Science
Main Authors: Sterling, Alexa R., Holland, Laura Z., Bundy, Randelle M., Burns, Shannon M., Buck, Kristen N., Chappell, P. Dreux, Jenkins, Bethany D.
Format: Article in Journal/Newspaper
Language:unknown
Published: ODU Digital Commons 2023
Subjects:
Online Access:https://digitalcommons.odu.edu/oeas_fac_pubs/479
https://doi.org/10.3389/fmars.2022.876830
https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1490/viewcontent/Chappell_2023_PotentialInteractionsBetweenDiatomsandBacteriaOCR.pdf
id ftolddominionuni:oai:digitalcommons.odu.edu:oeas_fac_pubs-1490
record_format openpolar
institution Open Polar
collection Old Dominion University: ODU Digital Commons
op_collection_id ftolddominionuni
language unknown
topic Antarctic Peninsula
Bacillariophyceae
Bacteria
Bioavailability
Biosynthesis
Carbon
Climate change
Community composition
Continental margins
Diatom-bacteria interactions
Diatoms
Gradients
Growth
Heavy metals
Iron
Ligands
Manganese
Marine microorganisms
Metabolites
Metals
Mutualism
Nutrients
Offshore
Organic carbon
Phytoplankton
Phytoplankton microbiome
Plankton
Polar environments
rRNA 16S
Salinity
Siderophores
Southern Ocean
Trace elements
Trace element nutrients
Trace metal limitation
Trace metals
Uptake
Vitamins
Environmental Chemistry
Marine Biology
Oceanography
spellingShingle Antarctic Peninsula
Bacillariophyceae
Bacteria
Bioavailability
Biosynthesis
Carbon
Climate change
Community composition
Continental margins
Diatom-bacteria interactions
Diatoms
Gradients
Growth
Heavy metals
Iron
Ligands
Manganese
Marine microorganisms
Metabolites
Metals
Mutualism
Nutrients
Offshore
Organic carbon
Phytoplankton
Phytoplankton microbiome
Plankton
Polar environments
rRNA 16S
Salinity
Siderophores
Southern Ocean
Trace elements
Trace element nutrients
Trace metal limitation
Trace metals
Uptake
Vitamins
Environmental Chemistry
Marine Biology
Oceanography
Sterling, Alexa R.
Holland, Laura Z.
Bundy, Randelle M.
Burns, Shannon M.
Buck, Kristen N.
Chappell, P. Dreux
Jenkins, Bethany D.
Potential Interactions Between Diatoms and Bacteria are Shaped by Trace Element Gradients in the Southern Ocean
topic_facet Antarctic Peninsula
Bacillariophyceae
Bacteria
Bioavailability
Biosynthesis
Carbon
Climate change
Community composition
Continental margins
Diatom-bacteria interactions
Diatoms
Gradients
Growth
Heavy metals
Iron
Ligands
Manganese
Marine microorganisms
Metabolites
Metals
Mutualism
Nutrients
Offshore
Organic carbon
Phytoplankton
Phytoplankton microbiome
Plankton
Polar environments
rRNA 16S
Salinity
Siderophores
Southern Ocean
Trace elements
Trace element nutrients
Trace metal limitation
Trace metals
Uptake
Vitamins
Environmental Chemistry
Marine Biology
Oceanography
description The growth of diatoms in the Southern Ocean, especially the region surrounding the West Antarctic Peninsula, is frequently constrained by low dissolved iron and other trace metal concentrations. This challenge may be overcome by mutualisms between diatoms and co-occurring associated bacteria, in which diatoms produce organic carbon as a substrate for bacterial growth, and bacteria produce siderophores, metal-binding ligands that can supply diatoms with metals upon uptake as well as other useful secondary compounds for diatom growth like vitamins. To examine the relationships between diatoms and bacteria in the plankton (diatom) size class (> 3 mu m), we sampled both bacterial and diatom community composition with accompanying environmental metadata across a naturally occurring concentration gradient of macronutrients, trace metals and siderophores at 21 stations near the West Antarctic Peninsula (WAP). Offshore Drake Passage stations had low dissolved iron (0.33 ± 0.15 nM), while the stations closer to the continental margin had higher dissolved iron (5.05 ± 1.83 nM). A similar geographic pattern was observed for macronutrients and most other trace metals measured, but there was not a clear inshore-offshore gradient in siderophore concentrations. The diatom and bacteria assemblages, determined using 18S and 16S rDNA sequencing respectively, were similar by location sampled, and variance in both assemblages was driven in part by concentrations of soluble reactive phosphorous, dissolved manganese, and dissolved copper, which were all higher near the continent. Some of the most common diatom sequence types observed were Thalassiosira and Fragilariopsis, and bacteria in the plankton size fraction were most commonly Bacteroidetes and Gammaproteobacteria. Network analysis showed positive associations between diatoms and bacteria, indicating possible in situ mutualisms through strategies such as siderophore and vitamin biosynthesis and exchange. This work furthers the understanding of how naturally occurring ...
format Article in Journal/Newspaper
author Sterling, Alexa R.
Holland, Laura Z.
Bundy, Randelle M.
Burns, Shannon M.
Buck, Kristen N.
Chappell, P. Dreux
Jenkins, Bethany D.
author_facet Sterling, Alexa R.
Holland, Laura Z.
Bundy, Randelle M.
Burns, Shannon M.
Buck, Kristen N.
