The La Frontera Formation ( es, Formación La Frontera, K
2F, Ksf) is a
geological formation
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics (lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock expo ...
, part of the
Villeta Group, of the
Altiplano Cundiboyacense
The Altiplano Cundiboyacense () is a high plateau located in the Eastern Cordillera of the Colombian Andes covering parts of the departments of Cundinamarca and Boyacá. The altiplano corresponds to the ancient territory of the Muisca. The Alt ...
and neighbouring areas of the
Eastern Ranges
The Eastern Ranges is an Australian rules football team in the NAB League, the Victorian statewide under-18s competition.
The club is a founding member of the competition (1992) and has produced several players for the Australian Football Le ...
of the
Colombian
Andes
The Andes, Andes Mountains or Andean Mountains (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long, wide (widest between 18°S – 20°S ...
. The sequence of
limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms wh ...
s and
lydites dates to the
Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', ...
period;
Turonian
The Turonian is, in the ICS' geologic timescale, the second age in the Late Cretaceous Epoch, or a stage in the Upper Cretaceous Series. It spans the time between 93.9 ± 0.8 Ma and 89.8 ± 1 Ma (million years ago). The Turonian is preceded ...
epoch and has a maximum thickness of .
Fossils of ''
Yaguarasaurus columbianus'' were said to be found in this formation (listed as "La Frontera Member"), although the geological mapping of the area state the time-equivalent
Hondita Formation
The Hondita Formation ( es, Formación Hondita, Ksh) is a List of fossiliferous stratigraphic units in Colombia, fossiliferous formation (geology), geological formation of the Upper Magdalena Valley (VSM) and surrounding Cordillera Central (Colomb ...
as the stratigraphic unit present in the Quebradas El Ocal and Itaibe in Huila. The La Frontera Formation does not outcrop south of Cundinamarca. A high diversity of
ammonite
Ammonoids are a group of extinct marine mollusc animals in the subclass Ammonoidea of the class Cephalopoda. These molluscs, commonly referred to as ammonites, are more closely related to living coleoids (i.e., octopuses, squid and cuttle ...
s has been found in the La Frontera Formation.
Etymology
The formation was first described by
Hubach in 1931 and elevated to formation in 1969 by Cáceres and
Etayo.
[Montoya & Reyes, 2005, p.24] The formation is named after the quarry La Frontera near
Albán, Cundinamarca.
[Acosta & Ulloa, 2001, p.41]
Description
Lithologies
The La Frontera Formation is characterised by a lower part consisting of
limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms wh ...
s and an upper part comprising
lydites.
[
]
Stratigraphy and depositional environment
The La Frontera Formation overlies the Simijaca Formation
The Simijaca Formation ( es, Formación Simijaca, K2S, Kss) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly mudstone formation dates to the Late Cretaceous period; Turonian and C ...
and is overlain by the Conejo Formation, all units belong to the Villeta Group. The age has been estimated to be Turonian
The Turonian is, in the ICS' geologic timescale, the second age in the Late Cretaceous Epoch, or a stage in the Upper Cretaceous Series. It spans the time between 93.9 ± 0.8 Ma and 89.8 ± 1 Ma (million years ago). The Turonian is preceded ...
.[ Stratigraphically, the formation is time equivalent with the Chipaque, Hondita and ]La Luna Formation
LA most frequently refers to Los Angeles, the second largest city in the United States.
La, LA, or L.A. may also refer to:
Arts and entertainment Music
* La (musical note), or A, the sixth note
* "L.A.", a song by Elliott Smith on ''Figure ...
s.[Montoya & Reyes, 2005, p.26] The formation has been deposited in an open marine platform to submarine fan setting.[García González et al., 2009, p.218] The deposition is represented by a maximum flooding surface.[Villamil, 2012, p.164] The formation contains concretion
A concretion is a hard, compact mass of matter formed by the precipitation of mineral cement within the spaces between particles, and is found in sedimentary rock or soil. Concretions are often ovoid or spherical in shape, although irregular ...
s and a high diversity of ammonite
Ammonoids are a group of extinct marine mollusc animals in the subclass Ammonoidea of the class Cephalopoda. These molluscs, commonly referred to as ammonites, are more closely related to living coleoids (i.e., octopuses, squid and cuttle ...
