Search results for "BIOSTRATIGRAPHY"

Les ammonites du Sinémuriensupérieur du Jebel-Bou-Hamid (Haut-Atlas central, Rich, Maroc). Approches paléontologique et biostratigraphique

1998

Resume L'etude des faunes d'ammonites - plus de 25 taxons - et de leur succession biostratigraphique dans unecoupe exceptionnellement complete et fossilifere du Haut-Atlas central de la region de Rich (Maroc) a permis la mise en evidence de 10 unites biochronologiques elementaires (=assemblages) pour une periode debutant au sein de la partie terminale du Sinemurien inferieur et s'achevant avec le Sinemurien superieur. Pour les zones a Oxynotum et Raricostatum, il s'agit des premieres donnees biostratigraphiques collectees avec une telle precision dans le Nord de l'Afrique. Pour le Sinemurien inferieur et la zone a Obtusum, les nombreuses donnees nouvellement acquises, completent, precisent …

Les ammonites du sinémurien supérieuret du carixien inférieur a moyen du gisement de lefterochori (Albanie méridionale). Témoin exceptionnel des faun…

2000

Resume L'exploitation du gisement de Lefterochori situe pres de Delvina a l'Est de Saranda (Zone ionienne, Albanie meridionale) a permis l'etude d'une riche faune d'ammonites datant du Sinemurien terminal et du Carixien inferieur a moyen. Une cinquantaine de taxons ont ete reconnus et trois especes nouvelles decrites (Lytoceras platypleura, Tropidoceras sulcatum et Protogrammoceras ionicum). Il s'agit en fait d'un materiel exceptionnel, tant en quantite qu'en qualite, car a l'exception de rares specimens isoles, les peuplements helleniques (Albanie et Grece) etaient jusqu'ici inconnus pour la periode consideree. Ces faunes presentent un maximum d'affinites avec celles de l'Apennin central e…

Les ammonites traditionnellement regroupées dans la sous-famille des Bouleiceratinae (Hildoceratidae, Toarcien) : aspects phylogénétiques, biogéograp…

2003

Resume Les genres d’ammonites, traditionnellement regroupes dans la sous-famille des Bouleiceratinae, appartiennent en fait a des lignees differentes de la famille des Hildoceratidae. Une approche utilisant des arguments paleogeographiques, stratigraphiques et morphologiques d’une part et une approche cladistique d’autre part ont permis de distinguer 3 groupes se succedant au cours du temps et a repartitions paleogeographiques differentes : • les Bouleiceratinae s.s. (genres Bouleiceras, Nejdia et Kohaticeras) du Toarcien inferieur ; • les Leukadiellinae (genres Leukadiella et Renziceras) du Toarcien moyen ; • et les Paroniceratinae (genres Frechiella, Paroniceras et Oxyparoniceras) du Toar…

Paleoceanographic and paleoenvironmental changes in the Red Sea during the Messinian/Zanclean: new data from Site 225.

2013

Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)

2017

[EN]: The Cuesta del Rey mammal sites located on the NE border of the Duero Basin are of great importance with regard to understand the general biostratigraphy of the basin, because Miocene mammal sites are extremely scarce in this area in comparison with the central part of the basin. The mammals identified in Cuesta del Rey-1 are: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. And Democricetodon sp. The Cuesta del Rey-1 rodent assemblage is characteristic of the end of the upper Aragonian (MN 7/8, end of the middle Miocene), equivalent to the local subzone G3 of …

ASTROCHRONOLOGY OF LATE MIDDLE MIOCENE MEDITERRANEAN SECTIONS

2004

Calcareous Nannofossil and Planktonic Foraminifera Biostratigraphy of selected Piacenzian-Gelasian Laminites from Southern Italy

2011

Here we present the biostratigraphic and chronostratigraphic framework of a number of selected diatomaceous laminated intervals from the Crotone Basin (Calabria, Southern Italy). These layers, which we consider correlative to the Eastern Mediterranean Sapropel Layers, range in age from the early Piacenzian to the Gelasian, and show surprising thicknesses, suggesting that they were probably laid down in a landlocked, overfed basin. Specifically, a thick laminite from the surroundings of Cropani (Catanzaro) can be ascribed to nannofossil biozone MNN 16a and planktonic foraminifera biozone MPL 4b (lower Piacenzian) according to the Mediterranean calcareous plankton biostratigraphic zonations. …

Astronomic forcing on the planktonic foraminifera assemblage in the Piacenzian Punta Piccola section (southern Italy)

2006

[1] A high-resolution quantitative analysis of the calcareous planktonic assemblages (planktonic foraminifers and calcareous nannofossils) at the Punta Piccola section (at the base of which, the global standard stratotype-section and point of the Piacenzian stage is defined) provided a more accurate biostratigraphy for the Mediterranean middle Pliocene (2.6–3.6 Ma). In particular, an astronomically calibrated age of 2.87 Ma was estimated for the Pliocene first occurrence of Neogloboquadrina atlantica instead of the younger previously proposed age of 2.72 Ma. Spectral analysis performed on the Globigerinoides species (spp.) planktonic foraminifera assemblage along with cross-spectral analysi…

Mediterranean Neogene planktonic foraminifer biozonation and biochronology

2019

Abstract Planktonic foraminifera are widely used for biostratigraphy and correlation of Mediterranean Neogene marine sediments, and are a fundamental component in the astronomical tuning of the Neogene Time Scale. Recent developments in high-resolution studies, focused on the astronomical calibration of cyclically marine sediments cropping out in land-based sections and recovered from deep-sea successions, increased the accuracy of stratigraphic ranges of planktonic foraminiferal species improving the biostratigraphic resolution and biochronology. The large amount of data on planktonic foraminifera obtained through quantitative/semiquantitative analyses, published in the recent years, allow…

Systematic and biostratigraphy of the genera Parasolenopleura, Badulesia, and Pardailhania in the Iberian Chains: a useful zonation for the Miaolingi…

2020

The trilobite species of three genera included in the Family Solenopleuridae: Parasolenopleura , Badulesia , and Pardailhania are revised. These genera have a great biostratigraphic interest due to their broad distribution in the Miaolingian Series (former middle Cambrian) of the Mediterranean Subprovince and because they constitute an evolutionary lineage, that facilitates an accurate regional correlation. Two of these genera ( Pardailhania and Badulesia ) have been used to define middle Cambrian zones in Spain (lower and middle Caesaraugustan, equivalent to the uppermost Wuliuan and the lower Drumian stages). Although, all authors have been using the same species to establish the Mediterr…