The Mao Formation is a geologic formation in the northwestern Dominican Republic. The reefal limestone and siltstone formation preserves bivalve, gastropod, echinoid and coral fossils dating back to the Pliocene period.[1]
Mao Formation | |
---|---|
Stratigraphic range: Pliocene | |
Type | Formation |
Lithology | |
Primary | Limestone |
Other | Siltstone |
Location | |
Coordinates | 19°30′N 71°12′W / 19.5°N 71.2°W |
Approximate paleocoordinates | 19°30′N 70°48′W / 19.5°N 70.8°W |
Country | Dominican Republic |
Fossil content
editSee also
editReferences
edit- ^ Mao Formation at Fossilworks.org
- ^ a b c Budd et al., 2019
- ^ Schwarzhans & Aguilera, 2013
Bibliography
edit- Ann F. Budd; James D. Woodell; Danwei Huang; James S. Klaus (2019). "Evolution of the Caribbean subfamily Mussinae (Anthozoa: Scleractinia: Faviidae): transitions between solitary and colonial forms". Journal of Systematic Palaeontology. 17 (18): 1581–1616. Bibcode:2019JSPal..17.1581B. doi:10.1080/14772019.2018.1541932. S2CID 92225764.
- Werner Schwarzhans; Orangel Aguilera (2013). "Otoliths of the Myctophidae from the Neogene of tropical America". Palaeo Ichthyologica. 13: 83–150.
Further reading
edit- A. F. Budd and K. G. Johnson. 1999. Neogene Paleontology in the northern Dominican Republic 19: The family Faviidae (Anthozoa, Scleractinia) part II: The genera Caulastraea, Favia, Diploria, Thysanus, Hadrophyllia, Manicina and Colpophyllia. Bulletins of American Paleontology 356:1-83
- A. W. Janssen. 1999. Neogene Paleontology in the Northern Dominican Republic 20. Holoplanktonic Mollusks (Gastropoda: Heteropoda and Thecosomata). Bulletins of American Paleontology (358)1-40
- A. Logan. 1987. Neogene paleontology in the northern Dominican Republic 6. The phylum Brachiopoda. Bulletins of American Paleontology 93(328):44-55
- J. B. Saunders, P. Jung, and B. Biju-Duval. 1986. Neogene Paleontology in the Northern Dominican Republic: 1. Field Surveys, Lithology, Environment, and Age. Bulletins of American Paleontology 89(323):1-79