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Response to "Comment on '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."

dc.contributor.authorLang, David C.
dc.contributor.authorBailey, Ian
dc.contributor.authorWilson, Paul A.
dc.contributor.authorFoster, Gavin L.
dc.contributor.authorBolton, Clara 
dc.contributor.authorFriedrich, Oliver
dc.contributor.authorGutjahr, Marcus
dc.date.accessioned2015-03-20T12:41:49Z
dc.date.available2015-03-20T12:41:49Z
dc.date.issued2014
dc.identifier.citationQuaternary Science Reviews, 103, p. 179-183 (2014); doi:10.1016/j.quascirev.2014.08.015
dc.identifier.issn0277-3791
dc.identifier.urihttp://hdl.handle.net/10651/30460
dc.format.extentp. 179-183
dc.language.isoeng
dc.relation.ispartofQuaternary Science Reviews
dc.rights©,
dc.sourceWOS:000344211000014
dc.titleResponse to "Comment on '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."
dc.typejournal article
dc.identifier.doi10.1016/j.quascirev.2014.08.015
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.quascirev.2014.08.015


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