From Wikipedia, the free encyclopedia
Bahía Inglesa Formation
Stratigraphic range: MiocenePleistocene
Bahía Inglesa Formation exposures at Chorrillos beach, far from Bahia Inglesa
Type Geological formation
Underlies Estratos de Caldera (Caldera Beds)
Overlies Angostura Formation
Lithology
Primary Conglomerate, coquina, sand, sandstone, siltstone, shale
Other Clay, limestone
Location
Region Atacama Region
Country  Chile
Extent Caldera Basin
Type section
Named for Bahía Inglesa

The Bahía Inglesa Formation (alternatively misspelled "Bahia") is a littoral, sedimentary, and highly fossiliferous geological formation that outcrops across the nearby coastal zones of Caldera, Chile. The unit is part of the greater Caldera Basin and was deposited in deep-shallow water, littoral paleoenvironments. It holds an exquisite fossil record in several localities (such as Cerro Ballena), mostly composed of marine mammals, as well as invertebrate taxa. [1] [2] [3] [4]

Gallery

Panoramic view of Salto del Gato locality with sediments of the Bahía Inglesa Formation

See also

References

  1. ^ Pyenson, N. D.; Gutsein, C. S.; Parham, J. F.; Le Roux, J. P.; Chavarria, C. C.; Little, H.; Metallo, A.; Rossi, V.; Valenzuela-Toro, A. M.; Velez-Juarbe, J.; Santelli, C. M.; Rogers, D. R.; Cozzuol, M. A; Suárez, M. E. (2014). "Repeated mass strandings of Miocene marine mammals from Atacama Region of Chile point to sudden death at sea". Proceedings of the Royal Society B: Biological Sciences. 281 (1781). doi: 10.1098/rspb.2013.3316. PMC  3953850. PMID  24573855. Supplemental Material
  2. ^ Le Roux, J. P.; Achurra, L.; Henríquez, Á.; Carreño, C.; Rivera, H.; Suárez, M. E.; Ishman, S. E.; Pyenson, N. D.; Gutstein, C. S. (2016). "Oroclinal bending of the Juan Fernández Ridge suggested by geohistory analysis of the Bahía Inglesa Formation, north-central Chile" (PDF). Sedimentary Geology. 333: 32–49. Bibcode: 2016SedG..333...32L. doi: 10.1016/j.sedgeo.2015.12.003.
  3. ^ Oyanadel-Urbina, P.; De Gracia, C.; Carrillo-Briceño, J. D.; Nielsen, S. N.; Flores, H.; Casteletto, V.; Kriwet, J.; Rivadeneira, M. M.; Villafaña, J. A. (2021). "Neogene Bony Fishes from the Bahía Inglesa Formation, Northern Chile" (PDF). Ameghiniana. 58 (4): 345−368. doi: 10.5710/amgh.26.05.2021.3375. S2CID  236644447.
  4. ^ Püschel, H. P.; Alarcón-Muñoz, J.; Soto-Acuña, S.; Ugalde, R.; Shelley, S. L.; Brusatte, S. L. (2023). "Anatomy and phylogeny of a new small macraucheniid (Mammalia: Litopterna) from the Bahía Inglesa Formation (late Miocene), Atacama Region, Northern Chile". Journal of Mammalian Evolution. 30 (2): 415–460. doi: 10.1007/s10914-022-09646-0.

External links

From Wikipedia, the free encyclopedia
Bahía Inglesa Formation
Stratigraphic range: MiocenePleistocene
Bahía Inglesa Formation exposures at Chorrillos beach, far from Bahia Inglesa
Type Geological formation
Underlies Estratos de Caldera (Caldera Beds)
Overlies Angostura Formation
Lithology
Primary Conglomerate, coquina, sand, sandstone, siltstone, shale
Other Clay, limestone
Location
Region Atacama Region
Country  Chile
Extent Caldera Basin
Type section
Named for Bahía Inglesa

The Bahía Inglesa Formation (alternatively misspelled "Bahia") is a littoral, sedimentary, and highly fossiliferous geological formation that outcrops across the nearby coastal zones of Caldera, Chile. The unit is part of the greater Caldera Basin and was deposited in deep-shallow water, littoral paleoenvironments. It holds an exquisite fossil record in several localities (such as Cerro Ballena), mostly composed of marine mammals, as well as invertebrate taxa. [1] [2] [3] [4]

Gallery

Panoramic view of Salto del Gato locality with sediments of the Bahía Inglesa Formation

See also

References

  1. ^ Pyenson, N. D.; Gutsein, C. S.; Parham, J. F.; Le Roux, J. P.; Chavarria, C. C.; Little, H.; Metallo, A.; Rossi, V.; Valenzuela-Toro, A. M.; Velez-Juarbe, J.; Santelli, C. M.; Rogers, D. R.; Cozzuol, M. A; Suárez, M. E. (2014). "Repeated mass strandings of Miocene marine mammals from Atacama Region of Chile point to sudden death at sea". Proceedings of the Royal Society B: Biological Sciences. 281 (1781). doi: 10.1098/rspb.2013.3316. PMC  3953850. PMID  24573855. Supplemental Material
  2. ^ Le Roux, J. P.; Achurra, L.; Henríquez, Á.; Carreño, C.; Rivera, H.; Suárez, M. E.; Ishman, S. E.; Pyenson, N. D.; Gutstein, C. S. (2016). "Oroclinal bending of the Juan Fernández Ridge suggested by geohistory analysis of the Bahía Inglesa Formation, north-central Chile" (PDF). Sedimentary Geology. 333: 32–49. Bibcode: 2016SedG..333...32L. doi: 10.1016/j.sedgeo.2015.12.003.
  3. ^ Oyanadel-Urbina, P.; De Gracia, C.; Carrillo-Briceño, J. D.; Nielsen, S. N.; Flores, H.; Casteletto, V.; Kriwet, J.; Rivadeneira, M. M.; Villafaña, J. A. (2021). "Neogene Bony Fishes from the Bahía Inglesa Formation, Northern Chile" (PDF). Ameghiniana. 58 (4): 345−368. doi: 10.5710/amgh.26.05.2021.3375. S2CID  236644447.
  4. ^ Püschel, H. P.; Alarcón-Muñoz, J.; Soto-Acuña, S.; Ugalde, R.; Shelley, S. L.; Brusatte, S. L. (2023). "Anatomy and phylogeny of a new small macraucheniid (Mammalia: Litopterna) from the Bahía Inglesa Formation (late Miocene), Atacama Region, Northern Chile". Journal of Mammalian Evolution. 30 (2): 415–460. doi: 10.1007/s10914-022-09646-0.

External links


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