Vegetation dynamics during the Late Triassic (Carnian-Norian): Response to climate and environmental changes inferred from palynology
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- Institutt for geofag [2331]
Abstract
Microscopic plant remains (spores and pollen) allow us to trace vegetation and detect environmental, especially climatic changes from deep time in the geological past. The Late Triassic (237-201 Ma) period is marked by an array of environmental changes such as large scale volcanism, a meteorite impact and global climate change. This study describes the response of vegetation from two periods of the Late Triassic, the Carnian (237-227 Ma) and Norian (227-209 Ma), from three locations: the UK, Hungary and SW USA.List of papers
Paper 1: Baranyi, V., Miller, C.S., Ruffell, A., Hounslow, M.W. & Kürschner, W.M. A continental record of the Carnian Pluvial Episode (CPE) from the Mercia Mudstone Group: palynology and climatic implications. Submitted to the Journal of the Geological Society. The paper is not available in DUO awaiting publishing. |
Paper 2: Baranyi, V., Rostási, Á., Raucsik, B. & Kürschner, W.M. Climatic fluctuations during the Carnian Pluvial Episode (CPE) in marine successions from the Transdanubian Range (western Hungary) inferred from palynology. In preparation, to be submitted. The paper is not available in DUO awaiting publishing. |
Paper 3: Baranyi, V., Reichgelt, T., Olsen, P.E., Parker, W.G. & Kürschner, W.M. 2017. Norian vegetation history and related environmental changes: New data from the Chinle Formation, Petrified Forest National Park (Arizona, SW USA). GSA Bulletin, Published Online First. The paper is not available in DUO due to publisher restrictions. The published version is available at: https://doi.org/10.1130/B31673.1 |
Paper 4: Baranyi, V., Wellmann, C.H. & Kürschner, W.M. 2017. Ultrastructure and probable botanical affinity of the enigmatic sporomorph Froelichsporites traversei from the Norian (Late Triassic) of North America. International Journal of Plant Sciences, 179, 100–114. The paper is included in the thesis. Also available at: https://doi.org/10.1086/694762 |