Bahía Inglesa Formation

{{Short description|Geologic formation in Chile}}

{{Infobox rockunit

| name = Bahía Inglesa Formation

| image = Chorrillos, Atacama.jpg

| caption = Bahía Inglesa Formation exposures at Chorrillos beach, far from Bahia Inglesa

| type = Geological formation

| period = Neogene

| age = MiocenePleistocene

| prilithology = Conglomerate, coquina, sand, sandstone, siltstone, shale

| otherlithology = Clay, limestone

| namedfor = Bahía Inglesa

| namedby =

| region = Atacama Region

| country = Chile

| coordinates =

| paleocoordinates =

| unitof =

| subunits =

| underlies = Estratos de Caldera (Caldera Beds)

| overlies = Angostura Formation

| thickness =

| extent = Caldera Basin

| area =

}}

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 or Los Dedos), mostly composed of marine mammals, as well as invertebrate taxa.{{cite journal|last1=Pyenson|first1=N. D.|last2=Gutsein|first2=C. S.|last3=Parham|first3=J. F.|last4=Le Roux|first4=J. P.|last5=Chavarria|first5=C. C.|last6=Little|first6=H.|last7=Metallo|first7=A.|last8=Rossi|first8=V.|last9=Valenzuela-Toro|first9=A. M.|last10=Velez-Juarbe|first10=J.|last11=Santelli|first11=C. M.|last12=Rogers|first12=D. R.|last13=Cozzuol|first13=M. A|last14=Suárez|first14=M. E.|date=2014|title=Repeated mass strandings of Miocene marine mammals from Atacama Region of Chile point to sudden death at sea|journal=Proceedings of the Royal Society B: Biological Sciences|volume=281|issue=1781|doi=10.1098/rspb.2013.3316|doi-access=free|pmc=3953850|pmid=24573855}} [https://royalsocietypublishing.org/action/downloadSupplement?doi=10.1098%2Frspb.2013.3316&file=rspb20133316supp1.pdf Supplemental Material]{{cite journal|last1=Le Roux|first1=J. P.|last2=Achurra|first2=L.|last3=Henríquez|first3=Á.|last4=Carreño|first4=C.|last5=Rivera|first5=H.|last6=Suárez|first6=M. E.|last7=Ishman|first7=S. E.|last8=Pyenson|first8=N. D.|last9=Gutstein|first9=C. S.|date=2016|title=Oroclinal bending of the Juan Fernández Ridge suggested by geohistory analysis of the Bahía Inglesa Formation, north-central Chile|journal=Sedimentary Geology|volume=333|pages=32–49|doi= 10.1016/j.sedgeo.2015.12.003|bibcode=2016SedG..333...32L |url=https://repositorio.uchile.cl/bitstream/handle/2250/139375/Oroclinal-bending-of-the-Juan-Fernandez-Ridge.pdf?sequence=1&isAllowed=y}}{{cite journal|last1=Oyanadel-Urbina|first1=P.|last2=De Gracia|first2=C.|last3=Carrillo-Briceño|first3=J. D.|last4=Nielsen|first4=S. N.|last5=Flores|first5=H.|last6=Casteletto|first6=V.|last7=Kriwet|first7=J.|last8=Rivadeneira|first8=M. M.|last9=Villafaña|first9=J. A.|date=2021|title=Neogene Bony Fishes from the Bahía Inglesa Formation, Northern Chile|journal=Ameghiniana|volume=58|issue=4|pages=345−368|doi=10.5710/amgh.26.05.2021.3375|s2cid=236644447 |url=https://www.zora.uzh.ch/id/eprint/206654/1/AMGH.26.05.2021.3375-1.pdf}}{{cite journal|last1=Püschel|first1=H. P.|last2=Alarcón-Muñoz|first2=J.|last3=Soto-Acuña|first3=S.|last4=Ugalde|first4=R.|last5=Shelley|first5=S. L.|last6=Brusatte|first6=S. L.|date=2023|title=Anatomy and phylogeny of a new small macraucheniid (Mammalia: Litopterna) from the Bahía Inglesa Formation (late Miocene), Atacama Region, Northern Chile|journal=Journal of Mammalian Evolution|volume=30 |issue=2 |pages=415–460 |doi=10.1007/s10914-022-09646-0|doi-access=free}}

Gallery

{{wide image|Panoramica Salto del gato.jpg|1500px|align-cap=center|Panoramic view of Salto del Gato locality with sediments of the Bahía Inglesa Formation}}

File:BHI ENE 09 111.jpg

File:Desierto junto al mar, Atacama.jpg

File:Parque Los Dedos (1).png

File:Farellones 2 Salto del gato.jpg

File:Erosión en salto del gato.jpg

See also

{{Portal|Chile|Paleontology|Geology}}

References

{{reflist}}