georefid:2013-008209SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2013-07-08T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1002/jqs.15672012-01-01publicationgeorefid:2013-008209doi:10.1002/jqs.1567Maslin, Mark A.University College London, Environmental Change Research Centre, London, United KingdomauthorEttwein, Virginia J.University of Bristol, United KingdomauthorBoot, Christopher S.University of Glasgow, United KingdomauthorBendle, JamesauthorPancost, Richard D.authorJohn Wiley and Sons for the Quaternary Research Association, Chichester, United KingdompublisherdocumentHardcopyJQS. Journal of Quaternary Science27 (5)451-460Ocean Drilling Program Leg 155 Site 942 on the Amazon Fan is an ideal location for monitoring palaeoclimatic changes within a significant proportion of the Amazon Basin. We present n-alkane delta (super 13) C and taraxerol and laevoglucosan concentration records from this site covering the last 38 ka. The entire n-alkane delta (super 13) C record is constrained between -31 ppm and -34 ppm, which is well within the isotopic range occupied by C (sub 3) vegetation. The concentration and relative abundance of taraxerol, a mangrove indicator, varies by over an order of magnitude, but seems to have had no effect on the n-alkane delta (super 13) C record. The laevoglucosan concentrations are extremely low during the last glacial period, suggesting a relatively low occurrence of forest fires. Laevoglucosan concentrations are highest between 13.5 and 12.5 ka, suggesting an increased incidence of Amazon forest fires at the very end of the Younger Dryas. These records, combined with previously published pollen records from Site 932, reveal no evidence for massive incursions of grasslands into Amazonia during the last glacial period, despite evidence of reduced outflow of the Amazon River indicating more arid conditions. We therefore suggest that savannah encroachment, as proposed by the Pleistocene refuge hypothesis, can be refuted as an explanation for high species endemism within the Amazon Basin, and alternative explanations are required. Abstract Copyright (2010), John Wiley & Sons, Ltd.completedIsotope geochemistryQuaternary geologyaliphatic hydrocarbonsalkanesAmazon FanAtlantic OceanbiochemistrybiomarkersC-13/C-12carbonCenozoicchemical compositionEquatorial Atlanticfiresforestshydrocarbonsisotope ratiosisotopesLeg 155n-alkanesNorth AtlanticOcean Drilling ProgramODP Site 942organic compoundspaleoecologypaleoenvironmentPleistoceneQuaternaryrain forestsrefugiastable isotopesupper Pleistoceneupper WeichselianWeichselianYounger Dryasurn:org.iodp:exp:155urnlargerWorkCitationcampaignurn:org.iodp:exp:155:site:942urnlargerWorkCitationstudyurn:org.iodp:exp:155urnlargerWorkCitationcampaignEnglishgeoscientificInformation-49.0528-49.05285.44335.4433