AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)

A succession of about 109 m thick of the La Frontera Formation lectostratotype (Colombia) is described as well as the fossils Wrightoceras munieri (Pervinquière, 1907), Vascoceras cf. constrictum (Renz and Álvarez, 1979), V. cf. venezolanum Renz, 1982, Kamerunoceras sp., K. cf. turoniense (...

Full description

Autores:

Tipo de recurso:

Fecha de publicación:: 2016

Institución:: Universidad Industrial de Santander

Repositorio:: Repositorio UIS

Idioma:: spa

id	UISANTADR2_fe72f8fb9636546961256981db9ea8cf
oai_identifier_str	oai:noesis.uis.edu.co:20.500.14071/5298
network_acronym_str	UISANTADR2
network_name_str	Repositorio UIS
repository_id_str
spelling	Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)http://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessAtribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)2016-07-012022-03-14T20:08:25Z2022-03-14T20:08:25Zhttps://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/560810.18273/revbol.v38n3-2016003https://noesis.uis.edu.co/handle/20.500.14071/5298A succession of about 109 m thick of the La Frontera Formation lectostratotype (Colombia) is described as well as the fossils Wrightoceras munieri (Pervinquière, 1907), Vascoceras cf. constrictum (Renz and Álvarez, 1979), V. cf. venezolanum Renz, 1982, Kamerunoceras sp., K. cf. turoniense (d’Orbigny, 1850), Hoplitoides cf. lagiraldae Etayo-Serna, 1979, Codazziceras ospinae (Karsten, 1858), Coilopoceras cf. newelli (Benavides-Cáceres, 1956); bivalves: Anomia colombiana Villamil, 1996, and inoceramids; and decapods and plants (woods). These fossils from La Frontera Formation indicate a lower - middle Turonian interval. It could not be confirmed the presence of uppermost Cenomanian deposits in the lower part of the La Frontera Formation.  Una sucesión de cerca de 109 m de espesor del lectoestratotipo de la Formación La Frontera (Colombia) se describe junto con el contenido fósil de Wrightoceras munieri (Pervinquière, 1907), Vascoceras cf. constrictum (Renz and Álvarez, 1979), V. cf. venezolanum Renz, 1982, Kamerunoceras sp., K. cf. turoniense (d’Orbigny, 1850), Hoplitoides cf. lagiraldae Etayo-Serna, 1979, Codazziceras ospinae (Karsten, 1858), Coilopoceras cf. newelli (Benavides-Cáceres, 1956); bivalvos: Anomia colombiana Villamil, 1996, e inocerámidos; y decápodos y plantas (troncos). Estos ejemplares incluidos dentro de la sucesión de la Formación La Frontera, en su mayoría, representan el Turoniano inferior - medio. La existencia de depósitos del Cenomaniano más alto hacia la base de la Formación La Frontera no se puede demostrar en este trabajo.application/pdftext/htmlspaUniversidad Industrial de Santanderhttps://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/5608/5786https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/5608/5934Boletín de Geología; Vol. 38 Núm. 3 (2016): Boletín de Geología; 41-54Boletín de Geología; Vol. 38 No. 3 (2016): Boletín de Geología; 41-54BOLETÍN DE GEOLOGÍA; v. 38 n. 3 (2016): Boletín de Geología; 41-542145-85530120-0283La Frontera FormationLectostratotypeAmmonitesTuronianSan Francisco-CundinamarcaColombiaFormación La FronteraLectoestratotipoAmonoideosTuronianoSan Francisco-CundinamarcaAMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)AMONOIDEOS Y OTROS MACROFÓSILES DEL LECTOESTRATOTIPO DE LA FORMACIÓN LA FRONTERA, TURONIANO INFERIOR - MEDIO (CRETÁCICO SUPERIOR) EN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)info:eu-repo/semantics/articlehttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_2df8fbb1Patarroyo, Pedro20.500.14071/5298oai:noesis.uis.edu.co:20.500.14071/52982022-03-16 12:39:35.768metadata.onlyhttps://noesis.uis.edu.coDSpace at UISnoesis@uis.edu.co
dc.title.en-US.fl_str_mv	AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)
dc.title.es-ES.fl_str_mv	AMONOIDEOS Y OTROS MACROFÓSILES DEL LECTOESTRATOTIPO DE LA FORMACIÓN LA FRONTERA, TURONIANO INFERIOR - MEDIO (CRETÁCICO SUPERIOR) EN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)
