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dc.contributor.authorEspinar, José L.-
dc.contributor.authorSerrano, Laura-
dc.date.accessioned2011-07-28T11:59:18Z-
dc.date.available2011-07-28T11:59:18Z-
dc.date.issued2009-
dc.identifier.citationAquatic Ecology 43 (2): 323-334 (2009)es_ES
dc.identifier.issn1386-2588-
dc.identifier.urihttp://hdl.handle.net/10261/38094-
dc.description12 páginas, 3 figuras, 3 tablas, 36 referencias, 1 apéndice: 2 anexos.es_ES
dc.description.abstractA quantitative hydrogeomorphic approach was applied to an extensive survey of temporary wetlands in the Doñana National Park (SW Spain) in search for quantitative thresholds for wetland classification. Twenty freshwater ponds on the aeolian sand mantle and 46 sites on silty-clay substrate, located in the southern marshland, were surveyed during the heaviest rainy period so far recorded (October 1995–September 1997). On average, temporary ponds showed higher water depth, longer flooding period, lower conductivity (\0.5 mS cm-1), lower pH (6.7), lower phosphate concentration (0.4 lM) and amore balanced proportion of Ca2+/Na+ than temporary marshes. During floods, marshland sites exhibited higher water transparency, pH (9.5), alkalinity (3.5 meq l-1), conductivity (8.2 mS cm-1), phosphate concentration (0.7 lM), Na+ and Ca2+ concentrations (97.2 and 3.5 meq l-1, respectively) than ponds. Study sites were significantly segregated (ANOSIM test: R = 0.88, P\0.01, n = 92) in relation to water depth and conductivity. A conductivity of 1.6 mS cm-1 is proposed as a threshold between marshland sites and ponds during floods. Marshland sites were further segregated into two groups (ANOSIM test: R = 0.777, P\0.01, n = 23) according to the Na+/Ca2+ ratio (in meq l-1) at a threshold value of 25. An ordination by PCA showed that five variables grouped 81.4%of the total variance in two axes. The first PCA axis (60.7% of variance) separated temporary wetlands into ponds andmarshland sites according to variables related to substrate and hydrology (Na+/Ca2+ ratio, conductivity, water depth and flooding period). Other variables (e.g., water transparency, alkalinity, pH, submersed macrophyte biomass, phosphate, nitrate and planktonic chlorophyll concentrations) did not produce a significant segregation between marshland and pond sites during floods. Further discrimination within each wetland type was thus not achieved.es_ES
dc.description.sponsorshipFinancial support came from the Spanish Ministry of the Environment (MMA, project 05/99), CICYT (AMB95-1054) and the Junta de Andalucía (research groups #4086 and 4033).es_ES
dc.language.isoenges_ES
dc.publisherSpringer Naturees_ES
dc.rightsclosedAccesses_ES
dc.subjectHydroperiodes_ES
dc.subjectMacrophyteses_ES
dc.subjectMediterranean wetlandses_ES
dc.subjectMultivariate analyseses_ES
dc.subjectSalinityes_ES
dc.titleA quantitative hydrogeomorphic approach to the classification of temporary wetlands in the Doñana National Park (SW Spain)es_ES
dc.typeartículoes_ES
dc.identifier.doi10.1007/s10452-007-9162-7-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1007/s10452-007-9162-7es_ES
dc.contributor.funderMinisterio de Medio Ambiente (España)-
dc.contributor.funderJunta de Andalucía-
dc.identifier.funderhttp://dx.doi.org/10.13039/501100011011es_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairetypeartículo-
item.grantfulltextnone-
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextNo Fulltext-
item.languageiso639-1en-
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