Landscape and Biotic Evolution of the Kochkor Basin, Kyrgyzstan

dc.contributor.advisorHopkins, Samantha
dc.contributor.authorMcLaughlin, Win
dc.date.accessioned2018-09-06T22:01:52Z
dc.date.available2018-09-06T22:01:52Z
dc.date.issued2018-09-06
dc.description.abstractKyrgyzstan is the single most seismically active country in the world. Accessing the past, and therefore future hazard of faults, necessitates a high-resolution understanding of the timing of different geologic events. With no radiometrically datable rocks from the Neogene of Kyrgyzstan, I herein present the first work formally describing Neogene vertebrate faunas from the Kochkor Basin of Kyrgyzstan. I utilize a combination of biostratigraphy and magnetostratigraphy to constrain the timing of when the vertebrate assemblages were emplaced, and have dated the three bone beds to all fall in the latest Miocene, spanning 9-5 million years ago. All four bone beds represent mass death assemblages, inferred to be from drought-caused mortality. The timing of the deposits corresponds to uplift in the Pamirs, Himalayan, and greater Tibetan Plateau, which would have blocked the Indian monsoon from reaching Central Asia, forever altering the climate and biota of the region. This change is reflected in the shifting mammals faunas, as evidenced by the novel rhinocerotid I describe in a phylogeographic context.en_US
dc.identifier.urihttps://hdl.handle.net/1794/23810
dc.language.isoen_US
dc.publisherUniversity of Oregon
dc.rightsCreative Commons BY-NC-ND 4.0-US
dc.subjectBiogeographyen_US
dc.subjectGeochronologyen_US
dc.subjectKyrgyzstanen_US
dc.subjectMammaliaen_US
dc.subjectPaleontologyen_US
dc.subjectRhinocerotidaeen_US
dc.titleLandscape and Biotic Evolution of the Kochkor Basin, Kyrgyzstan
dc.typeElectronic Thesis or Dissertation
thesis.degree.disciplineDepartment of Geological Sciences
thesis.degree.grantorUniversity of Oregon
thesis.degree.leveldoctoral
thesis.degree.namePh.D.

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