Identificador persistente para citar o vincular este elemento: https://accedacris.ulpgc.es/jspui/handle/10553/156937
Campo DC Valoridioma
dc.contributor.authorEgea, L.G.en_US
dc.contributor.authorInfantes Oanes, Eduardoen_US
dc.contributor.authorJiménez-Ramos, R.en_US
dc.date.accessioned2026-02-03T16:59:23Z-
dc.date.available2026-02-03T16:59:23Z-
dc.date.issued2023en_US
dc.identifier.issn0048-9697en_US
dc.identifier.urihttps://accedacris.ulpgc.es/jspui/handle/10553/156937-
dc.description.abstractCoastal development and climate change are sparking growing concern about the vulnerability of the organic carbon (OC) stocks in marine sediments to remineralization, especially in high threaten coastal ecosystems like seagrass meadows. Uncertainties still exist regarding the role played by hydrodynamics, seagrass canopies and sediment properties in OC resuspension and remineralization. A set of laboratory experiments were conducted to assess, for the first time, the mechanisms by which the particulate and dissolved organic carbon (POC and DOC) may be released and remineralized under hydrodynamic conditions (i.e., unidirectional and oscillatory flows) in two eelgrass densities and sediments properties (i.e., grain size and OC content). After a gradually increase in hydrodynamic forces, our results demonstrated that the presence of eelgrass reduced sediment erosion and OC loss in high-density canopies, while low-density canopies promote OC resuspension (on average, 1.8-fold higher than high-density canopies). We also demonstrated that unidirectional and oscillatory flows released similar DOC from surface sediments (on average, 15.5 ± 1.4 and 18.4 ± 1.8 g m−2, respectively), whereas oscillatory flow released significantly more POC than unidirectional flows (from 10.8 ± 1.1 to 32.1 ± 5.6 g m−2 for unidirectional and oscillatory flows, respectively). POC and DOC released was strongly influenced by both seagrass meadow structure (i.e., lower eelgrass density and shoot area) and sediment properties (i.e., lower mud and higher sediment water content). We found that, although >74 % of OC in upper sediments was remineralized within 30 days, a relatively high amount of OC in high-density canopies is recalcitrant, highlighting its potential for the formation of blue carbon deposits. This study highlights the vulnerability of OC deposits in seagrass sediments to resuspension if the meadow is degraded and/or the climate change yield stronger storms, which could potentially weaken the seagrass meadows' service as blue carbon ecosystem in the future.en_US
dc.languageengen_US
dc.relation.ispartofScience of the Total Environmenten_US
dc.sourceScience of the Total Environment [ISSN 0048-9697], v. 901 (Noviembre 2023)en_US
dc.subject251004 Botánica marinaen_US
dc.subject.otherBlue carbonen_US
dc.subject.otherOscillatory flowen_US
dc.subject.otherUnidirectional flowen_US
dc.subject.otherRemineralizationen_US
dc.subject.otherSediment erosion Zostera marinaen_US
dc.subject.otherZostera marinaen_US
dc.titleLoss of POC and DOC on seagrass sediments by hydrodynamicsen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.scitotenv.2023.165976en_US
dc.relation.volume901en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.description.numberofpages12en_US
dc.utils.revisionen_US
dc.date.coverdateNoviembre 2023en_US
dc.identifier.ulpgcNoen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.sjr1,998
dc.description.jcr8,2
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
dc.description.miaricds11,0
item.fulltextCon texto completo-
item.grantfulltextopen-
crisitem.author.deptDepartamento de Biología-
crisitem.author.orcid0000-0002-9724-9237-
crisitem.author.fullNameInfantes Oanes, Eduardo-
Colección:Artículos
Adobe PDF (5,39 MB)
Vista resumida

Citas de WEB OF SCIENCETM
Citations

34
actualizado el 05-abr-2026

Google ScholarTM

Verifica

Altmetric


Comparte



Exporta metadatos



Los elementos en ULPGC accedaCRIS están protegidos por derechos de autor con todos los derechos reservados, a menos que se indique lo contrario.