000005022 001__ 5022
000005022 005__ 20180208220105.0
000005022 0247_ $$2DOI$$a10.1016/j.quaint.2009.01.013
000005022 0247_ $$2WOS$$aWOS:000267570100008
000005022 037__ $$aPreJuSER-5022
000005022 041__ $$aeng
000005022 082__ $$a550
000005022 084__ $$2WoS$$aGeography, Physical
000005022 084__ $$2WoS$$aGeosciences, Multidisciplinary
000005022 1001_ $$0P:(DE-HGF)0$$aStriewski, B.$$b0
000005022 245__ $$aMulti-proxy evidence of late Holocene human-induced environmental changes at Lake Pupuke, Auckland (New Zealand)
000005022 260__ $$aAmsterdam [u.a.]$$bElsevier Science$$c2009
000005022 300__ $$a
000005022 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000005022 3367_ $$2DataCite$$aOutput Types/Journal article
000005022 3367_ $$00$$2EndNote$$aJournal Article
000005022 3367_ $$2BibTeX$$aARTICLE
000005022 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000005022 3367_ $$2DRIVER$$aarticle
000005022 440_0 $$013364$$aQuaternary International$$v202$$x1040-6182$$y1
000005022 500__ $$aRecord converted from VDB: 12.11.2012
000005022 520__ $$aNew Zealand was the last major landmass in the world to be colonised by people. Despite the short time-depth of human presence in the country there is ongoing debate about the date of earliest arrival of people that resulted in the emergence of two contrasting colonisation hypotheses: the Early hypothesis and the Short prehistory. To decide between both hypotheses we employed a range of multi-proxy investigations (geochemistry, stable isotopes and mineral magnetism) on a lacustrine sequence from Lake Pupuke, a maar lake in the city of Auckland and an area potentially among the first places in New Zealand to have been colonised by early people. The environmental history reconstructed from the multi-proxy evidence identified a clear lack of catchment disturbance from c. 2000 B.P. until several decades before the eruption of the Rangitoto volcano. The nature and abruptness of disturbance unambiguously point to anthropogenic forcings and are likely to mark the onset of prehistoric human colonisation at the site. Linear interpolation between independently dated tephrochronostratigraphic marker beds present in the sediments allowed to date this event to c. 610 cal yr B.P. This date is in compliance with the Short prehistory for this region. (C) 2009 Elsevier Ltd and INQUA. All rights reserved.
000005022 536__ $$0G:(DE-Juel1)FUEK407$$2G:(DE-HGF)$$aTerrestrische Umwelt$$cP24$$x0
000005022 588__ $$aDataset connected to Web of Science
000005022 650_7 $$2WoSType$$aJ
000005022 7001_ $$0P:(DE-HGF)0$$aMayr, C.$$b1
000005022 7001_ $$0P:(DE-HGF)0$$aFlenley, J.$$b2
000005022 7001_ $$0P:(DE-HGF)0$$aNaumann, R.$$b3
000005022 7001_ $$0P:(DE-HGF)0$$aTurner, G.$$b4
000005022 7001_ $$0P:(DE-Juel1)129567$$aLücke, A.$$b5$$uFZJ
000005022 773__ $$0PERI:(DE-600)2002133-1$$a10.1016/j.quaint.2009.01.013$$gVol. 202$$q202$$tQuaternary international$$v202$$x1040-6182$$y2009
000005022 8567_ $$uhttp://dx.doi.org/10.1016/j.quaint.2009.01.013
000005022 909CO $$ooai:juser.fz-juelich.de:5022$$pVDB
000005022 9131_ $$0G:(DE-Juel1)FUEK407$$bErde und Umwelt$$kP24$$lTerrestrische Umwelt$$vTerrestrische Umwelt$$x0
000005022 9141_ $$y2009
000005022 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000005022 9201_ $$0I:(DE-Juel1)VDB793$$d31.10.2010$$gICG$$kICG-4$$lAgrosphäre$$x1
000005022 970__ $$aVDB:(DE-Juel1)112402
000005022 980__ $$aVDB
000005022 980__ $$aConvertedRecord
000005022 980__ $$ajournal
000005022 980__ $$aI:(DE-Juel1)IBG-3-20101118
000005022 980__ $$aUNRESTRICTED
000005022 981__ $$aI:(DE-Juel1)IBG-3-20101118