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Whisky Bay, Western Antarctica, Antarctica
Formation | Whisky Bay |
---|---|
Member(s) | Bibby Point Brandy Bay Gin Cove Lewis Hill Rum Cove Tumbledown Cliffs |
Age: | 89.8 - 86.3 Ma Late/Upper Cretaceous |
Interval | Late Albian |
Tectonic Setting | Back-arc basin |
Lithology | siliciclastic, siltstone, conglomerate, sandstone/conglomerate, sandstone, conglomerate/sandstone |
Number of Collections | 13 |
Number of Occurrences | 72 |
Recorded Sample Locations
Associated Units
Stratigraphic Name | Age | Lithology | Occurrence Records |
---|---|---|---|
Hidden Lake | 86.3 - 83.6 Ma Late/Upper Cretaceous | sandstone | 15 |
Kotick Point | 105 - 99.6 Ma Cretaceous | mudstone/sandstone, conglomerate, mudstone | 116 |
Lopez de Bertodano | 66.0 - 56.0 Ma Paleocene | sandstone/siltstone, siltstone, sandstone/"shale", sandstone, siltstone/sandstone, "shale"/sandstone, siltstone/"carbonate", mudstone, "siliciclastic", "shale", siltstone/mudstone | 1719 |
Santa Marta | 83.5 - 70.6 Ma Late/Upper Cretaceous | siliciclastic, sandstone, siltstone | 180 |
Santa Marta - Herbert Sound | 83.6 - 72.1 Ma Late/Upper Cretaceous | shale | 9 |
Santa Marta - Lachman Crags | 83.5 - 70.6 Ma Late/Upper Cretaceous | sandstone/siltstone, mudstone/siltstone | 166 |
Santa Marta - Rabot | 83.5 - 66.0 Ma Late/Upper Cretaceous | siltstone, sandstone/siltstone, mudstone/tuff | 214 |
Whisky Bay - Bibby Point | 113 - 101 Ma Early/Lower Cretaceous | conglomerate | 5 |
Whisky Bay - Brandy Bay | 89.8 - 86.3 Ma Late/Upper Cretaceous | sandstone, siltstone, siltstone/conglomerate | 6 |
Whisky Bay - Gin Cove | 105 - 99.6 Ma Cretaceous | conglomerate/sandstone | 11 |
Whisky Bay - Lewis Hill | 113 - 101 Ma Early/Lower Cretaceous | conglomerate | 3 |
Whisky Bay - Rum Cove | 89.8 - 86.3 Ma Late/Upper Cretaceous | conglomerate/sandstone | 1 |
Whisky Bay - Tumbledown Cliffs | 101 - 93.9 Ma Late/Upper Cretaceous | conglomerate/sandstone | 12 |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!