The impact of the end-Devonian mass extinction (the Hangenberg extinction) on tetrapods is not well understood. One issue is that we have very little knowledge of the Devonian tetrapod fauna that immediately preceded, and experienced, the mass extinction. New specimens from an early tetrapod bone bed of the latest Famennian, Stensiö Bjerg Formation of Celsius Bjerg, East Greenland have the potential to shed light on this problem. In this study, five new well-preserved specimens are presented: a partial skull, two humeri, a left pelvis, and a strange vertebral element. The specimens were imaged using propagation phase-contrast synchrotron microtomography (PPC-SRμCT), and then virtually segmented and rendered. The partial skull and left pelvis share many similarities with Ichthyostega and Acanthostega, but also have some distinctive features. Notably, the epipterygoid does not articulate with the skull roof, the fenestra vestibuli appears to have an anterior lobe, the postorbital has a posteroventral process, and there is a sharp contrast between the rugose dermal ornament of the skull roof and the unornamented cheek. In addition, the partial skull is box-like in shape and has a laterally facing orbit, which are features seen in some Carboniferous tetrapods. Among other characters, the left pelvis has a differently curving posterior iliac process, and differently shaped ischium and anterior pubic margin compared to Ichthyostega and Acanthostega. The acetabulum of the left pelvis is also lacking a posterior notch, a feature seen in many other early tetrapods. The humeri presented in this thesis are curiously similar to the isolated tetrapod humerus from the Catskill Formation, Pennsylvania, USA known as ANSP 21350. In fact, they are more similar to each other and to ANSP 21350 than to any other early tetrapod humeri. This is in large part due to a distinctly distal supinator ridge which was previously only known from ANSP 21350. The mysterious vertebral element does not resemble any known early tetrapod bone due to its large, ventral, concave saddle-shaped projections. It consists of five fused vertebrae and is interpreted here to be a unique sacrum of an early tetrapod. The specimens described and interpreted in this study represent at least two new species, none of which can be assigned to known Devonian early tetrapods from Greenland. It is clear that a new and important faunal assemblage is emerging.
| Identifer | oai:union.ndltd.org:UPSALLA1/oai:DiVA.org:uu-531070 |
| Date | January 2024 |
| Creators | Sheng, Rebecca Ruo |
| Publisher | Uppsala universitet, Institutionen för geovetenskaper |
| Source Sets | DiVA Archive at Upsalla University |
| Language | English |
| Detected Language | English |
| Type | Student thesis, info:eu-repo/semantics/bachelorThesis, text |
| Format | application/pdf |
| Rights | info:eu-repo/semantics/openAccess |
| Relation | Examensarbete vid Institutionen för geovetenskaper, 1650-6553 ; 625 |
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