Search results for "PALEOBIOGEOGRAFIA"

showing 3 items of 3 documents

Multistratigraphic records of the Lower Cretaceous (Valanginian–Cenomanian) Puez key area in N. Italy

2016

Abstract We present a stratigraphic investigation of a Hauterivian to Cenomanian hemipelagic succession from Col Puez, in the Dolomites (Southern Alps, northern Italy). A composite section of seven segments was studied with bio-, magneto-, and chemostratigraphy, which enabled detailed and robust age calibration of the Puez succession. It also revealed the paleoceanographic history and helped identify the important global climatic events of that period. The age of the Lower Cretaceous Puez Formation in the Dolomites is refined as late Hauterivian to early Cenomanian. Ammonoids provide a detailed biostratigraphic subdivision that forms the basis for analyses of the faunal distribution and the…

010506 paleontologygeographyPlateaugeography.geographical_feature_categoryAptianPaleontology010502 geochemistry & geophysicsOceanography01 natural sciencesCretaceousPaleontologyChemostratigraphyFaciesPaleoclimatologyPeriod (geology)PALEOBIOGEOGRAFIACenomanianEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Sistematica, tafonomia e paleobiogeografia delle associazioni ad ammoniti del Giurassico Medio e Superiore della Sicilia Occidentale con particolare …

2012

AmmonitiSettore GEO/02 - Geologia Stratigrafica E SedimentologicaPaleobiogeografiaGiurassicoSiciliaSettore GEO/01 - Paleontologia E Paleoecologia
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Callovian to lower Kimmeridgian ammonite successions from West Sicily (Roccapalumba) and Northeast Iberian Range (Ariño, Teruel): A key for palaeogeo…

2010

La comparacion de las sucesiones de ammonites en el intervalo comprendido entre el Calloviense y el Kimmeridgiense inferior en la region de Sicilia occidental (Roccapalumba-Sciacca) y la Cordillera Iberica nororiental (Sierra de Arcos) muestra una clara similitud y paralelismo en el desarrollo estratigrafico. Esto incluye el registro incompleto del Calloviense inferior, una amplia laguna estratigrafica (Calloviense inferior-Oxfordiense medio) y un registro mas completo del Oxfordiense medio-superior (biozonas Transversarium-Bifurcatus) y Kimmeridgiense inferior. Esto permite inferir una evolucion paleogeografica paralela en ambas regiones del Tethys. Las asociaciones registradas de ammonite…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaAmmonoidea Jurásico Medio Jurásico Superior PaleobiogeografiaBioestratigrafia.Settore GEO/01 - Paleontologia E Paleoecologia
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