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Cambridge Greensand
From Wikipedia, the free encyclopedia
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The Cambridge Greensand is a geological unit in England whose strata are earliest Cenomanian in age.[1] It lies above the erosive contact between the Gault Formation and the Chalk Group in the vicinity of Cambridgeshire, and technically forms the lowest member bed of the West Melbury Marly Chalk Formation.[2] It is a remanié deposit, containing reworked fossils of late Albian age, including those of dinosaurs and pterosaurs.
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Description
The lithology is made out of glauconitic marl, described as a "chalk mud", containing abundant ostracod, coccolith and foram remains, with a concentration of phosphatic nodules and bones at the base.[1][2]
Vertebrate paleofauna
Birds
Dinosaurs
Ornithischians
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Notes Uncertain or tentative taxa are in small text; |
Saurischians
Pterosaurs
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Notes Uncertain or tentative taxa are in small text; |
Ichthyosaurs
Lepidosauria
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Notes Uncertain or tentative taxa are in small text; |
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Invertebrates
Ammonites
- Salaziceras salazacense[21]
See also
References
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