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http://hdl.handle.net/10261/212924
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Campo DC | Valor | Lengua/Idioma |
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dc.contributor.author | Badía-Villas, D. | es_ES |
dc.contributor.author | Buendía-García, L. | es_ES |
dc.contributor.author | Longares Aladrén, Luis Alberto | es_ES |
dc.contributor.author | Martí Dalmau, C. | es_ES |
dc.contributor.author | Peña Monné, José Luis | es_ES |
dc.contributor.author | González-Pérez, José Antonio | es_ES |
dc.contributor.author | Gómez García, Daniel | es_ES |
dc.date.accessioned | 2020-06-02T06:21:09Z | - |
dc.date.available | 2020-06-02T06:21:09Z | - |
dc.date.issued | 2020-09-10 | - |
dc.identifier.citation | Science of The Total Environment 734: 139121 (2020) | es_ES |
dc.identifier.issn | 0048-9697 | - |
dc.identifier.uri | http://hdl.handle.net/10261/212924 | - |
dc.description | 13 páginas.- 10 figuras. - 1 tabla.- referencias.- Supplementary data to this article can be found online athttps://doi.org/10.1016/j.scitotenv.2020.139121 | es_ES |
dc.description.abstract | The two most widely extended mountain grasslands in Europe (Nardus-mat grasslands and chalk grasslands) are distributed forming complex patterns. In the Ordesa and Monte Perdido National Park (Central Pyrenees, NE-Spain), they grow as secondary pastures within the treeline ecotone at the subalpine belt. This work aims to show the influence of soil properties on the spatial distribution of these pastures, under a dynamic geomorphology. Soils are sampled under both grasslands, which grow on different cumulative levels: Nardus-mat grasslands in the upper level (L1) and chalk grasslands in the lower level (L2). Soils in L1 have a significantly higher acidity, lower soluble ions and exchangeable calcium content than those in L2, reflecting a more intense leaching process, consistent with a longer period of slope stability. Qualitative differences are detected in the soil organic matter of the soil, using carbon and nitrogen isotopes, lighter in L2 soils than in L1 soils, due to a higher proportion of legumes growing in L2 (chalk grasslands). Soils in L1 and L2 shared many physical properties, such as a fine and homogeneous texture in the whole profile (silty clay or silty clay loam), and high aggregate stability and porosity in the topsoil. In contrast, the soils in L2 are shallower than in L1, which reduces their water-holding capacity. The soil is classified as Orthoeutric Cambisol (Clayic, Humic) in L1 but its rejuvenation, by gully erosion, transforms it into an Hypereutric Leptosol (Loamic, Ochric) in L2 (Typic Haplocryept and Lithic Haplocryept, respectively by Soil Taxonomy system). Definitely, the distribution of both grasslands for the studied area is linked to two cumulative levels of different ages, which in turn is strongy related to different soil properties. | es_ES |
dc.description.sponsorship | This study is part of the results of a microproject funded by the “Instituto de Estudios Altoaragoneses-Diputación de Huesca (Call 2018). Lucía Buendía was supported by a novel research contract, funded by the Institute for Research into Environmental Sciences (IUCA) of the University of Zaragoza. This work has been partially financed by the Regional Government of Aragón (Geoforest research group S51_17R) co-financed with FEDER 2014-2020 “Construyendo Europa desde Aragón”. The authors would also like to thank Federico Fillat for his help in the field and for their constructive comments and suggestions, which led to a substantial improvement of the paper. | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | Elsevier | es_ES |
dc.relation.isversionof | Postprint | - |
dc.relation.isversionof | Postprint | - |
dc.rights | openAccess | en_EN |
dc.subject | Cumulative levels | es_ES |
dc.subject | Nardus-mat grasslands | es_ES |
dc.subject | Soil formation | es_ES |
dc.subject | Soil classification | es_ES |
dc.subject | Late Holocene | es_ES |
dc.title | Soil-geomorphology relationships determine the distribution of the main subalpine grasslands in the Central Pyrenees (NE-Spain) | es_ES |
dc.type | artículo | es_ES |
dc.identifier.doi | 10.1016/j.scitotenv.2020.139121 | - |
dc.description.peerreviewed | Peer reviewed | es_ES |
dc.relation.publisherversion | http://dx.doi.org/10.1016/j.scitotenv.2020.139121 | es_ES |
dc.identifier.e-issn | 1879-1026 | - |
dc.embargo.terms | 2022-09-10 | - |
dc.embargo.terms | 2022-09-10 | - |
dc.contributor.funder | Instituto de Estudios Altoaragoneses | es_ES |
dc.contributor.funder | Universidad de Zaragoza | es_ES |
dc.contributor.funder | Gobierno de Aragón | es_ES |
dc.relation.csic | Sí | es_ES |
oprm.item.hasRevision | no ko 0 false | * |
dc.identifier.funder | http://dx.doi.org/10.13039/501100007041 | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100010067 | es_ES |
dc.contributor.orcid | Badía-Villas, D. [0000-0002-1006-5030] | es_ES |
dc.contributor.orcid | Martí Dalmau, C. | es_ES |
dc.contributor.orcid | González-Pérez, José Antonio [0000-0001-7607-1444] | es_ES |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.languageiso639-1 | en | - |
item.fulltext | With Fulltext | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.cerifentitytype | Publications | - |
item.grantfulltext | open | - |
item.openairetype | artículo | - |
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Soil_geomorphology_relationships_determine_distribution_2020_Posprint.pdf | 889,83 kB | Adobe PDF | Visualizar/Abrir |
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