Characterizing marine subsurface fungi from oligotrophic South Pacific Gyre sediments

dc.contributor.advisorReese, Brandi Kiel
dc.contributor.authorSobol, Morgan Starr
dc.contributor.committeeMemberTurner, Jeffrey W.
dc.contributor.committeeMemberGonzales, Xavier Fonz
dc.date.accessioned2018-12-19T15:55:02Z
dc.date.available2018-12-19T15:55:02Z
dc.date.issued2018-08
dc.description.abstractFungal communities from the deep marine subsurface may be important in global biogeochemical cycles through remineralization of sedimentary organic matter, but this has not yet been thoroughly observed. This study analyzes the fungal role in subsurface biogeochemical cycles and understands how these organisms have adapted to extreme environments, such as the nutrient and organic matter depleted sediments of the South Pacific Gyre. Sediment cores were collected during the Integrated Ocean Drilling Program Expedition 329 to the South Pacific Gyre on board the D/V JOIDES Resolution in the Fall of 2010. Two fungal isolates were cultured from 70 million year old sediments. Previous analysis found that the two isolates were closely related to Penicillium species. To fully characterize the isolates and test their physiological boundaries, we grew them at different temperatures, salinities and pH. Whole genomic analysis was used to understand the fungi’s physiology and metabolism on a molecular level. The fungi were found to prefer growth at mesophilic temperatures and low NaCl concentrations. Growth occurred between pH 3 and pH 8. The isolate from 12 mbsf grew optimally from pH 3 to pH 8 and the isolate from 124 mbsf grew optimally from pH 3 to pH 6. Fermentation of lactose and sucrose was confirmed, but not nitrate and sulfate reduction. The fungal isolates from the South Pacific Gyre sediment had physiological capabilities that were consistent with the in situ subsurface conditions and contained genes that were capable of utilizing the recalcitrant carbon sources found in situ. The results from this study expand on the fungal limits of life and highlight their important role global carbon cycle.en_US
dc.description.collegeCollege of Science and Engineeringen_US
dc.description.departmentLife Sciencesen_US
dc.format.extent122 pagesen_US
dc.identifier.urihttps://hdl.handle.net/1969.6/87089
dc.language.isoen_USen_US
dc.rightsThis material is made available for use in research, teaching, and private study, pursuant to U.S. Copyright law. The user assumes full responsibility for any use of the materials, including but not limited to, infringement of copyright and publication rights of reproduced materials. Any materials used should be fully credited with its source. All rights are reserved and retained regardless of current or future development or laws that may apply to fair use standards. Permission for publication of this material, in part or in full, must be secured with the author and/or publisher.en_US
dc.subjectCarbon Cycleen_US
dc.subjectEcophysiologyen_US
dc.subjectgenomicsen_US
dc.subjectMarine Deep Subsurfaceen_US
dc.subjectMycologyen_US
dc.subjectSediment Microbial Ecologyen_US
dc.titleCharacterizing marine subsurface fungi from oligotrophic South Pacific Gyre sedimentsen_US
dc.typeTexten_US
dc.type.genreThesisen_US
thesis.degree.disciplineMarine Biologyen_US
thesis.degree.grantorTexas A & M University--Corpus Christien_US
thesis.degree.levelMastersen_US
thesis.degree.nameMaster of Scienceen_US

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