Updated estimates of carbon accumulation rates in coastal marsh sediments

Studies on carbon stock in salt marsh sediments have increased since the review by Chmura et al. (2003). However, uncertainties exist in estimating global carbon storage in these vulnerable coastal habitats, thus hindering the assessment of their importance. Combining direct data and indirect estima...

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Main Authors: X. Ouyang, S. Y. Lee
Format: Article
Language:English
Published: Copernicus Publications 2014-09-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/11/5057/2014/bg-11-5057-2014.pdf
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spelling doaj-e475aad9a22a45c5a833bcdd5d69eeea2020-11-24T23:19:40ZengCopernicus PublicationsBiogeosciences1726-41701726-41892014-09-0111185057507110.5194/bg-11-5057-2014Updated estimates of carbon accumulation rates in coastal marsh sedimentsX. Ouyang0S. Y. Lee1Australian Rivers Institute-Coast and Estuaries and School of Environment, Griffith University Gold Coast campus, Southport Qld 4222, AustraliaAustralian Rivers Institute-Coast and Estuaries and School of Environment, Griffith University Gold Coast campus, Southport Qld 4222, AustraliaStudies on carbon stock in salt marsh sediments have increased since the review by Chmura et al. (2003). However, uncertainties exist in estimating global carbon storage in these vulnerable coastal habitats, thus hindering the assessment of their importance. Combining direct data and indirect estimation, this study compiled studies involving 143 sites across the Southern and Northern hemispheres, and provides an updated estimate of the global average carbon accumulation rate (CAR) at 244.7 g C m<sup>−2</sup> yr<sup>−1</sup> in salt marsh sediments. Based on region-specific CAR and estimates of salt marsh area in various geographic regions between 40° S to 69.7° N, total CAR in global salt marsh sediments is estimated at ~10.2 Tg C yr<sup>−1</sup>. Latitude, tidal range and elevation appear to be important drivers for CAR of salt marsh sediments, with considerable variation among different biogeographic regions. The data indicate that while the capacity for carbon sequestration by salt marsh sediments ranked the first amongst coastal wetland and forested terrestrial ecosystems, their carbon budget was the smallest due to their limited and declining global areal extent. However, some uncertainties remain for our global estimate owing to limited data availability.http://www.biogeosciences.net/11/5057/2014/bg-11-5057-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author X. Ouyang
S. Y. Lee
spellingShingle X. Ouyang
S. Y. Lee
Updated estimates of carbon accumulation rates in coastal marsh sediments
Biogeosciences
author_facet X. Ouyang
S. Y. Lee
author_sort X. Ouyang
title Updated estimates of carbon accumulation rates in coastal marsh sediments
title_short Updated estimates of carbon accumulation rates in coastal marsh sediments
title_full Updated estimates of carbon accumulation rates in coastal marsh sediments
title_fullStr Updated estimates of carbon accumulation rates in coastal marsh sediments
title_full_unstemmed Updated estimates of carbon accumulation rates in coastal marsh sediments
title_sort updated estimates of carbon accumulation rates in coastal marsh sediments
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2014-09-01
description Studies on carbon stock in salt marsh sediments have increased since the review by Chmura et al. (2003). However, uncertainties exist in estimating global carbon storage in these vulnerable coastal habitats, thus hindering the assessment of their importance. Combining direct data and indirect estimation, this study compiled studies involving 143 sites across the Southern and Northern hemispheres, and provides an updated estimate of the global average carbon accumulation rate (CAR) at 244.7 g C m<sup>−2</sup> yr<sup>−1</sup> in salt marsh sediments. Based on region-specific CAR and estimates of salt marsh area in various geographic regions between 40° S to 69.7° N, total CAR in global salt marsh sediments is estimated at ~10.2 Tg C yr<sup>−1</sup>. Latitude, tidal range and elevation appear to be important drivers for CAR of salt marsh sediments, with considerable variation among different biogeographic regions. The data indicate that while the capacity for carbon sequestration by salt marsh sediments ranked the first amongst coastal wetland and forested terrestrial ecosystems, their carbon budget was the smallest due to their limited and declining global areal extent. However, some uncertainties remain for our global estimate owing to limited data availability.
url http://www.biogeosciences.net/11/5057/2014/bg-11-5057-2014.pdf
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