Changing perspectives in the concept of “Lago-Mare” in Mediterranean Late Miocene evolution

F Orszag-Sperber - Sedimentary Geology, 2006 - Elsevier
The Cenozoic Alpine orogeny caused the partition of Tethys into several basins. During the
Late Neogene, the Mediterranean attained its final configuration, whereas, eastwards, the …

[HTML][HTML] Changing seas in the late Miocene Northern Aegean: A Paratethyan approach to Mediterranean basin evolution

W Krijgsman, DV Palcu, F Andreetto, M Stoica… - Earth-Science …, 2020 - Elsevier
Abstract The Northern Aegean region evolved during the Miocene as a restricted land-
locked basin with small ephemeral connections to both the Eastern Paratethys (former Black …

Slab detachment beneath eastern Anatolia: A possible cause for the formation of the North Anatolian fault

C Faccenna, O Bellier, J Martinod, C Piromallo… - Earth and Planetary …, 2006 - Elsevier
In this paper, we discuss the possibility that the North Anatolian fault (NAF) results from the
deep deformation of the slab beneath the Bitlis–Hellenic subduction zone. We described the …

Phylogenetic relationships and biogeographical patterns in Circum-Mediterranean subfamily Leuciscinae (Teleostei, Cyprinidae) inferred from both mitochondrial and …

S Perea, M Böhme, P Zupančič, J Freyhof… - BMC evolutionary …, 2010 - Springer
Background Leuciscinae is a subfamily belonging to the Cyprinidae fish family that is widely
distributed in Circum-Mediterranean region. Many efforts have been carried out to …

Rise and fall of the Paratethys Sea during the Messinian Salinity Crisis

W Krijgsman, M Stoica, I Vasiliev, VV Popov - Earth and Planetary Science …, 2010 - Elsevier
Extremely thick evaporite units were deposited during the so-called Messinian Salinity Crisis
(MSC: 5.96–5.33 Ma) in a deep Mediterranean basin that was progressively disconnected …

Lithospheric-scale geodynamic context of the Messinian salinity crisis

L Jolivet, R Augier, C Robin, JP Suc, JM Rouchy - Sedimentary geology, 2006 - Elsevier
Comparison between the tectonic and palaeogeographic evolution of the Mediterranean
region from the Oligocene to the Present shows that the isolation of the Mediterranean …

The isolation of the Pannonian basin (Central Paratethys): New constraints from magnetostratigraphy and biostratigraphy

M ter Borgh, I Vasiliev, M Stoica, S Knežević… - Global and Planetary …, 2013 - Elsevier
In this paper we establish when and how the Pannonian basin and associated Central
Paratethys basins were isolated from the remainder of the Paratethys, a system of back-arc …

Propagation of a strike-slip plate boundary within an extensional environment: the westward propagation of the North Anatolian Fault

X Le Pichon, AMC Şengör, J Kende… - Canadian Journal of …, 2016 - cdnsciencepub.com
We document the establishment of the Aegea–Anatolia/Eurasia plate boundary in Pliocene–
Pleistocene time. Before 2 Ma, no localized plate boundary existed north of the Aegean …

Late Miocene–Early Pliocene evolution of Mediterranean gobies and their environmental and biogeographic significance

W Schwarzhans, K Agiadi, G Carnevale - Rivista Italiana di …, 2020 - riviste.unimi.it
The Lago Mare phase at the end of the Messinian Salinity Crisis (MSC) in the Mediterranean
has long been known for the Paratethyan affinities of its biota. The taxonomic level of these …

Paleoenvironmental evolution of the East Carpathian foredeep during the late Miocene–early Pliocene (Dacian Basin; Romania)

M Stoica, I Lazăr, W Krijgsman, I Vasiliev, D Jipa… - Global and Planetary …, 2013 - Elsevier
The thick and continuous Mio-Pliocene sedimentary successions of the Focşani Depression
in the Dacian Basin of Romania provide an excellent opportunity to study the …