Multigene phylogeny of the Mustelidae: Resolving relationships, tempo and biogeographic history of a mammalian adaptive radiation-4

Emperature curve (smoothed mean in red) based on global deep-sea oxygen isotope (δO) records (modified from [60]). The development of full-scale ice-sheets in each hemisphere as well as key changes in vegetation in the northern hemisphere during the Neogene are also shown. Following the Mid-Miocene...

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Bibliographic Details
Main Authors: Klaus-Peter Koepfli, Deere, Kerry A, Slater, Graham J, Begg, Colleen, Begg, Keith, Grassman, Lon, Lucherini, Mauro, Veron, Geraldine, Wayne, Robert K
Format: Still Image
Language:unknown
Published: figshare 2011
Subjects:
Genetics
FOS Biological sciences
taiga
Online Access:https://dx.doi.org/10.6084/m9.figshare.76257.v1
https://figshare.com/articles/figure/Multigene_phylogeny_of_the_Mustelidae:_Resolving_relationships,_tempo_and_biogeographic_history_of_a_mammalian_adaptive_radiation-4/76257/1
Description
Summary:Emperature curve (smoothed mean in red) based on global deep-sea oxygen isotope (δO) records (modified from [60]). The development of full-scale ice-sheets in each hemisphere as well as key changes in vegetation in the northern hemisphere during the Neogene are also shown. Following the Mid-Miocene climatic optimum, forested habitats (A) gave way to more open vegetation habitats such as woodlands and grasslands (B). Taiga forests greatly expand during the Pliocene (C). See the text for further details. PLE. denotes Pleistocene. Copyright information: Taken from "Multigene phylogeny of the Mustelidae: Resolving relationships, tempo and biogeographic history of a mammalian adaptive radiation"http://www.biomedcentral.com/1741-7007/6/10BMC Biology 2008;6():10-10.Published online 14 Feb 2008PMCID:PMC2276185.

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