Chappell, P. Dreux
Jenkins, Bethany D.
author_sort Sterling, Alexa R.
title Potential Interactions Between Diatoms and Bacteria are Shaped by Trace Element Gradients in the Southern Ocean
title_short Potential Interactions Between Diatoms and Bacteria are Shaped by Trace Element Gradients in the Southern Ocean
title_full Potential Interactions Between Diatoms and Bacteria are Shaped by Trace Element Gradients in the Southern Ocean
title_fullStr Potential Interactions Between Diatoms and Bacteria are Shaped by Trace Element Gradients in the Southern Ocean
title_full_unstemmed Potential Interactions Between Diatoms and Bacteria are Shaped by Trace Element Gradients in the Southern Ocean
title_sort potential interactions between diatoms and bacteria are shaped by trace element gradients in the southern ocean
publisher ODU Digital Commons
publishDate 2023
url https://digitalcommons.odu.edu/oeas_fac_pubs/479
https://doi.org/10.3389/fmars.2022.876830
https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1490/viewcontent/Chappell_2023_PotentialInteractionsBetweenDiatomsandBacteriaOCR.pdf
geographic Antarctic
Southern Ocean
Antarctic Peninsula
Drake Passage
geographic_facet Antarctic
Southern Ocean
Antarctic Peninsula
Drake Passage
genre Antarc*
Antarctic
Antarctic Peninsula
Drake Passage
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Drake Passage
Southern Ocean
op_source OES Faculty Publications
op_relation https://digitalcommons.odu.edu/oeas_fac_pubs/479
doi:10.3389/fmars.2022.876830
https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1490/viewcontent/Chappell_2023_PotentialInteractionsBetweenDiatomsandBacteriaOCR.pdf
op_rights © 2023 Sterling, Holland, Bundy, Burns, Buck, Chappell and Jenkins. This is an open-access article distributed under the terms of the Creative Commons Attribution 4.0 International License (CC BY 4.0) . The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
op_doi https://doi.org/10.3389/fmars.2022.876830
container_title Frontiers in Marine Science
container_volume 9
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spelling ftolddominionuni:oai:digitalcommons.odu.edu:oeas_fac_pubs-1490 2023-12-10T09:41:15+01:00 Potential Interactions Between Diatoms and Bacteria are Shaped by Trace Element Gradients in the Southern Ocean Sterling, Alexa R. Holland, Laura Z. Bundy, Randelle M. Burns, Shannon M. Buck, Kristen N. Chappell, P. Dreux Jenkins, Bethany D. 2023-01-01T08:00:00Z application/pdf https://digitalcommons.odu.edu/oeas_fac_pubs/479 https://doi.org/10.3389/fmars.2022.876830 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1490/viewcontent/Chappell_2023_PotentialInteractionsBetweenDiatomsandBacteriaOCR.pdf unknown ODU Digital Commons https://digitalcommons.odu.edu/oeas_fac_pubs/479 doi:10.3389/fmars.2022.876830 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1490/viewcontent/Chappell_2023_PotentialInteractionsBetweenDiatomsandBacteriaOCR.pdf © 2023 Sterling, Holland, Bundy, Burns, Buck, Chappell and Jenkins. This is an open-access article distributed under the terms of the Creative Commons Attribution 4.0 International License (CC BY 4.0) . The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. OES Faculty Publications Antarctic Peninsula Bacillariophyceae Bacteria Bioavailability Biosynthesis Carbon Climate change Community composition Continental margins Diatom-bacteria interactions Diatoms Gradients Growth Heavy metals Iron Ligands Manganese Marine microorganisms Metabolites Metals Mutualism Nutrients Offshore Organic carbon Phytoplankton Phytoplankton microbiome Plankton Polar environments rRNA 16S Salinity Siderophores Southern Ocean Trace elements Trace element nutrients Trace metal limitation Trace metals Uptake Vitamins Environmental Chemistry Marine Biology Oceanography article 2023 ftolddominionuni https://doi.org/10.3389/fmars.2022.876830 2023-11-13T19:09:43Z The growth of diatoms in the Southern Ocean, especially the region surrounding the West Antarctic Peninsula, is frequently constrained by low dissolved iron and other trace metal concentrations. This challenge may be overcome by mutualisms between diatoms and co-occurring associated bacteria, in which diatoms produce organic carbon as a substrate for bacterial growth, and bacteria produce siderophores, metal-binding ligands that can supply diatoms with metals upon uptake as well as other useful secondary compounds for diatom growth like vitamins. To examine the relationships between diatoms and bacteria in the plankton (diatom) size class (> 3 mu m), we sampled both bacterial and diatom community composition with accompanying environmental metadata across a naturally occurring concentration gradient of macronutrients, trace metals and siderophores at 21 stations near the West Antarctic Peninsula (WAP). Offshore Drake Passage stations had low dissolved iron (0.33 ± 0.15 nM), while the stations closer to the continental margin had higher dissolved iron (5.05 ± 1.83 nM). A similar geographic pattern was observed for macronutrients and most other trace metals measured, but there was not a clear inshore-offshore gradient in siderophore concentrations. The diatom and bacteria assemblages, determined using 18S and 16S rDNA sequencing respectively, were similar by location sampled, and variance in both assemblages was driven in part by concentrations of soluble reactive phosphorous, dissolved manganese, and dissolved copper, which were all higher near the continent. Some of the most common diatom sequence types observed were Thalassiosira and Fragilariopsis, and bacteria in the plankton size fraction were most commonly Bacteroidetes and Gammaproteobacteria. Network analysis showed positive associations between diatoms and bacteria, indicating possible in situ mutualisms through strategies such as siderophore and vitamin biosynthesis and exchange. This work furthers the understanding of how naturally occurring ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Drake Passage Southern Ocean Old Dominion University: ODU Digital Commons Antarctic Southern Ocean Antarctic Peninsula Drake Passage Frontiers in Marine Science 9