Phylogeography of a widespread small carnivore, the western spotted skunk (Spilogale gracilis) reveals temporally variable signatures of isolation across western North America. Issue 12 (3rd May 2017)

• Record Type: Journal Article
• Authors: Ferguson, Adam W.; McDonough, Molly M.; Guerra, Gema I.; Rheude, Margaret; Dragoo, Jerry W.; Ammerman, Loren K.; Dowler, Robert C.
• Is Part Of: Ecology and evolution. Volume 7:Issue 12(2017:Jul.)
• Page Start: 4229
• Page End: 4240
• Publication Date: 2017-05-03
• Subjects: Carnivora -- desert southwest -- ecological niche modeling -- Mephitidae -- mitochondrial DNA -- pre‐Pleistocene divergence -- Quaternary climate change -- refugia; Ecology -- Periodicals; Evolution -- Periodicals; 577.05
• DOI: 10.1002/ece3.2931
• Languages: English
• ISSNs: 2045-7758

Abstract

Abstract: We analyzed phylogeographic patterns in the western spotted skunk, Spilogale gracilis Merriam, 1890 (Carnivora: Mephitidae) in relation to historical events associated with Pre‐Pleistocene Divergence (PPD) and Quaternary climate change (QCC) using mitochondrial DNA from 97 individuals distributed across Western North America. Divergence times were generated using BEAST to estimate when isolation in putative refugia occurred. Patterns and timing of demographic expansion was performed using Bayesian skyline plot. Putative climatic refugia resulting from Quaternary climate change were identified using paleoecological niche modeling and divergence dates compared to major vicariant events associated with Pre‐Pleistocene conditions. We recovered three major mitochondrial clades corresponding to western North America (California, Baja, and across the Great Basin), east‐central North America (Texas, central Mexico, New Mexico), and southwestern Arizona/northwestern Mexico. Time to most recent common ancestor for S. gracilis occurred ~1.36 Ma. Divergence times for each major clade occurred between 0.25 and 0.12 Ma, with signature of population expansion occurring 0.15 and 0.10 Ma. Ecological niche models identified three potential climatic refugia during the Last Interglacial, (1) west coast of California and Oregon, (2) northwestern Mexico, and (3) southern Texas/northeastern Mexico as well as two refugia during the Last Glacial Maximum, (1) western USA and (2) southern Texas/northeastern Mexico. This study supports PPD in shaping species‐level diversity compared to QCC‐driven changes at the intraspecific level for Spilogale, similar to the patterns reported for other small mammals (e.g., rodents and bats). Phylogeographic patterns also appear to have been shaped by both habitat and river vicariance, especially across the desert southwest. Further, continuing climate change during the Holocene coupled with anthropogenic modifications during the Anthropocene appears to be removing both of these barriers to current dispersal of western spotted skunks. Abstract : Our study provides novel insights into the biogeographic history of western North America through the application of ecological niche modeling (ENM) and phylogenetic methods to the western spotted skunk ( Spilogale gracilis ). Our results support Pre‐Pleistocene Divergence in shaping species‐level diversity compared to Quaternary Climate Change‐driven changes at the intraspecific level for Spilogale, similar to the patterns reported for other small mammals (e.g., rodents and bats). Phylogeographic patterns also appear to have been shaped by both habitat and river vicariance, especially across the desert southwest.