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dc.contributor.authorSmeaton, Craig
dc.contributor.authorLadd, Cai
dc.contributor.authorMiller, Lucy
dc.contributor.authorMcMahon, Lucy
dc.contributor.authorGarrett, Ed
dc.contributor.authorBarlow, Natasha
dc.contributor.authorGehrels, W. Roland
dc.contributor.authorSkov, Martin W
dc.contributor.authorAustin, William
dc.date.accessioned2023-12-04T09:30:06Z
dc.date.available2023-12-04T09:30:06Z
dc.date.issued2023-12-04
dc.identifier296641058
dc.identifieraaa6bb5c-48e7-45d3-a8ad-5ffeea14b6d6
dc.identifier85180214287
dc.identifier.citationSmeaton , C , Ladd , C , Miller , L , McMahon , L , Garrett , E , Barlow , N , Gehrels , W R , Skov , M W & Austin , W 2023 , ' Organic carbon stocks of Great British saltmarshes ' , Frontiers in Marine Science , vol. 10 . https://doi.org/10.3389/fmars.2023.1229486en
dc.identifier.issn2296-7745
dc.identifier.otherORCID: /0000-0003-4535-2555/work/148421090
dc.identifier.urihttps://hdl.handle.net/10023/28811
dc.descriptionFunding: This research was finically supported by the Natural Environment Research Council funded Carbon Storage in Intertidal Environments (C-SIDE) project (grant NE/R010846/1) with additional support from the Scottish Blue Forum.en
dc.description.abstractCoastal wetlands, such as saltmarshes, are globally widespread and highly effective at capturing and storing 'blue carbon' and have the potential to regulate climate over varying timescales. Yet only Australia and the United States of America have national inventories of organic carbon held within saltmarsh habitats, hindering the development of policies and management strategies to protect and preserve these organic carbon stores. Here we couple a new observational dataset with 4,797 samples from 26 saltmarshes across Great Britain to spatially model organic carbon stored in the soil and the above and belowground biomass of Great British saltmarshes. Using average values derived from the 26 marshes, we deliver first-order estimates of organic carbon stocks across Great Britain's 448 saltmarshes (451.66 km 2 ). The saltmarshes of Great Britain contain 5.20 ± 0.65 Mt of organic carbon, 93% of which is in the soil. On average, the saltmarshes store 11.55 ± 1.56 kg C m -2 with values ranging between 2.24 kg C m -2 and 40.51 kg C m -2 depending on interlinked factors such as geomorphology, organic carbon source, sediment type (mud vs sand), sediment supply, and relative sea level history. These findings affirm that saltmarshes represent the largest intertidal blue carbon store in Great Britian, yet remain an unaccounted for component of the United Kingdom's natural carbon stores.
dc.format.extent18
dc.format.extent9001012
dc.language.isoeng
dc.relation.ispartofFrontiers in Marine Scienceen
dc.subjectCoastalen
dc.subjectWetlandsen
dc.subjectSoilen
dc.subjectVegetationen
dc.subjectBelowground storageen
dc.subjectUnited Kingdomen
dc.subjectBlue carbonen
dc.subjectCarbonen
dc.subjectOrganic carbonen
dc.subjectOrganic matteren
dc.subjectAbovegrounden
dc.subjectBelowgrounden
dc.subjectSaltmarshen
dc.subjectSalt marshen
dc.subjectUKen
dc.subjectWalesen
dc.subjectScotlanden
dc.subjectEnglanden
dc.subjectGBen
dc.subjectGreat Britainen
dc.subjectGB Physical geographyen
dc.subjectGE Environmental Sciencesen
dc.subjectEarth and Planetary Sciences (miscellaneous)en
dc.subjectEarth-Surface Processesen
dc.subjectGeneral Environmental Scienceen
dc.subjectGlobal and Planetary Changeen
dc.subjectDASen
dc.subjectSDG 14 - Life Below Wateren
dc.subjectSDG 15 - Life on Landen
dc.subjectSDG 13 - Climate Actionen
dc.subject.lccGBen
dc.subject.lccGEen
dc.titleOrganic carbon stocks of Great British saltmarshesen
dc.typeJournal articleen
dc.contributor.sponsorNERCen
dc.contributor.institutionUniversity of St Andrews. School of Geography & Sustainable Developmenten
dc.contributor.institutionUniversity of St Andrews. Environmental Change Research Groupen
dc.contributor.institutionUniversity of St Andrews. Marine Alliance for Science & Technology Scotlanden
dc.contributor.institutionUniversity of St Andrews. St Andrews Sustainability Instituteen
dc.identifier.doi10.3389/fmars.2023.1229486
dc.description.statusPeer revieweden
dc.identifier.grantnumberNE/R010846/1en


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