New evidence for complex mosasaur paleobiology: oxygen isotopes in enamel reveal habitat variation of clidastes from the Mooreville Chalk, Alabama

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dc.contributor Tobin, Thomas
dc.contributor Lambert, W. Joe
dc.contributor Suarez, Celina A.
dc.contributor.advisor Totten Minzoni, Rebecca
dc.contributor.author Travis Taylor, Leah Marie
dc.date.accessioned 2020-01-16T15:04:40Z
dc.date.available 2020-01-16T15:04:40Z
dc.date.issued 2019
dc.identifier.other u0015_0000001_0003490
dc.identifier.other TravisTaylor_alatus_0004M_13990
dc.identifier.uri http://ir.ua.edu/handle/123456789/6547
dc.description Electronic Thesis or Dissertation
dc.description.abstract The Late Cretaceous Mississippi Embayment includes some of the most complete, well-preserved mosasaur specimens in the world. Here I investigate the paleobiology of these extinct swimming lizards through schlerochronological analysis of fossil teeth with unparalleled temporal resolution. By analyzing the oxygen isotope composition of enamel phosphate in eight consecutive, fully erupted teeth, I reconstruct the ecological niche of a Clidastes propython individual from the Mooreville Chalk in Pickens County, Alabama. The isotopic record is then compared with the previously studied Platecarpus ictericus mosasaurs from the time-equivalent Kansas Niobrara Chalk of the Western Interior Seaway. Phosphate oxygen isotope records from all eight teeth in the C. propython specimen correlate well and are spliced to build a longer record of water composition change. The spliced isotopic record is characterized by two primary features: 1.) well-correlated, semi-regular negative spikes in δ18O that have a 12 to 20 day recurrence and are up to ~4.0‰ amplitude, and 2.) a long-term decrease in δ18O from ~21.5‰ to ~20.0‰ (‰ V-SMOW), followed by a gradual increase to ~22.0‰ and a final decrease to ~20.0‰. The short-term excursions in δ18O indicate rapidly changing water habitats for the mosasaur, possibly resulting from incursion into freshwater sources with low δ18O composition. Semi-regular incursion of the C. propython individual into freshwater suggests that mosasaurs had osmoregulatory function similar to those of their living relatives, sea snakes, who must drink freshwater periodically. The long-term trend in δ18O further suggests that the C. propython individual may have migrated from open ocean water into the shallow, evaporative, 18O-enriched environments of the Mississippi Embayment. The mean δ18O value of the Alabama C. propython is ~3.7‰ higher than that of the Kansas P. ictericus. This difference is likely due to the varying isotopic composition of the open, central Western Interior Seaway vs. the evaporative, lower latitude Mississippi Embayment. An important similarity between the P. ictericus and the C. propython is that they both exibit semi-regular, negative excursions in δ18O, further implicating the freshwater incursions to be the result of a biological requirement spanning multiple, if not all, mosasaur genera.
dc.format.extent 85 p.
dc.format.medium electronic
dc.format.mimetype application/pdf
dc.language English
dc.language.iso en_US
dc.publisher University of Alabama Libraries
dc.relation.ispartof The University of Alabama Electronic Theses and Dissertations
dc.relation.ispartof The University of Alabama Libraries Digital Collections
dc.relation.hasversion born digital
dc.rights All rights reserved by the author unless otherwise indicated.
dc.subject.other Paleontology
dc.subject.other Paleoecology
dc.subject.other Geochemistry
dc.title New evidence for complex mosasaur paleobiology: oxygen isotopes in enamel reveal habitat variation of clidastes from the Mooreville Chalk, Alabama
dc.type thesis
dc.type text
etdms.degree.department University of Alabama. Department of Geological Sciencess
etdms.degree.discipline Geology
etdms.degree.grantor The University of Alabama
etdms.degree.level master's
etdms.degree.name M.S.


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