Miocene/Pliocene shift: one step or several?
Thure E. Cerling,
John M. Harris,
Bruce J. MacFadden,
Jay Quade,
Meave G. Leakey,
Vera Eisenmann and
James R. Ehleringer
Additional contact information
Thure E. Cerling: University of Utah
John M. Harris: Page Museum
Bruce J. MacFadden: Florida Museum of Natural History
Jay Quade: University of Arizona
Meave G. Leakey: National Museums of Kenya
Vera Eisenmann: Museé National dHistoire Naturelle
James R. Ehleringer: University of Utah
Nature, 1998, vol. 393, issue 6681, 127-127
Abstract:
Abstract Cerling et al. reply — Köhler et al. suggest that phenomena other than floral change may be involved in the late Miocene global vegetation change, such as monsoonal dynamics or unnamed “other factors”. Citing evidence from Spain and Pakistan, they do not believe that there is necessarily a synchronicity or a causal link between faunal and vegetation change in the late Miocene epoch. However, on the contrary, it seems highly unlikely that a vegetation change on the scale documented1 would be uncorrelated with faunal change.
Date: 1998
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DOI: 10.1038/30127
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