- E-mailmelanie.kling@uib.no
- Visitor AddressAllégaten 41Realfagbygget5007 BergenRoom2A12b - 2101
- Postal AddressPostboks 78035020 Bergen
My project aims to better understand source to sink systems and disentangle how they are affected by step-changes in forcing factors (climate and tectonics). Therefore, I will investigate sedimentary changes across the Permian-Triassic transition on Svalbard and combine/compare them with the Finnmark Platform to identify local and shared processes.
- (2021). Quantifying the diagenetic impact in the late Ediacaran and early Palaeozoic of the Avalon Peninsula using illite “crystallinity”. Canadian journal of earth sciences (Print).
- (2022). Evolution of a clastic source-to-sink system through the Permian-Triassic transition: Provenance and petrography of the Havert Formation on Finnmark Platform, Barents Sea, Norway.
- (2021). Impact of climatic step-changes on source-to-sink systems: Petrographic changes across the Permian-Triassic changes on the Finnmark Platform, Barents Sea, N Norway.
More information in national current research information system (CRIStin)
Gregor Austermann, Melanie Kling, Christina Ifrim, Pascale D. Emondt, and Anne Hildenbrand. Quantifying the diagenetic impact in the late Ediacaran and early Palaeozoic of the Avalon Peninsula using illite “crystallinity”. Canadian Journal of Earth Sciences. e-First https://doi.org/10.1139/cjes-2020-0207
Kling, M., Sirevaag, H., Pucéat, E., and Eide, C. H.: Impact of climatic step-changes on source-to-sink systems: Petrographic changes across the Permian-Triassic changes on the Finnmark Platform, Barents Sea, N Norway, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-9296, https://doi.org/10.5194/egusphere-egu21-9296, 2021.
Kling, M., Sirevaag, H., and Eide, C. H.: Evolution of a clastic source-to-sink system through the Permian-Triassic transition: Provenance and petrography of the Havert Formation on Finnmark Platform, Barents Sea, Norway, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-5009, https://doi.org/10.5194/egusphere-egu22-5009, 2022.