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Elsevier, Quaternary Science Reviews, (103), p. 179-183

DOI: 10.1016/j.quascirev.2014.08.015

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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.”

This paper is available in a repository.
This paper is available in a repository.

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