s;[Villamil, 2012, p.181] '' Wrightoceras munieri'', '' Vascoceras cf. constrictum'', '' Vascoceras cf. venezolanum'', '' Kamerunoceras sp.'', '' Kamerunoceras cf. turoniense'', '' Hoplitoides cf. lagiraldae'', '' Codazziceras ospinae'', '' Coilopoceras cf. newelli'',[Patarroyo, 2016, p.41] '' Hoplitoides wohltmanni'', '' Neoptychites crassus'', '' Hoplitoides ingens'', '' Mammites sp.'', '' ?Fagesia sp.'', and '' Prionocycloceras sp''.[Blanco et al., 2004, p.26] Also the bivalves '' Anomia colombiana'' and '' Inoceramus sp.'' have been found in the La Frontera Formation.[
]
''Yaguarasaurus''
Fossils of '' Yaguarasaurus columbianus'' were described as coming from the "La Frontera Member", part of the "Villeta Formation", in the Quebrada El Ocal, southwest of Neiva
Neiva () is the capital of the Department of Huila. It is located in the valley of the Magdalena River in south central Colombia with a population of about 357,392 inhabitants. It is one of the most important cities in southern Colombia, mainly ...
, Huila,[''Yaguarasaurus columbianus'']
at Fossilworks
Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database, a large relational database assembled by hundreds of paleontologists from around the world.
History
Fossilworks was cre ...
.org and in the Quebrada Itaibe southwest of Neiva,[Páramo Fonseca, 2000, p.124] although in these areas the time-equivalent Hondita Formation
The Hondita Formation ( es, Formación Hondita, Ksh) is a List of fossiliferous stratigraphic units in Colombia, fossiliferous formation (geology), geological formation of the Upper Magdalena Valley (VSM) and surrounding Cordillera Central (Colomb ...
is mapped.[Plancha 344, 1999][Plancha 345, 1999]
Outcrops
The La Frontera Formation is apart from its type locality
Type locality may refer to:
* Type locality (biology)
* Type locality (geology)
See also
* Local (disambiguation)
* Locality (disambiguation)
{{disambiguation ...
, found at surface in the north of the Bogotá savanna
The Bogotá savanna is a montane savanna, located in the southwestern part of the Altiplano Cundiboyacense in the center of Colombia. The Bogotá savanna has an extent of and an average altitude of . The savanna is situated in the Eastern Ra ...
, in the Tabio anticlinal, along the road Ubaté-Carmen de Carupa
Carmen de Carupa is a municipality and town of Colombia in the Ubaté Province, part of the department of Cundinamarca. The municipality, located in the Ubaté-Chiquinquirá Valley on the Altiplano Cundiboyacense borders San Cayetano in the w ...
,[ north and east of ]Chiquinquirá
Chiquinquirá is a town and municipality in the Colombian Department of Boyacá, part of the subregion of the Western Boyacá Province. Located some 115 km north of Bogotá, Chiquinquirá is above sea level and has a yearly average temp ...
,[Plancha 190, 2009] south of Cachipay
Cachipay is a municipality and town of Colombia in the Tequendama Province, part of the department of Cundinamarca. Cachipay borders Quipile in the west, Zipacón in the east, Anolaima in the north and La Mesa in the south. The urban centre is ...
,[Plancha 227, 1998] to a thin band east of Viotá
Viotá is a municipality and town of Colombia in the department
Department may refer to:
* Departmentalization, division of a larger organization into parts with specific responsibility
Government and military
*Department (administrative divisi ...
.[Plancha 246, 1998]
Regional correlations
See also
: Geology of the Eastern Hills
: Geology of the Ocetá Páramo
: Geology of the Altiplano Cundiboyacense
References
Bibliography
*
*
*
*
*
*
*
Maps La Frontera Fm. proper
*
*
*
*
*
*
Maps ''Yaguarasaurus'' locations
*
*
External links
*
{{DEFAULTSORT:Frontera Formation, La
Geologic formations of Colombia
Cretaceous Colombia
Upper Cretaceous Series of South America
Turonian Stage
Limestone formations
Deep marine deposits
Open marine deposits
Fossiliferous stratigraphic units of South America
Paleontology in Colombia
Formations
Geography of Cundinamarca Department
Geography of Boyacá Department