PhotosLocation


dos+bocas+formation Latitude and Longitude:

1°48′S 80°48′W / 1.8°S 80.8°W / -1.8; -80.8
From Wikipedia, the free encyclopedia
Dos Bocas Formation
Stratigraphic range: Chattian
( Deseadan)
~26–24  Ma
O
S
D
C
P
T
J
K
N
Montañita-Olón locality with outcrops of the Dos Bocas Formation
Type Geological formation
Unit of Subibaja Group
Underlies Villingota Formation
Overlies Zapotal Formation
Lithology
Primary Sandstone
Location
Coordinates 1°48′S 80°48′W / 1.8°S 80.8°W / -1.8; -80.8
Approximate paleocoordinates 3°36′S 75°30′W / 3.6°S 75.5°W / -3.6; -75.5
Region Santa Elena Province
Country  Ecuador
Extent Progreso Basin

The Dos Bocas Formation is a sedimentary geological formation of the Progreso Basin in southwestern Ecuador. It is dated to the Chattian, about 26 to 24 Ma, ( Deseadan in the SALMA classification).

Description

Stratigraphy of the Montañita-Olón locality

The formation comprises moderately-sorted, fine to medium sandstones with angular quartz- feldspathic clasts. Conspicuous rounded green grains are probably glauconite, but berthierine cannot be dismissed. The matrix is micritic and volcanogenic, possibly bentonitic. The formation was deposited in an estuarine to mid shelf environment. Fossils of sharks, turtles and the tropical dolphin Urkudelphis were recovered from the formation. [1] [2]

Fossil content

The formation has provided fossils of:

See also

References

  1. ^ Tanaka, Y.; Abella, J.; Aguirre-Fernández, G.; Gregori, M.; Fordyce, E. R. (2017). "A new tropical Oligocene dolphin from Montañita/Olón, Santa Elena, Ecuador". PLOS ONE. 12 (12): e0188380. Bibcode: 2017PLoSO..1288380T. doi: 10.1371/journal.pone.0188380. PMC  5737981. PMID  29261688.
  2. ^ Carrillo-Briceño, J. D.; Villafaña, J. A.; De Gracia, C.; Flores-Alcívar, F. F.; Kindlimann, R.; Abella, J. (2020). "Diversity and paleoenvironmental implications of an elasmobranch assemblage from the Oligocene–Miocene boundary of Ecuador". PeerJ. 8: e9051. doi: 10.7717/peerj.9051. PMC  7195833. PMID  32391203.

dos+bocas+formation Latitude and Longitude:

1°48′S 80°48′W / 1.8°S 80.8°W / -1.8; -80.8
From Wikipedia, the free encyclopedia
Dos Bocas Formation
Stratigraphic range: Chattian
( Deseadan)
~26–24  Ma
O
S
D
C
P
T
J
K
N
Montañita-Olón locality with outcrops of the Dos Bocas Formation
Type Geological formation
Unit of Subibaja Group
Underlies Villingota Formation
Overlies Zapotal Formation
Lithology
Primary Sandstone
Location
Coordinates 1°48′S 80°48′W / 1.8°S 80.8°W / -1.8; -80.8
Approximate paleocoordinates 3°36′S 75°30′W / 3.6°S 75.5°W / -3.6; -75.5
Region Santa Elena Province
Country  Ecuador
Extent Progreso Basin

The Dos Bocas Formation is a sedimentary geological formation of the Progreso Basin in southwestern Ecuador. It is dated to the Chattian, about 26 to 24 Ma, ( Deseadan in the SALMA classification).

Description

Stratigraphy of the Montañita-Olón locality

The formation comprises moderately-sorted, fine to medium sandstones with angular quartz- feldspathic clasts. Conspicuous rounded green grains are probably glauconite, but berthierine cannot be dismissed. The matrix is micritic and volcanogenic, possibly bentonitic. The formation was deposited in an estuarine to mid shelf environment. Fossils of sharks, turtles and the tropical dolphin Urkudelphis were recovered from the formation. [1] [2]

Fossil content

The formation has provided fossils of:

See also

References

  1. ^ Tanaka, Y.; Abella, J.; Aguirre-Fernández, G.; Gregori, M.; Fordyce, E. R. (2017). "A new tropical Oligocene dolphin from Montañita/Olón, Santa Elena, Ecuador". PLOS ONE. 12 (12): e0188380. Bibcode: 2017PLoSO..1288380T. doi: 10.1371/journal.pone.0188380. PMC  5737981. PMID  29261688.
  2. ^ Carrillo-Briceño, J. D.; Villafaña, J. A.; De Gracia, C.; Flores-Alcívar, F. F.; Kindlimann, R.; Abella, J. (2020). "Diversity and paleoenvironmental implications of an elasmobranch assemblage from the Oligocene–Miocene boundary of Ecuador". PeerJ. 8: e9051. doi: 10.7717/peerj.9051. PMC  7195833. PMID  32391203.

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