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dc.creatorCastillo Segura, Jesús Manueles
dc.creatorGallego Tévar, Blancaes
dc.creatorCastellanos, Eloy M.es
dc.creatorFigueroa Clemente, Manuel Enriquees
dc.creatorDavy, Anthony J.es
dc.date.accessioned2021-12-16T15:31:07Z
dc.date.available2021-12-16T15:31:07Z
dc.date.issued2021
dc.identifier.citationCastillo Segura, J.M., Gallego Tévar, B., Castellanos, E.M., Figueroa Clemente, M.E. y Davy, A.J. (2021). Primary succession in an Atlantic salt marsh: From intertidal flats to mid-marsh platform in 35 years. Journal of Ecology, 109 (8), 2909-2921.
dc.identifier.issn0022-0477es
dc.identifier.issn1365-2745es
dc.identifier.urihttps://hdl.handle.net/11441/128339
dc.description.abstractAlthough salt marsh is a classic example of primary succession, the underlying mechanisms and their time-scales are poorly understood. As salt marsh succession depends on sediment accretion, the amelioration of abiotic conditions associated with increasing elevation suggests potential explanatory roles for facilitation, competition and the stress-gradient hypothesis. We present a 35-year longitudinal study of salt marsh development from intertidal flat to a mid-marsh platform at Odiel Marshes in south-western Iberia. Using permanent plots, this work chronicles changes in elevation and marsh morphology, their evolving effects on sediment redox potential and salinity and the colonisation and changing patterns of dominance of halophytic species. Sporadically colonising clumps of the low-marsh species Spartina maritima trapped sediment to form raised tussocks, which increased in elevation and area. Reduced tidal inundation and locally improved drainage promoted higher redox potentials and allowed colonisation by a sequence of species less tolerant of reducing conditions: Sarcocornia perennis, its hybrid with high-marsh S. fruticosa, and Atriplex portulacoides. Unlike its centrifugally colonising predecessors, A. portulacoides invaded from the tussock edges. Transplant experiments designed to investigate its late establishment on tussocks showed that seedling survival depended on elevational differences as small as 4 cm. After increasing in elevation by c. 1 m (c. 29 mm/year), coalescence of the tussocks formed a marsh platform at a level corresponding to mean high tides. This supports a theoretical punctuated transition from ‘submergence marsh’ to ‘emergence marsh’, previously postulated for this tidal elevation. Synthesis. The unexpected rapidity of this primary succession highlights the central role of facilitation. Vertical sediment accretion, locally engineered by colonising species, progressively alleviates abiotic stress and allows colonisation by species that are less tolerant of chemically reducing conditions but are ultimately better competitors.es
dc.formatapplication/pdfes
dc.format.extent13 p.es
dc.language.isoenges
dc.publisherWiley-Blackwelles
dc.relation.ispartofJournal of Ecology, 109 (8), 2909-2921.
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectAtriplex portulacoideses
dc.subjectElevationes
dc.subjectEmergence marshes
dc.subjectFacilitationes
dc.subjectInvasiones
dc.subjectRedox potentiales
dc.subjectSediment accretiones
dc.subjectStress-gradient hypothesises
dc.titlePrimary succession in an Atlantic salt marsh: From intertidal flats to mid-marsh platform in 35 yearses
dc.typeinfo:eu-repo/semantics/articlees
dcterms.identifierhttps://ror.org/03yxnpp24
dc.type.versioninfo:eu-repo/semantics/publishedVersiones
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Biología Vegetal y Ecologíaes
dc.relation.publisherversionhttps://doi.org/10.1111/1365-2745.13692es
dc.identifier.doi10.1111/1365-2745.13692es
dc.journaltitleJournal of Ecologyes
dc.publication.volumen109es
dc.publication.issue8es
dc.publication.initialPage2909es
dc.publication.endPage2921es

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