Loss of 'blue carbon' from coastal salt marshes following habitat disturbance.

Increased recognition of the global importance of salt marshes as 'blue carbon' (C) sinks has led to concern that salt marshes could release large amounts of stored C into the atmosphere (as CO2) if they continue undergoing disturbance, thereby accelerating climate change. Empirical eviden...

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Autores principales: Peter I Macreadie, A Randall Hughes, David L Kimbro
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Publicado: Public Library of Science (PLoS) 2013
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spelling oai:doaj.org-article:7f9faa81466e40cf9b187a325593f65f2021-11-18T07:38:17ZLoss of 'blue carbon' from coastal salt marshes following habitat disturbance.1932-620310.1371/journal.pone.0069244https://doaj.org/article/7f9faa81466e40cf9b187a325593f65f2013-01-01T00:00:00Zhttps://www.ncbi.nlm.nih.gov/pmc/articles/pmid/23861964/?tool=EBIhttps://doaj.org/toc/1932-6203Increased recognition of the global importance of salt marshes as 'blue carbon' (C) sinks has led to concern that salt marshes could release large amounts of stored C into the atmosphere (as CO2) if they continue undergoing disturbance, thereby accelerating climate change. Empirical evidence of C release following salt marsh habitat loss due to disturbance is rare, yet such information is essential for inclusion of salt marshes in greenhouse gas emission reduction and offset schemes. Here we investigated the stability of salt marsh (Spartinaalterniflora) sediment C levels following seagrass (Thallasiatestudinum) wrack accumulation; a form of disturbance common throughout the world that removes large areas of plant biomass in salt marshes. At our study site (St Joseph Bay, Florida, USA), we recorded 296 patches (7.5 ± 2.3 m(2) mean area ± SE) of vegetation loss (aged 3-12 months) in a salt marsh meadow the size of a soccer field (7 275 m(2)). Within these disturbed patches, levels of organic C in the subsurface zone (1-5 cm depth) were ~30% lower than the surrounding undisturbed meadow. Subsequent analyses showed that the decline in subsurface C levels in disturbed patches was due to loss of below-ground plant (salt marsh) biomass, which otherwise forms the main component of the long-term 'refractory' C stock. We conclude that disturbance to salt marsh habitat due to wrack accumulation can cause significant release of below-ground C; which could shift salt marshes from C sinks to C sources, depending on the intensity and scale of disturbance. This mechanism of C release is likely to increase in the future due to sea level rise; which could increase wrack production due to increasing storminess, and will facilitate delivery of wrack into salt marsh zones due to higher and more frequent inundation.Peter I MacreadieA Randall HughesDavid L KimbroPublic Library of Science (PLoS)articleMedicineRScienceQENPLoS ONE, Vol 8, Iss 7, p e69244 (2013)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Peter I Macreadie
A Randall Hughes
David L Kimbro
Loss of 'blue carbon' from coastal salt marshes following habitat disturbance.
description Increased recognition of the global importance of salt marshes as 'blue carbon' (C) sinks has led to concern that salt marshes could release large amounts of stored C into the atmosphere (as CO2) if they continue undergoing disturbance, thereby accelerating climate change. Empirical evidence of C release following salt marsh habitat loss due to disturbance is rare, yet such information is essential for inclusion of salt marshes in greenhouse gas emission reduction and offset schemes. Here we investigated the stability of salt marsh (Spartinaalterniflora) sediment C levels following seagrass (Thallasiatestudinum) wrack accumulation; a form of disturbance common throughout the world that removes large areas of plant biomass in salt marshes. At our study site (St Joseph Bay, Florida, USA), we recorded 296 patches (7.5 ± 2.3 m(2) mean area ± SE) of vegetation loss (aged 3-12 months) in a salt marsh meadow the size of a soccer field (7 275 m(2)). Within these disturbed patches, levels of organic C in the subsurface zone (1-5 cm depth) were ~30% lower than the surrounding undisturbed meadow. Subsequent analyses showed that the decline in subsurface C levels in disturbed patches was due to loss of below-ground plant (salt marsh) biomass, which otherwise forms the main component of the long-term 'refractory' C stock. We conclude that disturbance to salt marsh habitat due to wrack accumulation can cause significant release of below-ground C; which could shift salt marshes from C sinks to C sources, depending on the intensity and scale of disturbance. This mechanism of C release is likely to increase in the future due to sea level rise; which could increase wrack production due to increasing storminess, and will facilitate delivery of wrack into salt marsh zones due to higher and more frequent inundation.
format article
author Peter I Macreadie
A Randall Hughes
David L Kimbro
author_facet Peter I Macreadie
A Randall Hughes
David L Kimbro
author_sort Peter I Macreadie
title Loss of 'blue carbon' from coastal salt marshes following habitat disturbance.
title_short Loss of 'blue carbon' from coastal salt marshes following habitat disturbance.
title_full Loss of 'blue carbon' from coastal salt marshes following habitat disturbance.
title_fullStr Loss of 'blue carbon' from coastal salt marshes following habitat disturbance.
title_full_unstemmed Loss of 'blue carbon' from coastal salt marshes following habitat disturbance.
title_sort loss of 'blue carbon' from coastal salt marshes following habitat disturbance.
publisher Public Library of Science (PLoS)
publishDate 2013
url https://doaj.org/article/7f9faa81466e40cf9b187a325593f65f
work_keys_str_mv AT peterimacreadie lossofbluecarbonfromcoastalsaltmarshesfollowinghabitatdisturbance
AT arandallhughes lossofbluecarbonfromcoastalsaltmarshesfollowinghabitatdisturbance
AT davidlkimbro lossofbluecarbonfromcoastalsaltmarshesfollowinghabitatdisturbance
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