5   Artículos

 
en línea
Agata Di Stefano, Natale Maria D?Andrea, Salvatore Distefano, Salvatore Urso, Laura Borzì, Niccolò Baldassini and Viviana Barbagallo    
The quantitative analysis of the calcareous nannofossil content yield in the 600 m thick succession drilled at ODP Site 1123 (offshore New Zealand), considered as a reference section for the Southern Ocean region, allowed the recognition of 43 bioevents ... ver más
Revista: Journal of Marine Science and Engineering    Formato: Electrónico

 
en línea
George Kontakiotis, Assimina Antonarakou, Evangelia Besiou, Elisavet Skampa and Maria V. Triantaphyllou    
The late Quaternary is a key stratigraphic interval as it encompasses the Late Glacial to Holocene transition, which is characterized by a series of pronounced centennial climate oscillations and subsequent short-term events of paleoceanographic variabil... ver más
Revista: Journal of Marine Science and Engineering    Formato: Electrónico

 
en línea
Felix Gradstein, Anna Waskowska and Larisa Glinskikh    
We provide a biochronology of Jurassic planktonic foramininfera, using first order linkage to ammonite and nannofossil stratigraphy and geochronology. This enigmatic and understudied group of microfossils occurred from middle Toarcian through Tithonian t... ver más
Revista: Geosciences    Formato: Electrónico

 
en línea
Ignacio Arenillas, Vicente Gilabert and José A. Arz    
After the Cretaceous/Paleogene boundary (KPB) catastrophic mass extinction event, an explosive evolutionary radiation of planktic foraminifera took place in consequence of the prompt occupation of empty niches. The rapid evolution of new species makes it... ver más
Revista: Geosciences    Formato: Electrónico

 
en línea
Antonella Cinzia Marra    
The Quaternary mammals of Sicily are well known, and five faunal complexes have been distinguished on the basis of bioevents (extinctions and new arrivals) and evolution of endemic species. It is clear that the composition of mammal faunas is strictly re... ver más
Revista: Geosciences    Formato: Electrónico

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