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dc.contributor.authorSchildgen, Taylor F.
dc.contributor.authorRobinson, Ruth A. J.
dc.contributor.authorSavi, Sara
dc.contributor.authorPhillips, William M.
dc.contributor.authorSpencer, Joel Q. G.
dc.contributor.authorBookhagen, Bodo
dc.contributor.authorScherler, Dirk
dc.contributor.authorTofelde, Stefanie
dc.contributor.authorAlonso, Ricardo N.
dc.contributor.authorKubik, Peter W.
dc.contributor.authorBinnie, Steven A.
dc.contributor.authorStrecker, Manfred R.
dc.date.accessioned2016-08-23T23:33:47Z
dc.date.available2016-08-23T23:33:47Z
dc.date.issued2016-02
dc.identifier.citationSchildgen , T F , Robinson , R A J , Savi , S , Phillips , W M , Spencer , J Q G , Bookhagen , B , Scherler , D , Tofelde , S , Alonso , R N , Kubik , P W , Binnie , S A & Strecker , M R 2016 , ' Landscape response to late Pleistocene climate change in NW Argentina : sediment flux modulated by basin geometry and connectivity ' Journal of Geophysical Research - Earth Surface , vol. 121 , no. 2 , pp. 392-414 . https://doi.org/10.1002/2015JF003607en
dc.identifier.issn2169-9003
dc.identifier.otherPURE: 241576059
dc.identifier.otherPURE UUID: 72e291af-1081-4b1e-8dc1-3cf33f05433f
dc.identifier.otherScopus: 84959450403
dc.identifier.urihttp://onlinelibrary.wiley.com/doi/10.1002/2015JF003607/abstract#footer-support-infoen
dc.descriptionThis work was funded by the Emmy Noether Programme of the Deutsche Forschungsgemeinschaft (DFG) grant SCHI 1241/1-1 awarded to T. Schildgen, awards from the Petroleum Research Fund and the Carnegie Trust to R. Robinson, and a DFG Leibniz Award to M. Strecker (DFG 373/18-1).en
dc.description.abstractFluvial fill terraces preserve sedimentary archives of landscape responses to climate change, typically over millennial timescales. In the Humahuaca Basin of NW Argentina (Eastern Cordillera, southern Central Andes), our 29 new optically stimulated luminescence ages of late Pleistocene fill terrace sediments demonstrate that the timing of past river aggradation occurred over different intervals on the western and eastern sides of the valley, despite their similar bedrock lithology, mean slopes, and precipitation. In the west, aggradation coincided with periods of increasing precipitation, while in the east, aggradation coincided with decreasing precipitation or more variable conditions. Erosion rates and grain size dependencies in our cosmogenic 10Be analyses of modern and fill terrace sediments reveal an increased importance of landsliding compared to today on the west side during aggradation, but of similar importance during aggradation on the east side. Differences in the timing of aggradation and the 10Be data likely result from differences in valley geometry, which causes sediment to be temporarily stored in perched basins on the east side. It appears as if periods of increasing precipitation triggered landslides throughout the region, which induced aggradation in the west, but blockage of the narrow bedrock gorges downstream from the perched basins in the east. As such, basin geometry and fluvial connectivity appear to strongly influence the timing of sediment movement through the system. For larger basins that integrate subbasins with differing geometries or degrees of connectivity (like Humahuaca), sedimentary responses to climate forcing are likely attenuated.
dc.format.extent23
dc.language.isoeng
dc.relation.ispartofJournal of Geophysical Research - Earth Surfaceen
dc.rights©2016. American Geophysical Union. All Rights Reserved. This work is made available online in accordance with the publisher’s policies. This is the final published version of the work, which was originally published at https://dx.doi.org/10.1002/2015JF003607en
dc.subjectBerylium-10en
dc.subjectFluvial terracesen
dc.subjectHumahuaca Basinen
dc.subjectLandscape connectivityen
dc.subjectOptically stimulated luminescenceen
dc.subjectSouth American Monsoon Systemen
dc.subjectGE Environmental Sciencesen
dc.subjectEarth-Surface Processesen
dc.subjectGeophysicsen
dc.subjectNDASen
dc.subject.lccGEen
dc.titleLandscape response to late Pleistocene climate change in NW Argentina : sediment flux modulated by basin geometry and connectivityen
dc.typeJournal articleen
dc.description.versionPostprinten
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.Earth and Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.School of Geography and Geosciencesen
dc.contributor.institutionUniversity of St Andrews.Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews.St Andrews Sustainability Instituteen
dc.identifier.doihttps://doi.org/10.1002/2015JF003607
dc.description.statusPeer revieweden
dc.date.embargoedUntil2016-08-23


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