Please use this identifier to cite or link to this item: http://bura.brunel.ac.uk/handle/2438/10242
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dc.contributor.authorSilva-Sánchez, N-
dc.contributor.authorMartínez Cortizas, A-
dc.contributor.authorLópez-Merino, L-
dc.date.accessioned2015-02-16T12:29:54Z-
dc.date.available2014-
dc.date.available2015-02-16T12:29:54Z-
dc.date.issued2014-
dc.identifier.citationHolocene, 24 (6): 714 - 725, (2014)en_US
dc.identifier.issn0959-6836-
dc.identifier.issn1477-0911-
dc.identifier.urihttp://hol.sagepub.com/content/24/6/714-
dc.identifier.urihttp://bura.brunel.ac.uk/handle/2438/10242-
dc.descriptionThis article is distributed under the terms of the Creative Commons Attribution-NonCommercial 3.0 License (http://www.creativecommons.org/licenses/by-nc/3.0/) which permits non-commercial use, reproduction and distribution of the work without further permission provided the original work is attributed as specified on the SAGE and Open Access page (http://www.uk.sagepub.com/aboutus/openaccess.htm).en_US
dc.descriptionThis article has been made available through the Brunel Open Access Publishing Fund.-
dc.description.abstractForest clearance is one of the main drivers of soil erosion and hydrological changes in mires, although climate may also play a significant role. Because of the wide range of factors involved, understanding these complex links requires long-term multi-proxy approaches and research on the best proxies to focus. A peat core from NW Spain (Cruz do Bocelo mire), spanning the last ~3000 years, has been studied at high resolution by physical (density and loss on ignition (LOI)), geochemical (elemental composition) and palynological (pollen and non-pollen palynomorphs) analyses. Proxies related to mineral matter fluxes from the catchment (lithogenic tracers, Glomus and Entorrhiza), rainfall (Bromine), mire hydrology (HdV-18), human pressure (Cerealia-type, nitrophilous taxa and coprophilous fungi) and forest cover (mesophilous tree taxa) were the most useful to reconstruct the evolution of the mire and its catchment. Forest clearance for farming was one of the main drivers of environmental change from at least the local Iron Age (~2685 cal. yr BP) onwards. The most intense phase of deforestation occurred during Roman and Germanic times and the late Middle Ages. During these phases, the entire catchment was affected, resulting in enhanced soil erosion and severe hydrological modifications of the mire. Climate, especially rainfall, may have also accelerated these processes during wetter periods. However, it is noteworthy that the hydrology of the mire seems to have been insensitive to rainfall variations when mesophilous forest dominated. Abrupt changes were only detected once intense forest clearance commenced during the Iron Age/Roman transition (~2190 cal. yr BP) phase, which represented a tipping point in catchment's ability to buffer impacts. Overall, our findings highlight the importance of studying ecosystems' long-term trajectories and catchment-wide processes when implementing mire habitat protection measures.en_US
dc.description.sponsorshipThis work was funded by the projects CGL2010-20672 (Plan Nacional I+D+i, Spanish Ministry of Science and Innovation) and 10PXIB200182PR (General Directorate of I+D, Xunta de Galicia). N Silva-Sánchez and L López-Merino are currently supported by a FPU predoctoral scholarship (AP2010-3264) funded by the Spanish Government and a MINT postdoctoral fellowship funded by the Brunel Institute for the Environment, respectively.en_US
dc.format.extent714 - 725-
dc.format.extent714 - 725-
dc.languageeng-
dc.language.isoenen_US
dc.publisherSAGE Publications Ltden_US
dc.subjectCatchment hydrologyen_US
dc.subjectDeforestationen_US
dc.subjectGeochemistryen_US
dc.subjectHdV-18en_US
dc.subjectNon-pollen palynomorphsen_US
dc.subjectPollenen_US
dc.subjectPrincipal components analysisen_US
dc.subjectSoil erosionen_US
dc.titleLinking forest cover, soil erosion and mire hydrology to late-Holocene human activity and climate in NW Spainen_US
dc.typeArticleen_US
dc.identifier.doihttp://dx.doi.org/10.1177/0959683614526934-
dc.relation.isPartOfHolocene-
dc.relation.isPartOfHolocene-
pubs.issue6-
pubs.issue6-
pubs.volume24-
pubs.volume24-
pubs.organisational-data/Brunel-
pubs.organisational-data/Brunel/Brunel Staff by College/Department/Division-
pubs.organisational-data/Brunel/Brunel Staff by College/Department/Division/College of Health and Life Sciences-
pubs.organisational-data/Brunel/Brunel Staff by College/Department/Division/College of Health and Life Sciences/Dept of Life Sciences-
pubs.organisational-data/Brunel/Brunel Staff by College/Department/Division/College of Health and Life Sciences/Dept of Life Sciences/Biological Sciences-
pubs.organisational-data/Brunel/Brunel Staff by Institute/Theme-
pubs.organisational-data/Brunel/Brunel Staff by Institute/Theme/Institute of Environmental, Health and Societies-
pubs.organisational-data/Brunel/Brunel Staff by Institute/Theme/Institute of Environmental, Health and Societies/Health and Environment-
pubs.organisational-data/Brunel/Specialist Centres-
pubs.organisational-data/Brunel/Specialist Centres/IfE-
Appears in Collections:Brunel OA Publishing Fund
Institute for the Environment

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