Results 41 to 50 of about 3,089 (207)

Rediscovering Globigerina bollii Cita and Premoli Silva 1960 [PDF]

open access: yesJournal of Micropalaeontology
Globigerina bollii Cita and Premoli Silva was described from the historical Langhian-type section in Langhe, Piedmont (Italy). Due to its peculiar compact morphology, it was set apart from all the other globigerinids typical of the coeval Mediterranean ...
A. Fabbrini   +5 more
doaj   +1 more source

The antiquity of the Rhine River : stratigraphic coverage of the Dinotheriensande (Eppelsheim Formation) of the Mainz Basin (Germany) [PDF]

open access: yes, 2012
Background: Mammalian fossils from the Eppelsheim Formation (Dinotheriensande) have been a benchmark for Neogene vertebrate palaeontology since 200 years.
Aiglstorfer, Manuela   +3 more
core   +4 more sources

THE STRATIGRAPHIC RECORD OF NEOGENE EVENTS IN THE TIRANA DEPRESSION

open access: yesRivista Italiana di Paleontologia e Stratigrafia, 1997
The Tirana Depression is located in the eastern and inner part of the Periadriatic Depression.It forms an elongated NW-SE oriented structural element,60 km in length, located between the front of west -verging Dinaric structures and the east-verging ...
ROMANO GELATI   +3 more
doaj   +1 more source

The phylogenetic and palaeogeographic evolution of the miogypsinid larger benthic foraminifera [PDF]

open access: yes, 2012
Access to new material from South Africa, Corsica, Cyprus, Syria and Sumatra has allowed a systematic biostratigraphic comparison and correlation of the miogypsinids from the Mediterranean–West Africa and the Indo-Pacific provinces, and for the first ...
Boudagher-Fadel, MK, Price, GD
core   +1 more source

Geology of the Mt. Cosce sector (Narni Ridge, Central Apennines, Italy) [PDF]

open access: yes, 2016
This paper is companion to a 1:15,000 scale geological map of the southern sector of the Narni Range in Central Italy. This sector of the Apenninic Chain was affected by the western Tethyan rifting stage during the Early Jurassic, and the inherited ...
Cipriani, Angelo
core   +1 more source

24 million years of pollination interaction between European linden flowers and bumble bees. [PDF]

open access: yesNew Phytol
Summary Pollination is the most common insect–plant mutualism, binding them in a co‐evolutionary framework. Historic evidence of this interaction can be partly inferred from time‐calibrated molecular phylogenies of plant and insect lineages or directly from fossils.
Geier C   +9 more
europepmc   +2 more sources

Paleogene evolution of the External Betic Zone and geodynamic implications [PDF]

open access: yes, 2014
Interdisciplinary studies combining field data (geological and tectonic mapping, lithostratigraphic reconstructions, lithofacies characterization, correlations and sampling) and laboratory analyses (biostratigraphy, chronostratigraphy, clay mineralogy ...
Guerrera, Francesco   +5 more
core   +4 more sources

Stratigraphy of Cretaceous to Lower Pliocene sediments in the northern part of Cyprus based on comparative 87Sr/86Sr isotopic, nannofossil and planktonic foraminiferal dating [PDF]

open access: yes, 2012
New age data from Sr isotope analysis and both planktonic foraminifera and nannofossils are presented and discussed here for the Upper Eocene–Upper Miocene sedimentary rocks of the Değirmenlik (Kythrea) Group.
Ellam, Robert M.   +5 more
core   +2 more sources

The middle miocene (Badenian) holoplanktonic mollusks (Euthecosomata - Pteropoda) from Serbia, central paratethys [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva
The present paper deals with holoplanktonic gastropods (Pteropoda) from the Middle Miocene (Badenian) deposits of Serbia. The material for the present study comes from three localities at the southern margin of the Pannonian Basin (Central Paratethys ...
Jovanović Gordana   +4 more
doaj   +1 more source

The implications of K-Ar glauconite dating of the Diest Formation on the paleogeography of the Upper Miocene in Belgium [PDF]

open access: yes, 2014
The glauconite-rich Diest Formation in central and north Belgium contains sands in the Campine subsurface and the hilly Hageland area that can be distinguished from each other.
Adriaens, Rieko   +13 more
core  

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