000057072 001__ 57072
000057072 005__ 20190625112131.0
000057072 0247_ $$2DOI$$a10.1016/j.quaint.2006.05.029
000057072 0247_ $$2WOS$$aWOS:000242432600008
000057072 0247_ $$2altmetric$$aaltmetric:3670418
000057072 037__ $$aPreJuSER-57072
000057072 041__ $$aeng
000057072 082__ $$a550
000057072 084__ $$2WoS$$aGeography, Physical
000057072 084__ $$2WoS$$aGeosciences, Multidisciplinary
000057072 1001_ $$0P:(DE-HGF)0$$aHaberzettl, T.$$b0
000057072 245__ $$aEnvironmental change and fire history of southern Patagonia (Argentina) during the last five centuries
000057072 260__ $$aAmsterdam [u.a.]$$bElsevier Science$$c2006
000057072 300__ $$a72 - 82
000057072 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000057072 3367_ $$2DataCite$$aOutput Types/Journal article
000057072 3367_ $$00$$2EndNote$$aJournal Article
000057072 3367_ $$2BibTeX$$aARTICLE
000057072 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000057072 3367_ $$2DRIVER$$aarticle
000057072 440_0 $$013364$$aQuaternary International$$v158$$x1040-6182$$y1
000057072 500__ $$aRecord converted from VDB: 12.11.2012
000057072 520__ $$aGeochemical, geophysical, charcoal and pollen analyses from the very poorly investigated southern Patagonian steppe area show that in the vicinity of Laguna Potrok Aike (Santa Cruz Province, Argentina) and north of the Strait of Magellan the detectable impact of Europeans as explorers, settlers and farmers on fire intensity, vegetation and lake ecosystems started with first regional signs during the 1840s. A massive anthropogenic impact on a supra-regional scale followed as the result of the introduction of sheep farming at the end of the 19th century. Furthermore, since the first European explorations, fires in the steppe areas of southernmost Patagonia as recorded at Laguna Potrok Aike occurred contemporaneously in the steppe-forest ecotone further west and probably also in the Andean forest itself. Environmental changes which are not caused by anthropogenic influence are also revealed and were most likely the result of temperature variations and enhanced and reduced wind speeds, respectively. A fire event around AD 1600, before the arrival of European settlers, occurred during a dry period in the forest and steppe-forest ecotone and followed a wet phase in the steppe that caused favorable ignition conditions in all environments. (c) 2006 Elsevier Ltd and INQUA. All rights reserved.
000057072 536__ $$0G:(DE-Juel1)FUEK405$$2G:(DE-HGF)$$aGeosysteme - Erde im Wandel$$cP21$$x0
000057072 588__ $$aDataset connected to Web of Science
000057072 650_7 $$2WoSType$$aJ
000057072 7001_ $$0P:(DE-HGF)0$$aWille, M.$$b1
000057072 7001_ $$0P:(DE-HGF)0$$aFey, M$$b2
000057072 7001_ $$0P:(DE-HGF)0$$aJanssen, S.$$b3
000057072 7001_ $$0P:(DE-Juel1)129567$$aLücke, A.$$b4$$uFZJ
000057072 7001_ $$0P:(DE-Juel1)VDB57755$$aMayr, C.$$b5$$uFZJ
000057072 7001_ $$0P:(DE-HGF)0$$aOhlendorf, C.$$b6
000057072 7001_ $$0P:(DE-HGF)0$$aSchäbitz, F.$$b7
000057072 7001_ $$0P:(DE-Juel1)VDB1420$$aSchleser, G. H.$$b8$$uFZJ
000057072 7001_ $$0P:(DE-HGF)0$$aZolitschka, B.$$b9
000057072 773__ $$0PERI:(DE-600)2002133-1$$a10.1016/j.quaint.2006.05.029$$gVol. 158, p. 72 - 82$$p72 - 82$$q158<72 - 82$$tQuaternary international$$v158$$x1040-6182$$y2006
000057072 8567_ $$uhttp://dx.doi.org/10.1016/j.quaint.2006.05.029
000057072 909CO $$ooai:juser.fz-juelich.de:57072$$pVDB
000057072 9131_ $$0G:(DE-Juel1)FUEK405$$bUmwelt$$kP21$$lGeosysteme - Erde im Wandel$$vGeosysteme - Erde im Wandel$$x0
000057072 9141_ $$aNachtrag$$y2006
000057072 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000057072 9201_ $$0I:(DE-Juel1)VDB51$$d31.12.2006$$gICG$$kICG-V$$lSedimentäre Systeme$$x1
000057072 970__ $$aVDB:(DE-Juel1)89784
000057072 980__ $$aVDB
000057072 980__ $$aConvertedRecord
000057072 980__ $$ajournal
000057072 980__ $$aI:(DE-Juel1)ICG-5-20090406
000057072 980__ $$aUNRESTRICTED
000057072 981__ $$aI:(DE-Juel1)ICG-5-20090406