Dissolved Organic Carbon Source Influences Tropical Coastal Heterotrophic Bacterioplankton Response to Experimental Warming

Global change impacts on marine biogeochemistry will be partly mediated by heterotrophic bacteria. Besides ocean warming, future environmental changes have been suggested to affect the quantity and quality of organic matter available for bacterial growth. However, it is yet to be determined in what...

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Main Authors: Christian Lønborg, Federico Baltar, Cátia Carreira, Xosé Anxelu G. Morán
Format: Article
Language:English
Published: Frontiers Media S.A. 2019-12-01
Series:Frontiers in Microbiology
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fmicb.2019.02807/full
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spelling doaj-b7f34658a9b749d59a297bf0d064d9582020-11-25T01:20:43ZengFrontiers Media S.A.Frontiers in Microbiology1664-302X2019-12-011010.3389/fmicb.2019.02807494478Dissolved Organic Carbon Source Influences Tropical Coastal Heterotrophic Bacterioplankton Response to Experimental WarmingChristian Lønborg0Federico Baltar1Federico Baltar2Cátia Carreira3Xosé Anxelu G. Morán4Australian Institute of Marine Science, Townsville, QLD, AustraliaDepartment of Limnology and Bio-Oceanography, University of Vienna, Vienna, AustriaDepartment of Marine Science, University of Otago, Dunedin, New ZealandDepartamento de Biologia and CESAM, Universidade de Aveiro, Aveiro, PortugalRed Sea Research Center, King Abdullah University of Science and Technology, Thuwal, Saudi ArabiaGlobal change impacts on marine biogeochemistry will be partly mediated by heterotrophic bacteria. Besides ocean warming, future environmental changes have been suggested to affect the quantity and quality of organic matter available for bacterial growth. However, it is yet to be determined in what way warming and changing substrate conditions will impact marine heterotrophic bacteria activity. Using short-term (4 days) experiments conducted at three temperatures (−3°C, in situ, +3°C) we assessed the temperature dependence of bacterial cycling of marine surface water used as a control and three different dissolved organic carbon (DOC) substrates (glucose, seagrass, and mangrove) in tropical coastal waters of the Great Barrier Reef, Australia. Our study shows that DOC source had the largest effect on the measured bacterial response, but this response was amplified by increasing temperature. We specifically demonstrate that (1) extracellular enzymatic activity and DOC consumption increased with warming, (2) this enhanced DOC consumption did not result in increased biomass production, since the increases in respiration were larger than for bacterial growth with warming, and (3) different DOC bioavailability affected the magnitude of the microbial community response to warming. We suggest that in coastal tropical waters, the magnitude of heterotrophic bacterial productivity and enzyme activity response to warming will depend partly on the DOC source bioavailability.https://www.frontiersin.org/article/10.3389/fmicb.2019.02807/fulldissolved organic carbontemperaturemicrobial carbon cyclingextracellular enzymatic activitytropical coastal watersGreat Barrier Reef
collection DOAJ
language English
format Article
sources DOAJ
author Christian Lønborg
Federico Baltar
Federico Baltar
Cátia Carreira
Xosé Anxelu G. Morán
spellingShingle Christian Lønborg
Federico Baltar
Federico Baltar
Cátia Carreira
Xosé Anxelu G. Morán
Dissolved Organic Carbon Source Influences Tropical Coastal Heterotrophic Bacterioplankton Response to Experimental Warming
Frontiers in Microbiology
dissolved organic carbon
temperature
microbial carbon cycling
extracellular enzymatic activity
tropical coastal waters
Great Barrier Reef
author_facet Christian Lønborg
Federico Baltar
Federico Baltar
Cátia Carreira
Xosé Anxelu G. Morán
author_sort Christian Lønborg
title Dissolved Organic Carbon Source Influences Tropical Coastal Heterotrophic Bacterioplankton Response to Experimental Warming
title_short Dissolved Organic Carbon Source Influences Tropical Coastal Heterotrophic Bacterioplankton Response to Experimental Warming
title_full Dissolved Organic Carbon Source Influences Tropical Coastal Heterotrophic Bacterioplankton Response to Experimental Warming
title_fullStr Dissolved Organic Carbon Source Influences Tropical Coastal Heterotrophic Bacterioplankton Response to Experimental Warming
title_full_unstemmed Dissolved Organic Carbon Source Influences Tropical Coastal Heterotrophic Bacterioplankton Response to Experimental Warming
title_sort dissolved organic carbon source influences tropical coastal heterotrophic bacterioplankton response to experimental warming
publisher Frontiers Media S.A.
series Frontiers in Microbiology
issn 1664-302X
publishDate 2019-12-01
description Global change impacts on marine biogeochemistry will be partly mediated by heterotrophic bacteria. Besides ocean warming, future environmental changes have been suggested to affect the quantity and quality of organic matter available for bacterial growth. However, it is yet to be determined in what way warming and changing substrate conditions will impact marine heterotrophic bacteria activity. Using short-term (4 days) experiments conducted at three temperatures (−3°C, in situ, +3°C) we assessed the temperature dependence of bacterial cycling of marine surface water used as a control and three different dissolved organic carbon (DOC) substrates (glucose, seagrass, and mangrove) in tropical coastal waters of the Great Barrier Reef, Australia. Our study shows that DOC source had the largest effect on the measured bacterial response, but this response was amplified by increasing temperature. We specifically demonstrate that (1) extracellular enzymatic activity and DOC consumption increased with warming, (2) this enhanced DOC consumption did not result in increased biomass production, since the increases in respiration were larger than for bacterial growth with warming, and (3) different DOC bioavailability affected the magnitude of the microbial community response to warming. We suggest that in coastal tropical waters, the magnitude of heterotrophic bacterial productivity and enzyme activity response to warming will depend partly on the DOC source bioavailability.
topic dissolved organic carbon
temperature
microbial carbon cycling
extracellular enzymatic activity
tropical coastal waters
Great Barrier Reef
url https://www.frontiersin.org/article/10.3389/fmicb.2019.02807/full
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