Response of Seagrass ‘Blue Carbon’ Stocks to Increased Water Temperatures

Seagrass meadows are globally important sinks of ‘Blue Carbon’, but warming water temperatures due to climate change may undermine their capacity to sequester and retain organic carbon (Corg). We tested the effects of warming on seagrass Corg stocks in situ by transplanting seagr...

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Main Authors: Peter I. Macreadie, Simon S. S. Hardy
Format: Article
Language:English
Published: MDPI AG 2018-10-01
Series:Diversity
Subjects:
Online Access:http://www.mdpi.com/1424-2818/10/4/115
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spelling doaj-c5da8114776e47adaff775f4d6ff01652020-11-24T20:40:37ZengMDPI AGDiversity1424-28182018-10-0110411510.3390/d10040115d10040115Response of Seagrass ‘Blue Carbon’ Stocks to Increased Water TemperaturesPeter I. Macreadie0Simon S. S. Hardy1Centre for Integrative Ecology, School of Life and Environmental Sciences, Deakin University, Burwood 3216, AustraliaSchool of the Environment, University of Technology Sydney, Broadway, NSW 2007, AustraliaSeagrass meadows are globally important sinks of ‘Blue Carbon’, but warming water temperatures due to climate change may undermine their capacity to sequester and retain organic carbon (Corg). We tested the effects of warming on seagrass Corg stocks in situ by transplanting seagrass soil cores along a thermal plume generated by a coal-fired power plant in a seagrass-dominated estuary (Lake Macquarie, Australia). Transplanted cores were subjected to temperatures 2 and 4 °C above ambient temperatures and Corg content was measured after 7, 30, 90 and 180 days. We were unable to detect any significant effect of warming on Corg concentration, stocks, chemical composition (as measured by labile, recalcitrant, refractory ratios), or microbial abundance at any time point. In fact, Corg levels were temporally variable. These findings contrast those of previous studies (mostly laboratory-based) that have reported increases in microbial remineralisation (breakdown) of Corg in response to warming. To explain the lack of any detectable warming effect, we suggest that higher temperatures, longer durations of warming exposure, or additional stressors (e.g., oxygen exposure) may be needed to overcome microbial activation barriers and stimulate Corg remineralisation.http://www.mdpi.com/1424-2818/10/4/115Blue Carbonwarmingtemperatureseagrass ecosystemdisturbancesoil organic carbon
collection DOAJ
language English
format Article
sources DOAJ
author Peter I. Macreadie
Simon S. S. Hardy
spellingShingle Peter I. Macreadie
Simon S. S. Hardy
Response of Seagrass ‘Blue Carbon’ Stocks to Increased Water Temperatures
Diversity
Blue Carbon
warming
temperature
seagrass ecosystem
disturbance
soil organic carbon
author_facet Peter I. Macreadie
Simon S. S. Hardy
author_sort Peter I. Macreadie
title Response of Seagrass ‘Blue Carbon’ Stocks to Increased Water Temperatures
title_short Response of Seagrass ‘Blue Carbon’ Stocks to Increased Water Temperatures
title_full Response of Seagrass ‘Blue Carbon’ Stocks to Increased Water Temperatures
title_fullStr Response of Seagrass ‘Blue Carbon’ Stocks to Increased Water Temperatures
title_full_unstemmed Response of Seagrass ‘Blue Carbon’ Stocks to Increased Water Temperatures
title_sort response of seagrass ‘blue carbon’ stocks to increased water temperatures
publisher MDPI AG
series Diversity
issn 1424-2818
publishDate 2018-10-01
description Seagrass meadows are globally important sinks of ‘Blue Carbon’, but warming water temperatures due to climate change may undermine their capacity to sequester and retain organic carbon (Corg). We tested the effects of warming on seagrass Corg stocks in situ by transplanting seagrass soil cores along a thermal plume generated by a coal-fired power plant in a seagrass-dominated estuary (Lake Macquarie, Australia). Transplanted cores were subjected to temperatures 2 and 4 °C above ambient temperatures and Corg content was measured after 7, 30, 90 and 180 days. We were unable to detect any significant effect of warming on Corg concentration, stocks, chemical composition (as measured by labile, recalcitrant, refractory ratios), or microbial abundance at any time point. In fact, Corg levels were temporally variable. These findings contrast those of previous studies (mostly laboratory-based) that have reported increases in microbial remineralisation (breakdown) of Corg in response to warming. To explain the lack of any detectable warming effect, we suggest that higher temperatures, longer durations of warming exposure, or additional stressors (e.g., oxygen exposure) may be needed to overcome microbial activation barriers and stimulate Corg remineralisation.
topic Blue Carbon
warming
temperature
seagrass ecosystem
disturbance
soil organic carbon
url http://www.mdpi.com/1424-2818/10/4/115
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