The Location and Styles of Ice-Free “Oases” during Neoproterozoic Glaciations with Evolutionary Implications

• Published in: Geosciences
• Main Author: Daniel Paul Le Heron
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2012
• Subjects: Neoproterozoic; Snowball Earth; glaciation; evolution; Geology; QE1-996.5; East Antarctica; Antarc*; Antarctica; Siberia
• Online Access: https://doi.org/10.3390/geosciences2020090; https://doaj.org/article/3d8fa0a28ea5458c9a73447545a86d88

Evidence based on molecular clocks, together with molecular evidence/biomarkers and putative body fossils, points to major evolutionary events prior to and during the intense Cryogenian and Ediacaran glaciations. The glaciations themselves were of global extent. Sedimentological evidence, including hummocky cross-stratification (representing ice-free seas affected by intra-glacial storms), dropstone textures, microbial mat-bearing ironstones, ladderback ripples, and wave ripples, militates against a “hard” Snowball Earth event. Each piece of sedimentological evidence potentially allows insight into the shape and location, with respect to the shoreline, of ice-free areas (“oases”) that may be viewed as potential refugia. The location of such oases must be seen in the context of global paleogeography, and it is emphasized that continental reconstructions at 600 Ma (about 35 millions years after the “Marinoan” ice age) are non-unique solutions. Specifically, whether continents such as greater India, Australia/East Antarctica, Kalahari, South and North China, and Siberia, were welded to a southern supercontinent or not, has implications for island speciation, faunal exchange, and the development of endemism.