Abstract Ultrahigh‐pressure (UHP) rocks in North‐East Greenland lie within a larger region of high‐pressure Laurentian crust formed in the overthickened upper plate of the collision with Baltica. Coesite‐bearing zircon dates UHP metamorphism to 365–350 Ma, which formed at the end of the Caledonian collision as a result of intracontinental subduction ...
Jane A. Gilotti +3 more
wiley +1 more source
GIVETIAN–FRASNIAN BOUNDARY CONODONTS FROM KERMAN PROVINCE, CENTRAL IRAN
The Middle - Late Devonian boundary is investigated based on twenty-two conodont species and subspecies from three sections in the north and west of Kerman, southeastern central Iran.
HOSSEIN GHOLAMALIAN +4 more
doaj +1 more source
Miospores in givetian to lower frasnian sediments dated by conodonts from the Boulonnais, France [PDF]
Abstract The Calcaire de Blacourt and the lower part of the Schistes de Beaulieu exposed in the new railroad trench Caffiers-Ferques and in the Griset Quarry (Boulonnais, France) contain well-preserved miospore assemblages which have been previously described from continental beds in Scotland, Spitsbergen and the Canadian Arctic Islands.
Loboziak, S, Streel, Maurice
openaire +1 more source
The main features of the Givetian-Frasnian shoal deposits of the Sub-Polar Urals (Matyashor formation) are considered. The study part of the section corresponds to varcus - rhenana zones on the basis of conodonts.
D. A. Gruzdev +3 more
doaj +2 more sources
Investigating a Devonian vertebrate assemblage with synchrotron microtomography of coprolites
Fossilised faeces (coprolites) are a unique source of information as they record palaeontological evidence of animal behaviour (autecology) as well as interactions between extinct organisms and their environment (synecology).
Arnaud Rebillard +3 more
doaj +1 more source
Occurrence of subnormal size phenotype in the latest Eifelian/earliest Givetian boundary, Tibagi city, Paraná State, Brazil: taphonomic and paleosynecologic implications [PDF]
Subnormal size phenotype of marine invertebrates is recorded at the interval Neo-Eifelian/eo-Givetian (Devonian). These fossils represent a relictual fauna that resulted from a biotic crisis.
Andressa Carla Penteado +4 more
doaj
Towards a palaeogeographical and sequential framework for the Givetian of Belgium
This paper starts with a review of facies and reef morphologies from the Givet Group in the Ardenne area. Platform initiation and evolution are analyzed and related to external factors at a global scale (sea level changes, climate changes), at a regional scale (local subsidence, change in detrital supply) and to internal factors like organic ...
Boulvain, Frédéric +3 more
openaire +1 more source
NEW DATA ON MIDDLE DEVONIAN CONODONTS FROM SW-SARDINIA:THE SU NUARGI II SECTION REVISITED
The conodont collection from the nodular limestone beds of the Su Nuargi II outcrop near Domusnovas in SW-Sardinia (Italy) is restudied for the purpose of reassessing the outcrop and updating the conodont collection to the most recent taxonomy. Su Nuargi
SOFIE GOUWY
doaj +1 more source
Spore Evidence for the Origin of Isoetalean Lycopsids? [PDF]
Bek J, Frojdová JV.
europepmc +1 more source
A New Genus of Lungfish from the Givetian (Middle Devonian) of Central Australia
A new Dipterus-like lungfish, Harajicadipterus youngi, is described from the Givetian (Middle Devonian) Harajica Sandstone Member of central Australia. The material is comprised of five specimens representing the skull roof, orbital bones, tooth plates, operculo-gular bones, a partial pectoral girdle, centra and scales.
openaire +3 more sources

