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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00008845naa a2200937 4500
001oai:DiVA.org:lnu-68286
003SwePub
008171011s2017 | |||||||||||000 ||eng|
009oai:lup.lub.lu.se:ad8042ce-a7e2-429e-ad09-fa9675074298
024a https://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-682862 URI
024a https://doi.org/10.1016/j.quascirev.2017.07.0012 DOI
024a https://lup.lub.lu.se/record/ad8042ce-a7e2-429e-ad09-fa96750742982 URI
040 a (SwePub)lnud (SwePub)lu
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Marquer, Laurentu Linnaeus University,Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science,University of Toulouse4 aut0 (Swepub:lu)nate-lam
2451 0a Quantifying the effects of land use and climate on Holocene vegetation in Europe
264 1b Pergamon Press,c 2017
338 a print2 rdacarrier
520 a Early agriculture can be detected in palaeovegetation records, but quantification of the relative importance of climate and land use in influencing regional vegetation composition since the onset of agriculture is a topic that is rarely addressed. We present a novel approach that combines pollen-based REVEALS estimates of plant cover with climate, anthropogenic land-cover and dynamic vegetation modelling results. This is used to quantify the relative impacts of land use and climate on Holocene vegetation at a sub-continental scale, i.e. northern and western Europe north of the Alps. We use redundancy analysis and variation partitioning to quantify the percentage of variation in vegetation composition explained by the climate and land-use variables, and Monte Carlo permutation tests to assess the statistical significance of each variable. We further use a similarity index to combine pollen based REVEALS estimates with climate-driven dynamic vegetation modelling results. The overall results indicate that climate is the major driver of vegetation when the Holocene is considered as a whole and at the sub-continental scale, although land use is important regionally. Four critical phases of land-use effects on vegetation are identified. The first phase (from 7000 to 6500 BP) corresponds to the early impacts on vegetation of farming and Neolithic forest clearance and to the dominance of climate as a driver of vegetation change. During the second phase (from 4500 to 4000 BP), land use becomes a major control of vegetation. Climate is still the principal driver, although its influence decreases gradually. The third phase (from 2000 to 1500 BP) is characterised by the continued role of climate on vegetation as a consequence of late-Holocene climate shifts and specific climate events that influence vegetation as well as land use. The last phase (from 500 to 350 BP) shows an acceleration of vegetation changes, in particular during the last century, caused by new farming practices and forestry in response to population growth and industrialization. This is a unique signature of anthropogenic impact within the Holocene but European vegetation remains climatically sensitive and thus may continue to respond to ongoing climate change. (C) 2017 Elsevier Ltd. All rights reserved.
650 7a NATURVETENSKAPx Biologix Ekologi0 (SwePub)106112 hsv//swe
650 7a NATURAL SCIENCESx Biological Sciencesx Ecology0 (SwePub)106112 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Annan geovetenskap och miljövetenskap0 (SwePub)105992 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Other Earth and Related Environmental Sciences0 (SwePub)105992 hsv//eng
653 a Climate
653 a Holocene
653 a Human impact
653 a Land use
653 a LPJ-GUESS
653 a Europe
653 a Pollen
653 a REVEALS
653 a Vegetation composition
653 a Paleoecology
653 a Paleoekologi
653 a Climate
653 a Europe
653 a Holocene
653 a Human impact
653 a Land use
653 a LPJ-GUESS
653 a Pollen
653 a REVEALS
653 a Vegetation composition
700a Gaillard, Marie-José,d 1953-u Linnaeus University,Linnéuniversitetet,Institutionen för biologi och miljö (BOM)4 aut0 (Swepub:lnu)egama
700a Sugita, Shinyau Tallinn Univ, Estonia,Tallinn University4 aut
700a Poska, Anneliu Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science,Tallinn University of Technology4 aut0 (Swepub:lu)nate-aep
700a Trondman, Anna-Kari,d 1980-u Linnaeus University,Linnéuniversitetet,Institutionen för biologi och miljö (BOM)4 aut0 (Swepub:lnu)etran
700a Mazier, Florenceu Univ Toulouse Jean Jaures, France,University of Toulouse-Jean Jaurès4 aut0 (Swepub:lu)geol-flm
700a Nielsen, Anne Birgitteu Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Institutionen för naturgeografi och ekosystemvetenskap,Quaternary Sciences,Department of Geology,Faculty of Science,Dept of Physical Geography and Ecosystem Science4 aut0 (Swepub:lu)geol-ans
700a Fyfe, Ralph M.u Univ Plymouth, UK,Plymouth University4 aut
700a Jönsson, Anna Mariau Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science4 aut0 (Swepub:lu)ple-amj
700a Smith, Benjaminu Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science4 aut0 (Swepub:lu)ple-bsm
700a Kaplan, Jed O.u Ecole Polytech Fed Lausanne, Switzerland,Swiss Federal Institute of Technology4 aut0 (Swepub:lu)extLU-697
700a Alenius, Teijau Univ Helsinki, Finland;Univ Turku, Finland,University of Turku,University of Helsinki4 aut
700a Birks, H. John B.u Univ Bergen, Norway;UCL, UK,University College London,University of Bergen4 aut
700a Bjune, Anne E.u Univ Bergen, Norway;Uni Res Climate, Norway,Uni Research AS,University of Bergen4 aut
700a Christiansen, Jorgu Univ Göttingen, Germany,University of Göttingen4 aut
700a Dodson, Johnu Univ Wollongong, Australia;Chinese Acad Sci, Peoples Republic of China,Institute of Earth Environment, Chinese Academy of Sciences,University of Wollongong4 aut
700a Edwards, Kevin J.u Univ Aberdeen, UK;Univ Cambridge, UK,University of Cambridge,University of Aberdeen4 aut
700a Giesecke, Thomasu Univ Göttingen, Germany,University of Göttingen4 aut
700a Herzschuh, Ulrikeu Univ Potsdam, Germany,University of Potsdam4 aut
700a Kangur, Mihkelu Tallinn Univ, Estonia,Tallinn University4 aut
700a Koff, Tiiuu Tallinn Univ, Estonia,Tallinn University4 aut
700a Latalowa, Maligorzatau Univ Gdansk, Poland,University of Gdansk4 aut
700a Lechterbeck, Juttau Univ Stavanger, Norway,University of Stavanger4 aut
700a Olofsson, Jörgenu Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science4 aut0 (Swepub:lu)nate-jol
700a Seppa, Heikkiu Univ Helsinki, Finland,University of Helsinki4 aut
710a Institutionen för naturgeografi och ekosystemvetenskapb Naturvetenskapliga fakulteten4 org
773t Quaternary Science Reviewsd : Pergamon Pressg 171, s. 20-37q 171<20-37x 0277-3791x 1873-457X
856u https://hal-univ-tlse2.archives-ouvertes.fr/hal-01831098/file/QSR2017QuantifyingeffectsoflanduseandclimateEurope_Marqueretal_cor.pdf
856u http://dx.doi.org/10.1016/j.quascirev.2017.07.001y FULLTEXT
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-68286
8564 8u https://doi.org/10.1016/j.quascirev.2017.07.001
8564 8u https://lup.lub.lu.se/record/ad8042ce-a7e2-429e-ad09-fa9675074298

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