Results 21 to 30 of about 9,786 (214)

The Albian-Cenomanian boudary in the northern part of the Don-Medveditsa dislocations. Paper 2. Oryctocoenoses analysis. Conclusions [PDF]

open access: yesИзвестия Саратовского университета. Новая серия: Серия Науки о Земле
Ammonite finds at the Miroshniki site, within the Albian-Cenomanian boundary interval, make it possible to identify the presence of the analogues of the Upper Albian zones Mortoniceras fallax (autochthonous burial within aleurolites) and Mortoniceras ...
Pervushov, Evgeniy Mikhaylovich   +3 more
doaj   +1 more source

The albian-cenomanian boudary in the northern part of the Don-Medveditsa dislocations. Paper 1. The history of studying and the section descriptions [PDF]

open access: yesИзвестия Саратовского университета. Новая серия: Серия Науки о Земле
The Albian-Cenomanian rocks compose a single complex of terrigenous deposits over the Volga Region. Delineation of the boundaries of the Cretaceous system units generally tends to cause difficulties, accounted for by rare finds of the fossils.
Pervushov, Evgeniy Mikhaylovich   +3 more
doaj   +1 more source

Biostratigraphy of the Mauddud Formation from selected Boreholes, central Iraq

open access: yesIraqi Geological Journal, 2023
The Mauddud Formation was one of the important and widespread Lower Cretaceous period formations in Iraq. It has been studied in three wells (EB. 55, EB. 58, and EB. 59) within the East Baghdad Oil Field, Baghdad, central Iraq. 280 thin sections
Luay Shakir, Anwar Mousa
doaj   +1 more source

Oyster-bioimmured ammonites from the Upper Albian of Annopol, Poland: stratigraphic and palaeobiogeographic implications [PDF]

open access: yes, 2013
Ammonites Mortoniceras (Subschloenbachia) sp. are preserved as attachment scars on the oyster shells from the topmost portion of the Albian succession at Annopol, Poland. These oyster-bioimmured ammonites show a closest affinity to the representatives of
Machalski, M., Kennedy, W. J.
core   +1 more source

A first high-resolution carbon isotope stratigraphy from the Boreal (NW Germany) for the Berriasian to Coniacian interval—implications for the timing of the Aptian–Albian boundary

open access: yesFrontiers in Earth Science, 2023
High-amplitude changes in sedimentary δ13C characterize the Cretaceous system and have been proven useful for supra-regional chemostratigraphic correlation.
André Bornemann   +5 more
doaj   +1 more source

A basal elasmosaurid plesiosaur from the upper Albian– lower Cenomanian? Cambridge Greensand

open access: yesActa Palaeontologica Polonica
An historical indeterminate elasmosaurid specimen CAMSM X50356 (CAMSM = Sedgwick Museum) collected during the 19th century is described. The specimen comes from the Cenomanian Cambridge Greensand although the possibility of an Albian–lower Cenomanian age
Jose P. O’Gorman, Roger B.J. Benson
doaj   +1 more source

Late Albian Col de Palluel (SE France, Niveau Breistroffer): results from palynomorphs

open access: yes, 2005
Late Albian Col de Palluel (SE France, Niveau Breistroffer): results from ...
Jörg Mutterlose (558960)   +11 more
core   +1 more source

Late Albian Col de Palluel (SE France, Niveau Breistroffer): results from planktic foraminifera

open access: yes, 2005
Late Albian Col de Palluel (SE France, Niveau Breistroffer): results from planktic ...
Jörg Mutterlose (558960)   +11 more
core   +1 more source

Mesozoic biostratigraphic, paleoenvironmental, and paleobiogeographic synthesis, equatorial Atlantic [PDF]

open access: yes, 1998
Cretaceous sediments from Ocean Drilling Program Leg 159 on the Côte d’Ivoire-Ghana Marginal Ridge (CIGMR), eastern equatorial Atlantic, are characterized by distinct stratigraphic changes in sedimentary facies associated with changes in the composition ...
Shin, I.C.   +55 more
core   +1 more source

Late Albian Col de Palluel (SE France, Niveau Breistroffer): Samples, lithology and geochemical results

open access: yes, 2005
Late Albian Col de Palluel (SE France, Niveau Breistroffer): Samples, lithology and geochemical ...
Jörg Mutterlose (558960)   +11 more
core   +1 more source

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