Results 1 to 10 of about 2,766 (223)

Mummified Wood of Juniperus (Cupressaceae) from the Late Miocene of Taman Peninsula, South Russia [PDF]

open access: yesPlants, 2022
Juniperus L. is the second-largest genus of conifers, having the widest distribution of all conifer genera. Its phytogeographic history is, however, obscure due to its very poor fossil record. We described a wood of Juniperus sp.
Anna V. Stepanova   +4 more
doaj   +2 more sources

The Upper Miocene of the Rostov Dome (Eastern Paratethys): Implication of the chronostratigraphy and bivalvia-based biostratigraphy [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva, 2005
The Rostov Dome is located in the south of the Russian Platform. In the Late Miocene this area was embraced by the Eastern Paratethys. The implications of a recently developed Neogene chronostratigraphy to the studied area are discussed.
Ruban Dmitry A.
doaj   +3 more sources

Late Miocene Leaves and Endocarps of Choerospondias (Anacardiaceae) from Zhejiang, Eastern China: Implications for Paleogeography and Paleoclimate [PDF]

open access: yesBiology, 2022
Choerospondias (Anacardiaceae), characterized by radially arranged germination pores near the top, is a monotypic genus mainly distributed in subtropical and tropical eastern Asia, while fossil records indicate a wide distribution throughout Eurasia ...
Liang Xiao   +8 more
doaj   +2 more sources

The Miocene seal Monachopsis pontica: isolated in a shrinking sea and adapting to its changing conditions [PDF]

open access: yesRoyal Society Open Science
More than 170 years have passed since the description of the dwarf Miocene seal Monachopsis pontica. However, its cranial materials were rarely found and described. This paper re-describes M. pontica and discusses its ecological adaptations. M.
Pavlo Otriazhyi   +4 more
doaj   +2 more sources

A new seal from the Late Miocene of the Eastern Paratethys highlights the past regional diversity of true seals (Phocidae) [PDF]

open access: yesSwiss Journal of Palaeontology
True seals rapidly evolved in many forms in the epicontinental basin of Paratethys during the Miocene. However, most of their nominal taxa so far were proposed based on isolated limb bones, and their taxonomy has long been under discussion.
Pavlo Otriazhyi   +4 more
doaj   +2 more sources

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

open access: yesRoyal Society Open Science
The Dniester valley is a spectacular example of a degrading bedrock fluvial system at the contact between the East European platform and the Carpathian orogen. This study is based upon a combined lithofacies–architecture–morphological study.
Andrei V. Matoshko, Philip Gibbard
doaj   +2 more sources

The Tanais Bay of the Eastern Paratethys Sea at the Sarmatian–Maeotian Transition (Late Miocene): Widespread Desiccations and Local Uplifts in the Light of Historical Information

open access: yesJournal of Marine Science and Engineering, 2022
The Late Miocene evolution of the Eastern Paratethys Sea was marked by significant palaeogeographical transformations. The knowledge of them should be improved with the information from the peripheral parts of this semi-enclosed marine basin.
Dmitry A. Ruban
doaj   +1 more source

Hydrological Changes in Restricted Basins: Insights From Strontium Isotopes on Late Miocene‐Pliocene Connectivity of the Eastern Paratethys (Dacian Basin, Romania)

open access: yesGeochemistry, Geophysics, Geosystems, 2021
The Dacian Basin was uniquely situated to record late Miocene hydrological changes that influenced depositional environments and faunal dispersal patterns in Central Eurasia's mega‐lake Paratethys.
Iuliana Vasiliev   +10 more
doaj   +1 more source

Late miocene ostracodes of Serbia: Morphologic and palaeoenvironmental considerations [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva, 2006
About 11.5 million years ago, a tectonic uplift of the Eastern and Western Carpathians separated the Pannonian Basin from the rest of the Paratethys. This orogenesis event caused an unconformity between the Sarmatian brackish sediments and the Pannonian ...
Rundić Ljupko M.
doaj   +1 more source

THE ENDEMIC MARINE FISH FAUNA FROM THE EASTERN PARATETHYS RECONSTRUCTED FROM OTOLITHS FROM THE MIOCENE (MIDDLE SARMATIAN S.L.; BESSARABIAN) OF JURKINE (KERCH PENINSULA, CRIMEA)

open access: yesRivista Italiana di Paleontologia e Stratigrafia, 2023
Reconstructing fossil bony fish faunas using otoliths is a well-established method that allows a diverse and dense record in time and space to be assembled. Here we report about a rich otolith-based fish fauna from the middle Sarmatian s.l.
ANDRIY BRATISHKO   +2 more
doaj   +1 more source

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