Results 1 to 10 of about 460 (165)

Specific features of carbon and oxygen stable isotopes (δ13C and δ18O) geochemistry in the isolated carbonate platform section on the east of the Urals (the Famennian and Tournaisian Stages)

Литосфера, 2016
New data about the stable carbon and oxygen isotopic composition for the Frasnian/Famennian and Devonian/Carboniferous boundary intervals, as well as for middle and upper parts of the Tournasian Stage (the Lower Carboniferous), are represented in this ...
G. A. Mizens, V. N. Kuleshov, S. A. Sapurin, T. I. Stepanova, O. L. Petrov   +4 more
doaj   +2 more sources

Survivorship dynamics of the flora of Devonian Angarida. [PDF]

Proc Biol Sci, 2023
Dowding EM, Akulov NI, Mashchuk IM.
europepmc   +1 more source

Paleoenvironments of Late Devonian tetrapods in China. [PDF]

Sci Rep, 2023
Guo X, Retallack GJ, Liu J.
europepmc   +1 more source

Geological structure and formation conditions of the Lodmin-Bayandy isolated carbonate platform [PDF]

Нефтегазовая геология: Теория и практика
The article presents the results of an analysis of the geological structure and development history of the Lodmin-Bayandy carbonate platform in the Timan-Pechora petroleum province.
Kolesnikov E.V., Martynov A.V., Zharkov A.M., Kalinin D.F.   +3 more
doaj  

Spore Evidence for the Origin of Isoetalean Lycopsids? [PDF]

Life (Basel), 2023
Bek J, Frojdová JV.
europepmc   +1 more source

A Late Devonian tree lycopsid with large strobili and isotomous roots. [PDF]

Commun Biol, 2022
Liu L, Wang DM, Zhou Y, Qin M, Ferguson DK, Meng MC.   +5 more
europepmc   +1 more source

Broad snouted cladoselachian with sensory specialization at the base of modern chondrichthyans. [PDF]

Swiss J Palaeontol, 2023
Klug C, Coates M, Frey L, Greif M, Jobbins M, Pohle A, Lagnaoui A, Haouz WB, Ginter M.   +8 more
europepmc   +1 more source

First ovules integument: what roles? [PDF]

Natl Sci Rev, 2022
Meyer-Berthaud B.
europepmc   +1 more source

Late Famennian correlation by miospores between the Refrath 1 borehole (Bergisch Gladbach-Paffrath Syncline, Germany) and the reference section of Chanxhe (Dinant Syncline, Belgium)

Carnets de Géologie, 2005
The Bergisch Gladbach-Paffrath Syncline and the Dinant Syncline are both part of the Ardennes-Rhenish Massif but are separated by some 100 km. In the Upper Devonian succession of the Bergisch Gladbach-Paffrath Syncline (The Bergisches Land), the ...
Hartkopf-Fröder Christoph, Streel Maurice   +1 more
doaj  

How Stiff Was Armorica During the Variscan Orogeny? A Reappraisal of the “Bretonian” Phase in Central Brittany

Geosciences
In collision belts, the upper plate is generally less deformed than the lower one that underwent syn-metamorphic ductile shearing, and frequently late-collisional crustal melting.
Michel Faure, Eric Marcoux, Marc Poujol, Clément Masson   +3 more
doaj   +1 more source