2013
DOI: 10.1016/j.gloplacha.2012.04.004
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Paleoenvironmental evolution of the East Carpathian foredeep during the late Miocene–early Pliocene (Dacian Basin; Romania)

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Cited by 83 publications
(102 citation statements)
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“…The total number of species reached a temporary maximum, mostly because of the presence of the rich fauna of Lake Dacia (31,33). With the isolation of the basin in the Late Dacian/Middle Zanclean, ∼4 Mya, freshwater conditions started to develop (31), offering suitable conditions for mollusk settlement and evolution.…”
Section: Significancementioning
confidence: 99%
“…The total number of species reached a temporary maximum, mostly because of the presence of the rich fauna of Lake Dacia (31,33). With the isolation of the basin in the Late Dacian/Middle Zanclean, ∼4 Mya, freshwater conditions started to develop (31), offering suitable conditions for mollusk settlement and evolution.…”
Section: Significancementioning
confidence: 99%
“…2012). For the Eastern Paratethys Neogene the following regional divisions were adopted: Caucasian, Batisifonian (Sakaraulian and Kotsakhurian), Tarkhanian, Chokrakian, Karaganian Konkian, Sarmatian, Meotian, Pontian, Kimmerian, Kuyalnikian (Akchagilian), Vasiliev et al (2011) and Stoica et al (2013). For the purpose of definition of correlation levels, the most complete sections of the Central Paratethys were studied in north-western Ukraine (Transcarpathian Basin, Outer Carpathian nappe units, Eastern Carpathian Foredeep and the adjacent part of the Eastern European Platform).…”
Section: History Fundamentals and Creation Of Correlation Levelsmentioning
confidence: 99%
“…atavus. In neighbouring Stoica et al (2013), and ter Borgh et al (2013). The boundaries of the intervals used by Wenz (1923Wenz ( -1930 are adapted to those of the current stages.…”
Section: Stratigraphymentioning
confidence: 99%