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Response to “Comment to “The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site, by David Lang et al. Quaternary Science Reviews 93: 125-141””

dc.contributor.authorLang, DC
dc.contributor.authorBailey, I
dc.contributor.authorWilson, PA
dc.contributor.authorFoster, GL
dc.contributor.authorBolton, CT
dc.contributor.authorFriedrich, O
dc.contributor.authorGutjahr, M
dc.date.accessioned2016-09-28T09:23:29Z
dc.date.issued2014-10-11
dc.description.abstractn/aen_GB
dc.identifier.citationVol. 103C, pp. 179-183en_GB
dc.identifier.doi10.1016/j.quascirev.2014.08.015
dc.identifier.urihttp://hdl.handle.net/10871/23667
dc.language.isoenen_GB
dc.publisherElsevieren_GB
dc.relation.sourceWe thank David Naafs for making available the secondary splice XRF Fe data for Site U1313 and David Hodell for access, at short notice, to his LECO carbon analyser at the Godwin Laboratory, Cambridge University to permit generation of additional CaCO3 data from the secondary splice at Site U1313 (data available on the on-line Pangaea database).en_GB
dc.relation.urlhttp://www.sciencedirect.com/science/journal/02773791/103/supp/Cen_GB
dc.rightsThis is the author accepted manuscript. The final version of the article is available from Elsevier via the DOI in this record.en_GB
dc.titleResponse to “Comment to “The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site, by David Lang et al. Quaternary Science Reviews 93: 125-141””en_GB
dc.typeArticleen_GB
dc.date.available2016-09-28T09:23:29Z
dc.identifier.issn0277-3791
dc.identifier.eissn1873-457X
dc.identifier.journalQuaternary Science Reviewsen_GB


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