000011661 001__ 11661
000011661 005__ 20180208233011.0
000011661 0247_ $$2DOI$$a10.1016/j.quaint.2008.12.009
000011661 0247_ $$2WOS$$aWOS:000274584900004
000011661 037__ $$aPreJuSER-11661
000011661 041__ $$aeng
000011661 082__ $$a550
000011661 084__ $$2WoS$$aGeography, Physical
000011661 084__ $$2WoS$$aGeosciences, Multidisciplinary
000011661 1001_ $$0P:(DE-HGF)0$$aWu, Y.$$b0
000011661 245__ $$aLacustrine radiocarbon reservoir ages in Co Ngoin and Zigê Tangco, central Tibetean Plateau
000011661 260__ $$aAmsterdam [u.a.]$$bElsevier Science$$c2010
000011661 300__ $$a21 - 25
000011661 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000011661 3367_ $$2DataCite$$aOutput Types/Journal article
000011661 3367_ $$00$$2EndNote$$aJournal Article
000011661 3367_ $$2BibTeX$$aARTICLE
000011661 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000011661 3367_ $$2DRIVER$$aarticle
000011661 440_0 $$013364$$aQuaternary International$$v212$$x1040-6182$$y1
000011661 500__ $$aRecord converted from VDB: 12.11.2012
000011661 520__ $$aA series of C-14 ages were made in two lake sediment cores from Co Ngoin and Zige Tangco, central Tibetan Plateau, China, using bulk organic carbon, plant remains, chitin of cladocera, and carbonates. The old C-14 ages of the surface sediments in both cores suggests that there is a significant reservoir effect in these lakes. The magnitude of the reservoir age of different material is variable. Authigenic carbonate has the largest reservoir age, while plant remains and chitin show smaller deviations. Due to a lack of terrestrial macrofossils at most depths, a regression approach was used to obtain the approximate C-14 reservoir correction for bulk organic matter, which is 3260 C-14 BP and 2010 C-14 BP for Co Ngoin and Zige Tingco respectively. (C) 2009 Elsevier Ltd and INQUA. All rights reserved.
000011661 536__ $$0G:(DE-Juel1)FUEK407$$2G:(DE-HGF)$$aTerrestrische Umwelt$$cP24$$x0
000011661 588__ $$aDataset connected to Web of Science
000011661 650_7 $$2WoSType$$aJ
000011661 7001_ $$0P:(DE-HGF)0$$aLi, S.$$b1
000011661 7001_ $$0P:(DE-Juel1)129567$$aLücke, A.$$b2$$uFZJ
000011661 7001_ $$0P:(DE-HGF)0$$aWünnemann, B.$$b3
000011661 7001_ $$0P:(DE-HGF)0$$aZhou, L.$$b4
000011661 7001_ $$0P:(DE-HGF)0$$aReimer, P.$$b5
000011661 7001_ $$0P:(DE-HGF)0$$aWang, S.$$b6
000011661 773__ $$0PERI:(DE-600)2002133-1$$a10.1016/j.quaint.2008.12.009$$gVol. 212, p. 21 - 25$$p21 - 25$$q212<21 - 25$$tQuaternary international$$v212$$x1040-6182$$y2010
000011661 8567_ $$uhttp://dx.doi.org/10.1016/j.quaint.2008.12.009
000011661 909CO $$ooai:juser.fz-juelich.de:11661$$pVDB
000011661 9131_ $$0G:(DE-Juel1)FUEK407$$bErde und Umwelt$$kP24$$lTerrestrische Umwelt$$vTerrestrische Umwelt$$x0
000011661 9141_ $$y2010
000011661 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000011661 9201_ $$0I:(DE-Juel1)VDB793$$d31.10.2010$$gICG$$kICG-4$$lAgrosphäre$$x1
000011661 970__ $$aVDB:(DE-Juel1)122948
000011661 980__ $$aVDB
000011661 980__ $$aConvertedRecord
000011661 980__ $$ajournal
000011661 980__ $$aI:(DE-Juel1)IBG-3-20101118
000011661 980__ $$aUNRESTRICTED
000011661 981__ $$aI:(DE-Juel1)IBG-3-20101118