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Natural oil slicks fuel surface water microbial activities in the northern Gulf of Mexico

We conducted a series of roller tank incubations with surface seawater from the Green Canyon oil reservoir, northern Gulf of Mexico, amended with either a natural oil slick (GCS-oil) or pristine oil. The goal was to test whether bacterial activities of natural surface water communities facilitate th...

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Autores principales: Ziervogel, Kai, D'souza, Nigel, Sweet, Julia, Yan, Beizhan, Passow, Uta
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4021148/
https://www.ncbi.nlm.nih.gov/pubmed/24847314
http://dx.doi.org/10.3389/fmicb.2014.00188
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author Ziervogel, Kai
D'souza, Nigel
Sweet, Julia
Yan, Beizhan
Passow, Uta
author_facet Ziervogel, Kai
D'souza, Nigel
Sweet, Julia
Yan, Beizhan
Passow, Uta
author_sort Ziervogel, Kai
collection PubMed
description We conducted a series of roller tank incubations with surface seawater from the Green Canyon oil reservoir, northern Gulf of Mexico, amended with either a natural oil slick (GCS-oil) or pristine oil. The goal was to test whether bacterial activities of natural surface water communities facilitate the formation of oil-rich marine snow (oil snow). Although oil snow did not form during any of our experiments, we found specific bacterial metabolic responses to the addition of GCS-oil that profoundly affected carbon cycling within our 4-days incubations. Peptidase and β-glucosidase activities indicative of bacterial enzymatic hydrolysis of peptides and carbohydrates, respectively, were suppressed upon the addition of GCS-oil relative to the non-oil treatment, suggesting that ascending oil and gas initially inhibits bacterial metabolism in surface water. Biodegradation of physically dispersed GCS-oil components, indicated by the degradation of lower molecular weight n-alkanes as well as the rapid transformation of particulate oil-carbon (C: N >40) into the DOC pool, led to the production of carbohydrate- and peptide-rich degradation byproducts and bacterial metabolites such as transparent exopolymer particles (TEP). TEP formation was highest at day 4 in the presence of GCS-oil; in contrast, TEP levels in the non-oil treatment already peaked at day 2. Cell-specific enzymatic activities closely followed TEP concentrations in the presence and absence of GCS-oil. These results demonstrate that the formation of oil slicks and activities of oil-degrading bacteria result in a temporal offset of microbial cycling of organic matter, affecting food web interactions and carbon cycling in surface waters over cold seeps.
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spelling pubmed-40211482014-05-20 Natural oil slicks fuel surface water microbial activities in the northern Gulf of Mexico Ziervogel, Kai D'souza, Nigel Sweet, Julia Yan, Beizhan Passow, Uta Front Microbiol Microbiology We conducted a series of roller tank incubations with surface seawater from the Green Canyon oil reservoir, northern Gulf of Mexico, amended with either a natural oil slick (GCS-oil) or pristine oil. The goal was to test whether bacterial activities of natural surface water communities facilitate the formation of oil-rich marine snow (oil snow). Although oil snow did not form during any of our experiments, we found specific bacterial metabolic responses to the addition of GCS-oil that profoundly affected carbon cycling within our 4-days incubations. Peptidase and β-glucosidase activities indicative of bacterial enzymatic hydrolysis of peptides and carbohydrates, respectively, were suppressed upon the addition of GCS-oil relative to the non-oil treatment, suggesting that ascending oil and gas initially inhibits bacterial metabolism in surface water. Biodegradation of physically dispersed GCS-oil components, indicated by the degradation of lower molecular weight n-alkanes as well as the rapid transformation of particulate oil-carbon (C: N >40) into the DOC pool, led to the production of carbohydrate- and peptide-rich degradation byproducts and bacterial metabolites such as transparent exopolymer particles (TEP). TEP formation was highest at day 4 in the presence of GCS-oil; in contrast, TEP levels in the non-oil treatment already peaked at day 2. Cell-specific enzymatic activities closely followed TEP concentrations in the presence and absence of GCS-oil. These results demonstrate that the formation of oil slicks and activities of oil-degrading bacteria result in a temporal offset of microbial cycling of organic matter, affecting food web interactions and carbon cycling in surface waters over cold seeps. Frontiers Media S.A. 2014-05-08 /pmc/articles/PMC4021148/ /pubmed/24847314 http://dx.doi.org/10.3389/fmicb.2014.00188 Text en Copyright © 2014 Ziervogel, D'souza, Sweet, Yan and Passow. http://creativecommons.org/licenses/by/3.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor 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.
spellingShingle Microbiology
Ziervogel, Kai
D'souza, Nigel
Sweet, Julia
Yan, Beizhan
Passow, Uta
Natural oil slicks fuel surface water microbial activities in the northern Gulf of Mexico
title Natural oil slicks fuel surface water microbial activities in the northern Gulf of Mexico
title_full Natural oil slicks fuel surface water microbial activities in the northern Gulf of Mexico
title_fullStr Natural oil slicks fuel surface water microbial activities in the northern Gulf of Mexico
title_full_unstemmed Natural oil slicks fuel surface water microbial activities in the northern Gulf of Mexico
title_short Natural oil slicks fuel surface water microbial activities in the northern Gulf of Mexico
title_sort natural oil slicks fuel surface water microbial activities in the northern gulf of mexico
topic Microbiology
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4021148/
https://www.ncbi.nlm.nih.gov/pubmed/24847314
http://dx.doi.org/10.3389/fmicb.2014.00188
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