Results 101 to 110 of about 544 (156)

The Dire Straits of Paratethys

, 2018
Prehistoric Eurasia contained the largest mega-lake on Earth, formed after the isolation of a fragmented region of dying seas known as Paratethys. In this realm, tectonics, sea-level fluctuations, and climate change led to ecological crises: brine seas, extinctions, great drying events and mega-floods.
openaire   +2 more sources

East Asian climate evolution during the Cenozoic: A review from the modeling perspective. [PDF]

Fundam Res
Zhang R, Jiang D, Li X, Shi J, Shen T.
europepmc   +1 more source

Evolutionary history of Old World cellar spiders in the context of Neo-Tethyan sea-land transformations. [PDF]

Zool Res
Yao ZY, Li SQ.
europepmc   +1 more source

The porcupine <i>Hystrix parvae</i> (Kretzoi, 1951) from the Late Miocene (Turolian, MN11) of Kohfidisch in Austria. [PDF]

Paleobiodivers Paleoenviron
Daxner-Höck G, Winkler V, Kalthoff DC.
europepmc   +1 more source

The river Dniester valley: a long record of late-Cenozoic fluvial evolution within the Eastern Carpathian foreland and East European Platform margin. [PDF]

R Soc Open Sci
Matoshko AV, Gibbard P.
europepmc   +1 more source

From Peri-Tethys to Paratethys

, 2017
From the Alps in western Europe to the great steppes of Kazakhstan, the former Paratethys Sea once covered a vast area of our planet, of which the Black Sea, Caspian Sea and Aral lake are today’s remnants. The Paratethys formed as the Tethys ocean gradually closed, and was known as ‘Peri-Tethys’ until the late Eocene.
openaire   +2 more sources

Late Miocene transformation of Mediterranean Sea biodiversity [PDF]

Sci Adv
Agiadi K, Hohmann N, Gliozzi E, Thivaiou D, Bosellini FR, Taviani M, Bianucci G, Collareta A, Londeix L, Faranda C, Bulian F, Koskeridou E, Lozar F, Mancini AM, Dominici S, Moissette P, Campos IB, Borghi E, Iliopoulos G, Antonarakou A, Kontakiotis G, Besiou E, Zarkogiannis SD, Harzhauser M, Sierro FJ, Coll M, Vasiliev I, Camerlenghi A, García-Castellanos D.   +28 more
europepmc   +2 more sources

Phylogenomic resolution of lampreys reveals the recent evolution of an ancient vertebrate lineage. [PDF]

Proc Biol Sci
Hughes LC, Bloom DD, Piller KR, Lang N, Mayden RL.   +4 more
europepmc   +1 more source

Sharks, rays and skates (Chondrichthyes, Elasmobranchii) from the Upper Marine Molasse (middle Burdigalian, early Miocene) of the Simssee area (Bavaria, Germany), with comments on palaeogeographic and ecological patterns. [PDF]

Palaontol Z, 2020
Villafaña JA, Marramà G, Klug S, Pollerspöck J, Balsberger M, Rivadeneira M, Kriwet J.   +6 more
europepmc   +1 more source

Changes in continental weathering regimes inhibited global marine deoxygenation during the Paleocene-Eocene thermal maximum. [PDF]

Nat Commun
Wei GY, Pohl A, Jiang S, Zhang H, Wang W, A E Pogge von Strandmann P, Maffre P, Xiong G, Shen SZ, Zhang F.   +9 more
europepmc   +1 more source