Detailed Characterization of Upper Cambrian Microbial Buildups (Mason County, Texas, USA)

dc.contributor.advisorDroxler, André Wen_US
dc.creatorHopson, Heath Hiltonen_US
dc.date.accessioned2019-05-17T13:34:01Zen_US
dc.date.available2019-05-17T13:34:01Zen_US
dc.date.created2017-12en_US
dc.date.issued2018-04-20en_US
dc.date.submittedDecember 2017en_US
dc.date.updated2019-05-17T13:34:01Zen_US
dc.description.abstractField studies, extensive shallow coring, thin section petrography, and hyperspectral scanning are used to characterize a series of Upper Cambrian (Wilberns Formation) subtidal microbial reefs outcropping in Mason County, central Texas. Results document details of microbial textures that were responsible for growth of the buildups, thereby providing an understanding of the environmental conditions that influenced varied stages in their evolution. Thrombolitic fabrics of dominantly microbial micrite with fossil fragments evidence carbonate precipitation induced by microbial colonies that produced a tight framework hindering diagenesis. Stromatolitic fabrics show alternating laminations of microbially precipitated calcite and amalgamated trapped grainstones exhibiting ferroan dolomite replacement and subsequent oxidation of these grains. Initial characterization of the microbial reefs identified successive growth stages, repeatedly identifiable across several separate outcrops, from which a three-phase growth model was formulated. Within the context of the three phases, the core-based geologic characterization of the buildups and coeval sediments refines the growth model into a more robust depositional model. Nucleating on lenses of flat pebbles, an initial “colonizing” Phase 1 growth results in 3-4 m high buildups defined by their distinct and early-cemented outer margins of a thick thrombolitic rind. Buildup interiors exhibit amalgamated microbial heads with poorly preserved internal structure enveloped by cm-thin thrombolitic rinds. The buildups grew in high-energy conditions, but without interacting with coeval interbuildup oolitic-bioclastic grainstones. Phase 1 terminated with onlapped terrigenous and calcareous silts (~35% CaCO3). The overlying Phase 2 growth produced buildups up to 8 m thick, characterized by a mutual interaction with interbuildup high-energy oolitic-bioclastic grainstones and packstones and generally lacking an external rind. Internally, Phase 2 growth consists of vertically aggrading and laterally expanding stromatolitic columns, each exhibiting cm-thick thrombolitic rinds directly interacting with intercolumn bioclastic grainstones. Phase 3 of growth produces a well-defined thrombolitic 2-3 m thick rind atop Phase 2, and in some instances on top of the interbuildup grainstones.en_US
dc.format.mimetypeapplication/pdfen_US
dc.identifier.citationHopson, Heath Hilton. "Detailed Characterization of Upper Cambrian Microbial Buildups (Mason County, Texas, USA)." (2018) Master’s Thesis, Rice University. <a href="https://hdl.handle.net/1911/105611">https://hdl.handle.net/1911/105611</a>.en_US
dc.identifier.urihttps://hdl.handle.net/1911/105611en_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.subjectcarbonate geologyen_US
dc.subjectsedimentologyen_US
dc.subjectpetrographyen_US
dc.subjectUpper Cambrianen_US
dc.subjectreefen_US
dc.subjectmicrobialen_US
dc.subjectmicrobial buildupen_US
dc.subjectbiohermen_US
dc.subjectTexasen_US
dc.subjecthyperspectralen_US
dc.subjectisotopeen_US
dc.subjectcoreen_US
dc.titleDetailed Characterization of Upper Cambrian Microbial Buildups (Mason County, Texas, USA)en_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.levelMastersen_US
thesis.degree.nameMaster of Scienceen_US
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