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dc.contributor.advisor Heermance, Richard V en
dc.contributor.author Riegel, Hannah en
dc.date.accessioned 2016-01-20T17:22:44Z en
dc.date.available 2016-01-20T17:22:44Z en
dc.date.copyright 2015 en
dc.date.issued 1/20/2016 en
dc.date.submitted 2015-12 en
dc.identifier.uri http://hdl.handle.net/10211.3/159873 en
dc.description Includes bibliographical references (pages 29-33) en
dc.description California State University, Northridge. Department of Geological Sciences. en
dc.description.abstract The Pliocene is a time of rapid, extreme climate variability, but geologic exposures of lacustrine strata from this time are rare, impeding observations of the impact of climate change on lake sedimentation. The Qaidam Basin (QB) in western China provides a unique geologic setting, where internally drained lakes have existed for the past few million years, and recent deformation of the basin floor has uplifted and exposed lacustrine strata. The stratigraphy presented in this thesis records a detailed history of lake level fluctuation, evaporite deposition, and climate change from one location in the QB. Samples for paleomagnetism and carbon/oxygen isotope dating were collected from the Huatugou region of the QB to document the environmental conditions present during deposition, and determine how subtle changes in evaporite concentrations changed as global climate changed in the Miocene-Pliocene. Although a 655 m section was described and measured, samples were only collected in the lower 475 m Samples were analyzed for their paleomagnetic properties and to determine the rate of sedimentation in this area. 12 magnetozones indicate an age for the lower half of the section between 6.033-033 Ma. The section consists of 9 lithofacies (1 mudstone, 4 sandstone, 1 conglomerate, 2 gypsum, 1 halite) that can be divided into 3 stratigraphic units based on evaporite concentration. Alternating mud, gypsum, and halite beds imply multiple lake-level fluctuations and occasional drying of the lake. There are two major transgression/regression, 1) ~6.033- 5.2 Ma and 2) ~5.2- 4.4 Ma, along with a gradual regression from 4.4 Ma- present. Lake transgression/regression cycles have an average recurrence rate of 100, 000 +/- 20,000 yrs, matching well with orbital eccentricity. Sedimentation rates were derived from correlating the paleomagnetostratigraphic column to the Astronomically Tuned Neogene Time Scale (ATNTS). The oldest sedimentation rate from ~6.033 Ma is 93.4 m/My. The middle, from ~5.235 Ma is 218.2 m/My. The youngest, ranging from ~4.187 Ma is 118.4 m/My. This is the rate assumed for the upper part of the section. Compared to other studies done in the Qaidam Basin, the Huatugou region began to dry out before the rest of the basin (at least 6 Ma), which is also seen by the southeastward migration of lake depocenters. Overall, the section shows shallowing of the lake throughout the Pliocene, and may correlate with uplift of nearby mountains and cooling climate. en
dc.description.statementofresponsibility by Hannah Riegel en
dc.format application/pdf en
dc.format.extent vii, 110 pages en
dc.language.iso en en
dc.publisher California State University, Northridge en
dc.rights.uri http://scholarworks.csun.edu/xmlui/handle/10211.2/286 en
dc.subject Stratigraphy en
dc.subject Magnetostratigraphy en
dc.subject Qaidam Basin en
dc.subject Lake Fluctuation en
dc.subject Climate Change en
dc.subject Geology en
dc.subject.other Dissertations, Academic -- CSUN -- Geology. en
dc.title Environmental Impacts Of Rapid Climate Change At The Pliocene-Quaternary Transition In The Qaidam Basin, China en
dc.type Thesis en
dc.date.updated 2016-01-20T17:22:44Z en
dc.contributor.department Geological Sciences en
dc.description.degree M.S. en
dc.contributor.committeemember Pedone, Vicki en
dc.contributor.committeemember Bogue, Scott en
dc.rights.license By signing and submitting this license, you the author grant permission to CSUN Graduate Studies to submit your thesis or dissertation, and any additional associated files you provide, to CSUN ScholarWorks, the institutional repository of the California State University, Northridge, on your behalf. You grant to CSUN ScholarWorks the non-exclusive right to reproduce and/or distribute your submission worldwide in electronic or any medium for non-commercial, academic purposes. You agree that CSUN ScholarWorks may, without changing the content, translate the submission to any medium or format, as well as keep more than one copy, for the purposes of security, backup and preservation. You represent that the submission is your original work, and that you have the right to grant the rights contained in this license. You also represent that your submission does not, to the best of your knowledge, infringe upon anyone's copyright. If the submission contains material for which you do not hold copyright, or for which the intended use is not permitted, or which does not reasonably fall under the guidelines of fair use, you represent that you have obtained the unrestricted permission of the copyright owner to grant CSUN ScholarWorks the rights required by this license, and that such third-party owned material is clearly identified and acknowledged within the text or content of the submission. If the submission is based upon work that has been sponsored or supported by an agency or organization other than the California State University, Northridge, you represent that you have fulfilled any right of review or other obligations required by such contract or agreement. CSUN ScholarWorks will clearly identify your name(s) as the author(s) or owner(s) of the submission, and will not make any alterations, other than those allowed by this license, to your submission. en


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