Erdei, Boglarka; Hably, Lilla; Kazmer, Miklos; Utescher, Torsten; Bruch, Angela A (2007): Oligocene to Pliocene palaeoclimate reconstructions from 18 sites in Hungary. PANGAEA, https://doi.org/10.1594/PANGAEA.587448, Supplement to: Erdei, B et al. (2007): Neogene flora and vegetation development of the Pannonian domain in relation to palaeoclimate and palaeogeography. Palaeogeography, Palaeoclimatology, Palaeoecology, 253(1-2), 131-156, https://doi.org/10.1016/j.palaeo.2007.03.036
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A survey of the Neogene flora and vegetation pattern of the Pannonian domain based on 18 selected fossil plant assemblages is given. Flora and vegetation patterns are based on well-documented and studied fossil plant assemblages (macrofloras, primarily leaves). A general but slow cooling trend is definitely observable after the Early Miocene as reflected by both quantitative climate reconstructions and floristic change, i.e. decrease of diversity, slow disappearance of thermophilous and exotic elements, as well as decrease in the variety of vegetation types. A significant decline of coldest month temperatures (as compared to warmest month temperatures) must have played a defining role in forming flora and vegetation through the Neogene.
Median Latitude: 47.668722 * Median Longitude: 19.624333 * South-bound Latitude: 46.250000 * West-bound Longitude: 17.017000 * North-bound Latitude: 48.283000 * East-bound Longitude: 21.367000
Andornaktalya * Latitude: 47.850000 * Longitude: 20.417000 * Elevation: 150.0 m * Location: Hungary * Campaign: NECLIME_campaign * Device: Quarry (QU)
Budapest_city * Latitude: 47.500000 * Longitude: 19.067000 * Location: Hungary * Campaign: NECLIME_campaign