Mixed provenance of organic carbon in Northeast Atlantic temperate intertidal seagrass sediments

Abstract Blue carbon accreditation for climate mitigation services provided by coastal ecosystems, such as seagrass beds, typically account only for autochthonous organic carbon, potentially underestimating the total carbon sequestration capacity of seagrass ecosystems. Here, a multi-proxy approach...

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Main Authors: Emma A. Ward, Sarah E. Reynolds, Melanie J. Leng, Jack H. Lacey, Marianna Cerasuolo, Bronwen Paxton, Federica Ragazzola, Joanne Preston
Format: Article
Language:English
Published: Nature Portfolio 2025-07-01
Series:Scientific Reports
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Online Access:https://doi.org/10.1038/s41598-025-12223-z
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author Emma A. Ward
Sarah E. Reynolds
Melanie J. Leng
Jack H. Lacey
Marianna Cerasuolo
Bronwen Paxton
Federica Ragazzola
Joanne Preston
author_facet Emma A. Ward
Sarah E. Reynolds
Melanie J. Leng
Jack H. Lacey
Marianna Cerasuolo
Bronwen Paxton
Federica Ragazzola
Joanne Preston
author_sort Emma A. Ward
collection DOAJ
description Abstract Blue carbon accreditation for climate mitigation services provided by coastal ecosystems, such as seagrass beds, typically account only for autochthonous organic carbon, potentially underestimating the total carbon sequestration capacity of seagrass ecosystems. Here, a multi-proxy approach is used to determine the provenance of organic carbon in two intertidal temperate seagrass ecosystems in the Northeast Atlantic. The organic carbon to nitrogen ratio (Corg/N) and carbon isotope composition (δ13C) of seagrass tissues and sediments from an open coastal sandy site (Ryde, UK) and a muddy tidal inlet site (Farlington Marshes, UK) were measured. Sedimentary Corg/N was higher at the muddy site than the sandy site, suggesting a greater contribution of marine algal organic matter in the latter. Isotopic mixing model analysis showed that seagrass biomass contributes between 12 and 25% to accumulated sedimentary Corg. These findings demonstrate that temperate Northeast Atlantic seagrass sediments are dominated by allochthonous Corg (75–88%) and that current blue carbon accreditation frameworks undervalue these ecosystems. Supporting the estimation and uptake of high integrity field-derived allochthonous deduction evidence would assist uptake of these frameworks to support implementation of nature-based solutions.
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spelling doaj-art-973e70bcd606451eaca43700657f32022025-08-20T04:01:49ZengNature PortfolioScientific Reports2045-23222025-07-0115111610.1038/s41598-025-12223-zMixed provenance of organic carbon in Northeast Atlantic temperate intertidal seagrass sedimentsEmma A. Ward0Sarah E. Reynolds1Melanie J. Leng2Jack H. Lacey3Marianna Cerasuolo4Bronwen Paxton5Federica Ragazzola6Joanne Preston7Faculty of Science and Health, School of Environment and Life Sciences, University of PortsmouthFaculty of Science and Health, School of Environment and Life Sciences, University of PortsmouthNational Environmental Isotope Facility, British Geological SurveyNational Environmental Isotope Facility, British Geological SurveyDepartment of Mathematics, School of Mathematical and Physical Sciences, University of SussexFaculty of Science and Health, School of Environment and Life Sciences, University of PortsmouthDepartment of Integrative Marine Ecology, Genoa Marine Centre, Stazione Zoologica Anton DohrnFaculty of Science and Health, School of Environment and Life Sciences, University of PortsmouthAbstract Blue carbon accreditation for climate mitigation services provided by coastal ecosystems, such as seagrass beds, typically account only for autochthonous organic carbon, potentially underestimating the total carbon sequestration capacity of seagrass ecosystems. Here, a multi-proxy approach is used to determine the provenance of organic carbon in two intertidal temperate seagrass ecosystems in the Northeast Atlantic. The organic carbon to nitrogen ratio (Corg/N) and carbon isotope composition (δ13C) of seagrass tissues and sediments from an open coastal sandy site (Ryde, UK) and a muddy tidal inlet site (Farlington Marshes, UK) were measured. Sedimentary Corg/N was higher at the muddy site than the sandy site, suggesting a greater contribution of marine algal organic matter in the latter. Isotopic mixing model analysis showed that seagrass biomass contributes between 12 and 25% to accumulated sedimentary Corg. These findings demonstrate that temperate Northeast Atlantic seagrass sediments are dominated by allochthonous Corg (75–88%) and that current blue carbon accreditation frameworks undervalue these ecosystems. Supporting the estimation and uptake of high integrity field-derived allochthonous deduction evidence would assist uptake of these frameworks to support implementation of nature-based solutions.https://doi.org/10.1038/s41598-025-12223-zCarbon accreditationBlue carbonGHG mitigationSustainable development goal 13
spellingShingle Emma A. Ward
Sarah E. Reynolds
Melanie J. Leng
Jack H. Lacey
Marianna Cerasuolo
Bronwen Paxton
Federica Ragazzola
Joanne Preston
Mixed provenance of organic carbon in Northeast Atlantic temperate intertidal seagrass sediments
Scientific Reports
Carbon accreditation
Blue carbon
GHG mitigation
Sustainable development goal 13
title Mixed provenance of organic carbon in Northeast Atlantic temperate intertidal seagrass sediments
title_full Mixed provenance of organic carbon in Northeast Atlantic temperate intertidal seagrass sediments
title_fullStr Mixed provenance of organic carbon in Northeast Atlantic temperate intertidal seagrass sediments
title_full_unstemmed Mixed provenance of organic carbon in Northeast Atlantic temperate intertidal seagrass sediments
title_short Mixed provenance of organic carbon in Northeast Atlantic temperate intertidal seagrass sediments
title_sort mixed provenance of organic carbon in northeast atlantic temperate intertidal seagrass sediments
topic Carbon accreditation
Blue carbon
GHG mitigation
Sustainable development goal 13
url https://doi.org/10.1038/s41598-025-12223-z
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