Zobrazeno 1 - 10
of 131
pro vyhledávání: '"OLEG MANDIC"'
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-14 (2024)
Abstract The Miocene Climate Optimum (MCO, ~ 17–14 Ma) was a time of extraordinary marine biodiversity in the Circum-Mediterranean Region. This boom is best recorded in the deposits of the vanished Central Paratethys Sea, which covered large parts
Externí odkaz:
https://doaj.org/article/ef31a29d61f943f79de7015ceefc53ba
Publikováno v:
Diversity, Vol 16, Iss 8, p 508 (2024)
The Croatian Natural History Museum (CNHM) houses rich fossil collections from the Neogene deposits of Northern Croatia, comprising numerous scallops (Bivalvia: Pectinidae). During the Middle Miocene (Badenian = Langhian and early Serravallian), this
Externí odkaz:
https://doaj.org/article/6b989ff1fb3241ac8146db65ccda61c3
Autor:
MICHAL ŠUJAN, RÉGIS BRAUCHER, OLEG MANDIC, KLEMENT FORDINÁL, BIBIANA BRIXOVÁ, RADOVAN KYŠKA PIPÍK, VLADIMÍR ŠIMO, MICHAL JAMRICH, SAMUEL RYBÁR, TOMÁŠ KLUČIAR, ASTER TEAM, ANDREJ RUMAN, IVAN ZVARA, MICHAL KOVÁČ
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 127, Iss 3 (2021)
The depocenters of epicontinental basins usually comprise relatively continuous depositional records, and these can be used in the determination of sediment routing and paleogeographic changes via a set of various geophysical, sedimentological, biost
Externí odkaz:
https://doaj.org/article/793635ecbeb242f8ac3cbffcf88e3df8
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 124, Iss 3 (2018)
We present a taxonomic and palaeoecological analysis of a continental mollusc fauna from a mammoth-bearing succession near Bullendorf in Lower Austria. The taxonomic analysis comprises morphological descriptions and SEM documentation of 15 Pleistocen
Externí odkaz:
https://doaj.org/article/c6f68dbe18724af4b989599cc6ac5b14
Publikováno v:
Geologia Croatica, Vol 68, Iss 3, Pp 179-207 (2015)
The mollusk fauna from the Pliocene Viviparus beds of Vukomeričke Gorice hills in central Croatia was investigated at four sites in the region of Kravarsko, S of Zagreb. The region represents a Pleistocene dome-anticline at the southern margin of th
Externí odkaz:
https://doaj.org/article/fa4481dafe77430082833ced3531f76c
Publikováno v:
ZooKeys, Vol 435, Iss 0, Pp 1-6 (2014)
Here we present a complete list of all valid species-group taxa of freshwater gastropods reported from Miocene and Pliocene deposits in Europe. The last comparable work dates back to the 1920s and covered about 1,600 names. The extensive literature r
Externí odkaz:
https://doaj.org/article/9f230bbce6e34d619451f82afe1ada79
Publikováno v:
ZooKeys, Vol 429, Iss 0, Pp 13-46 (2014)
In the course of a new database project on Miocene to Recent freshwater gastropods of Europe, a great many of primary and secondary homonyms were revealed. Such nomenclatural issues need clarification in order to avoid misunderstandings and wrong sta
Externí odkaz:
https://doaj.org/article/0866b6afc4924ce29cd0d21afaf618db
Autor:
Stjepan Ćorić, Davor Pavelić, Fred Rögl, Oleg Mandic, Sejfudin Vrabac, Radovan Avanić, Lazar Jerković, Alan Vranjković
Publikováno v:
Geologia Croatica, Vol 62, Iss 1, Pp 31-43 (2011)
The Pannonian Basin System (PBS) originated during the Early Miocene as a result of extensional processes between the Alpine-Carpathian and the Dinaride Orogenic Belts. The Paratethys Sea flooded the new basins successively during the Karpatian (late
Externí odkaz:
https://doaj.org/article/f68fd85ba5f84c7c93746a9a9695e07b
Autor:
MATHIAS HARZHAUSER, MARKUS REUTER, OLEG MANDIC, SIMON SCHNEIDER, WERNER E. PILLER, MARCO BRANDANO
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 119, Iss 3 (2013)
We present a revision of the Late Miocene mollusc assemblages from Faro Santa Croce (FSC) in SE Sicily. The FSC-section exposes lower Messinian coastal marine limestones of the Monte Carrubba Formation. Whilst the lowermost part is characterised by i
Externí odkaz:
https://doaj.org/article/64e3ae2d6246449e8fc2ede6abe582d3
The Central Paratethys Sea occupied the transition between the Alps, Dinarides and Carpathian mountains during Oligocene to Miocene times. However, its spatial and temporal evolution, i.e. southward expansion, subsequent salinity crisis, and governin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dfc667e7624e9975db64490b47b2ccec
https://doi.org/10.5194/egusphere-egu23-9107
https://doi.org/10.5194/egusphere-egu23-9107
