1987
DOI: 10.1127/nos/17/1987/129
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Biostratigraphic correlations in the Eastern Mediterranean Neogene - 8. Calibration of Sporomorph- and Rodent-Associations from the Megalopolis Basin (Peloponnesus, Greece)

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Cited by 8 publications
(3 citation statements)
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“…At the change from Pliocene to Pleistocene the temperature conditions were probably comparable to the present‐day conditions. The Megalopolis pollen‐association indicates a clearly cooler climate 1.6 Myr ago, probably related to the Euburon‐cold period of north‐western Europe (Benda et al ., 1987). This led to the successive vanishing of the thermophilic and humidophilic tertiary elements which were so characteristic for the vegetation composition before (Hesselbarth et al ., 1995).…”
Section: Discussionmentioning
confidence: 99%
“…At the change from Pliocene to Pleistocene the temperature conditions were probably comparable to the present‐day conditions. The Megalopolis pollen‐association indicates a clearly cooler climate 1.6 Myr ago, probably related to the Euburon‐cold period of north‐western Europe (Benda et al ., 1987). This led to the successive vanishing of the thermophilic and humidophilic tertiary elements which were so characteristic for the vegetation composition before (Hesselbarth et al ., 1995).…”
Section: Discussionmentioning
confidence: 99%
“…The faunal composition of the Apolakkia Formation suggests that it was formed during the Middle and Late Ruscinian, i.e., about 5.3-3.4 Ma (Van de weerd et al 1982;Benda et al 1987), an age determination that was recently corroborated by a palaeomagnetic study (Van hInsBerGen et al 2007).…”
Section: Introductionmentioning
confidence: 95%
“…The transition from Microtus (Allophaiomys) to Microtus (Microtus) species marks the transition between the Early and the Late Biharian and the Mimomys -Arvicola transition during the early Middle Pleistocene marks the end of the Biharian and the beginning of the Toringian (e.g., Fejfar and Heinrich, 1981;Tesakov, 2004). Benda et al (1987) In order to resolve the debate on the stratigraphical position of the Marathousa Member, Doukas and colleagues sampled the Marathousa Member in 1995 at a section exposed at Choremiou. The lowermost Lignite Seam I, the base of Lignite Seam II and Lignite Seam III yielded botanical as well as faunal remains; mammalian fossils are, however, not very abundant (Van Vugt, 2000;Doukas and Papayianni, 2016).…”
Section: Introductionmentioning
confidence: 99%