The Redmond Formation is a geologic formation in Newfoundland and Labrador. It preserves fossils dating back to the mid-Cretaceous (Cenomanian). It was a thin (up to thick) and restricted unit traced for in a single mine (Redmond No. 1) in Labrador, overlying Paleoproterozoic rocks, with large amounts of rubble, probably as a result of graben subsidence within the Labrador Trough. Argillite facies within the formation have produced a diverse flora and insect assemblage.
Fossil content
Animals
Susumaniidae
Labradorocoleidae
Plants
- Andromeda sp.
- A. novaecaesarae
- A. parlatorii
- âÂÂAraliaâ groenlandica
- Araliopsoides cretacea
- Celastrophyllum sp.
- C. albaedomus
- C. brittonianum
- Cissites sp.
- Crassidenticulum sp.
- Daphnophyllum dakotense
- âÂÂDensinervumâ kauli
- Dicotylophyllum sp.
- Diospyros primaeva
- Dryandroides lanceolata
- Dryandroides sp.
- Ficus berthoudi
- Liriodendron simplex
- Liriodendropsis simplex
- Magnolia
- Magnolia sp.
- Magnolia amplifolia
- Menispermites sp.
- M. obtusiloba
- M. trilobatus
- Platanus sp.
- P. heerii
- P. shirleyensis
- Salix newberryana
- Sassafras acutilobum
- âÂÂSterculiaâ lugubris
See also
References
Bibliography