Multiple early Eocene hyperthermal events: Their lithologic expressions and environmental consequences

dc.contributor.advisorDickens, Gerald R.en_US
dc.creatorNicolo, Micah Johnen_US
dc.date.accessioned2009-07-09T15:16:35Zen_US
dc.date.available2009-07-09T15:16:35Zen_US
dc.date.issued2009en_US
dc.description.abstractA gradual rise in Earth's surface temperature marks a transition from the late Paleocene to the early Eocene ca. 58-51 Ma. Paleocene/Eocene boundary (∼55.5 Ma) sediments deposited in the midst of this slow warming ubiquitously reveal evidence for a massive isotopically light carbon injection and an associated rapid but transient global warming event, or hyperthermal, that has been termed the Paleocene Eocene Thermal Maximum (PETM) and attributed to a carbon injection from multiple potential sources. The PETM has gained importance over the past two decades as a potential geologic analog to the modern anthropogenic carbon injection and climate change. However significant questions surrounding the nature of the carbon injection at the onset of the PETM remain. The Clarence River valley, located in the Marlborough region, South Island, New Zealand, contains a series of outcrops of lithified late Paleocene to early Eocene sediments originally deposited on a paleo-slope margin. Within these sections, the Lower Limestone Member of the Amuri Limestone Formation records the interval of interest. A Lower Limestone prominent recessed unit consisting of multiple marl-rich beds and recording a pronounced negative carbon isotopic excursion (CIE) marks the PETM at sections that have been bisected by tributaries to the Clarence River, including Mead Stream and Dee Stream. Here I detail and discuss Clarence valley Lower Limestone sections and relate these records to global trends with an emphasis on adding constraints to the PETM carbon injection. Specifically, I document the lithologic and carbon isotopic expression of the PETM and two younger paired sets of early Eocene events that, similar to the Mead Stream and Dee Stream PETM sections, reveal negative CIEs and expanded marl-rich units coincident to identical CIEs and condensed carbonate dissolution horizons in deep-sea sections. I further quantify the abundance of bioturbating macrofauna trace fossils through the PETM at both Mead Stream and Dee Stream and argue that New Zealand margin intermediate waters became hypoxic precisely coincident to the PETM carbon injection. In concert, these findings suggest a PETM carbon addition mechanism capable of both diminishing intermediate water dissolved oxygen and of repeated early Eocene injections.en_US
dc.description.sponsorshipU.S. National Science Foundation (NSF); Joint Oceanographic Institutions (JOI), Inc.en_US
dc.format.extent150 p.en_US
dc.format.mimetypeapplication/pdfen_US
dc.identifier.callnoTHESIS GEOL. 2008 NICOLOen_US
dc.identifier.citationNicolo, Micah John. "Multiple early Eocene hyperthermal events: Their lithologic expressions and environmental consequences." (2009) Diss., Rice University. <a href="https://hdl.handle.net/1911/26797">https://hdl.handle.net/1911/26797</a>.en_US
dc.identifier.urihttps://hdl.handle.net/1911/26797en_US
dc.language.isoengen_US
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.en_US
dc.subjectNew Zealanden_US
dc.subjectEoceneen_US
dc.subjectBioturbationen_US
dc.subjectHyperthermal eventsen_US
dc.subjectPaleocene eocene thermal maximumen_US
dc.titleMultiple early Eocene hyperthermal events: Their lithologic expressions and environmental consequencesen_US
dc.typeThesisen_US
dc.type.materialTexten_US
thesis.degree.departmentEarth Scienceen_US
thesis.degree.disciplineNatural Sciencesen_US
thesis.degree.grantorRice Universityen_US
thesis.degree.levelDoctoralen_US
thesis.degree.nameDoctor of Philosophyen_US
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