An Earliest Carboniferous Actinopterygian Fauna from the Horton Bluff Formation of Nova Scotia

dc.contributor.advisorAnderson, Jason S.
dc.contributor.authorWilson, Conrad Daniel Mackenzie
dc.contributor.committeememberTheodor, Jessica M.
dc.contributor.committeememberCote, Susanne
dc.contributor.committeememberJamniczky, Heather A.
dc.contributor.committeememberAnderson, Jason S.
dc.date2020-02
dc.date.accessioned2020-01-15T18:43:14Z
dc.date.available2020-01-15T18:43:14Z
dc.date.issued2020-01
dc.description.abstractThis thesis examines four earliest Carboniferous (Tournaisian) actinopterygian specimens from the Horton Bluff Formation of Nova Scotia. I used traditional and μCT descriptive techniques in order to better understand actinopterygian evolution and the transition between Devonian and Carboniferous vertebrate faunas. NSM 017.GF.017.001 was investigated using microscopy and latex peel techniques and represents the oldest occurrence of a deep-bodied actinopterygian. NSM 017.GF.017.007 and NSM 017.GF.017.004 were investigated using microscopy and μCT. Neither specimen can be assigned to genus or species, however, each can be compared to a broader group. NSM 017.GF.017.007 is most similar to Devonian taxa, whereas NSM 017.GF.017.004 is most similar to actinopterygians deeply nested in a broad post-Devonian radiation. NSM 017.GF.017.005 was examined using μCT and was incorporated into a phylogenetic analysis. In this specimen, the plesiomorphic anatomy of the dermal shoulder girdle, pectoral fin, and opercular-gular series are contrasted with the derived anatomy of the hyoid arch. In the phylogenetic analysis, it is recovered as a late-diverging member of a grade of otherwise Devonian actinopterygians. The presence of NSM 017.GF.017.001 and NSM 017.GF.017.004 suggests that derived actinopterygians faunas were established by the Tournaisian; whereas the presence of NSM 017.GF.017.007 and NSM 017.GF.017.005 suggests that Hangenberg extinction survivorship was inclusive of early-diverging actinopterygians. NSM 017.GF.017.001 and NSM 017.GF.017.005 also evince actinopterygian body plan exploration, perhaps related to resource acquisition, in the Tournaisian and revise previous models of post-Hangenberg actinopterygian differentiation. More broadly, the disparity of this fauna weakens interpretations of a homogeneous earliest Tournaisian caused by mass extinction and suggest that faunal turnover was more gradual than expected, at least in Actinopterygii.en_US
dc.identifier.citationWilson, C. D. M. (2020). An Earliest Carboniferous Actinopterygian Fauna from the Horton Bluff Formation of Nova Scotia (Master's thesis, University of Calgary, Calgary, Canada). Retrieved from https://prism.ucalgary.ca.en_US
dc.identifier.doihttp://dx.doi.org/10.11575/PRISM/37453
dc.identifier.urihttp://hdl.handle.net/1880/111496
dc.language.isoengen_US
dc.publisher.facultyScienceen_US
dc.publisher.institutionUniversity of Calgaryen
dc.rightsUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.en_US
dc.subjectActinopterygiien_US
dc.subjectactinopterygianen_US
dc.subjectray-finned fishen_US
dc.subjectCarboniferousen_US
dc.subjectDevonianen_US
dc.subjectHangenbergen_US
dc.subjectmass extinctionen_US
dc.subjectBlue Beach, Nova Scotiaen_US
dc.subject.classificationZoologyen_US
dc.subject.classificationPaleoecologyen_US
dc.subject.classificationPaleontologyen_US
dc.subject.classificationPaleozoologyen_US
dc.titleAn Earliest Carboniferous Actinopterygian Fauna from the Horton Bluff Formation of Nova Scotiaen_US
dc.typemaster thesisen_US
thesis.degree.disciplineBiological Sciencesen_US
thesis.degree.grantorUniversity of Calgaryen_US
thesis.degree.nameMaster of Science (MSc)en_US
ucalgary.item.requestcopytrueen_US
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