title	AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)
spellingShingle	AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA) La Frontera Formation Lectostratotype Ammonites Turonian San Francisco-Cundinamarca Colombia Formación La Frontera Lectoestratotipo Amonoideos Turoniano San Francisco-Cundinamarca
title_short	AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)
title_full	AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)
title_fullStr	AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)
title_full_unstemmed	AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)
title_sort	AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)
dc.subject.en-US.fl_str_mv	La Frontera Formation Lectostratotype Ammonites Turonian San Francisco-Cundinamarca Colombia
topic	La Frontera Formation Lectostratotype Ammonites Turonian San Francisco-Cundinamarca Colombia Formación La Frontera Lectoestratotipo Amonoideos Turoniano San Francisco-Cundinamarca
dc.subject.es-ES.fl_str_mv	Formación La Frontera Lectoestratotipo Amonoideos Turoniano San Francisco-Cundinamarca
description	A succession of about 109 m thick of the La Frontera Formation lectostratotype (Colombia) is described as well as the fossils Wrightoceras munieri (Pervinquière, 1907), Vascoceras cf. constrictum (Renz and Álvarez, 1979), V. cf. venezolanum Renz, 1982, Kamerunoceras sp., K. cf. turoniense (d’Orbigny, 1850), Hoplitoides cf. lagiraldae Etayo-Serna, 1979, Codazziceras ospinae (Karsten, 1858), Coilopoceras cf. newelli (Benavides-Cáceres, 1956); bivalves: Anomia colombiana Villamil, 1996, and inoceramids; and decapods and plants (woods). These fossils from La Frontera Formation indicate a lower - middle Turonian interval. It could not be confirmed the presence of uppermost Cenomanian deposits in the lower part of the La Frontera Formation.
publishDate	2016
dc.date.accessioned.none.fl_str_mv	2022-03-14T20:08:25Z
dc.date.available.none.fl_str_mv	2022-03-14T20:08:25Z
dc.date.none.fl_str_mv	2016-07-01
dc.type.none.fl_str_mv	info:eu-repo/semantics/article
dc.type.coarversion.fl_str_mv	http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.coar.fl_str_mv	http://purl.org/coar/resource_type/c_2df8fbb1
dc.identifier.none.fl_str_mv	https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/5608 10.18273/revbol.v38n3-2016003
dc.identifier.uri.none.fl_str_mv	https://noesis.uis.edu.co/handle/20.500.14071/5298
url	https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/5608 https://noesis.uis.edu.co/handle/20.500.14071/5298
identifier_str_mv	10.18273/revbol.v38n3-2016003
dc.language.none.fl_str_mv	spa
language	spa
dc.relation.none.fl_str_mv	https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/5608/5786 https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/5608/5934
dc.rights.license.none.fl_str_mv	Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
dc.rights.coar.none.fl_str_mv	http://purl.org/coar/access_right/c_abf2
dc.rights.accessrights.none.fl_str_mv	info:eu-repo/semantics/openAccess
dc.rights.creativecommons.none.fl_str_mv	Atribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)
rights_invalid_str_mv	Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)
eu_rights_str_mv	openAccess
dc.format.none.fl_str_mv	application/pdf text/html
dc.publisher.es-ES.fl_str_mv	Universidad Industrial de Santander
dc.source.es-ES.fl_str_mv	Boletín de Geología; Vol. 38 Núm. 3 (2016): Boletín de Geología; 41-54
dc.source.en-US.fl_str_mv	Boletín de Geología; Vol. 38 No. 3 (2016): Boletín de Geología; 41-54
dc.source.pt-BR.fl_str_mv	BOLETÍN DE GEOLOGÍA; v. 38 n. 3 (2016): Boletín de Geología; 41-54
dc.source.none.fl_str_mv	2145-8553 0120-0283
institution	Universidad Industrial de Santander
repository.name.fl_str_mv	DSpace at UIS
repository.mail.fl_str_mv	noesis@uis.edu.co
_version_	1814095218953158656

AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA)

Publicaciones similares