A new Oligocene flora from Ludvíkovice near Děčín (České středohoří Mts., the Czech Republic)

Stránky 297-314
DOI 10.37520/fi.2020.024
Klíčová slova fossil, leaves, fruit, morphology, vegetation, climate, North Bohemia, Palaeogene
Typ článku Recenzovaný článek
Citace TEODORIDIS, Vasilis, KVAČEK, Zlatko, RADOŇ, Miroslav, RAPRICH, Vladislav a BRUCH, Angela A.. A new Oligocene flora from Ludvíkovice near Děčín (České středohoří Mts., the Czech Republic). Fossil Imprint / Acta Musei Nationalis Pragae, Series B – Historia Naturalis. Praha: Národní muzeum, 2020, 76(2), 297-314. DOI: https://doi.org/10.37520/fi.2020.024. ISSN 2533-4050 (tisk), 2533-4069 (online). Dostupné také z: https://publikace.nm.cz/periodicke-publikace/fiamnpsbhn/76-2/a-new-oligocene-flora-from-ludvikovice-near-decin-ceske-stredohori-mts-the-czech-republic
Fossil Imprint / Acta Musei Nationalis Pragae, Series B – Historia Naturalis | 2020/76/2

A recently recovered site of plant macrofossils, Ludvíkovice, in the České středohoří Mts. is situated on Sokolí vrch hill, belonging to the Děčín Formation (radiometrically dated to 30.8–24.7 Ma), according to regional stratigraphy. The flora has yielded a fern, Rumohra recentior, and several angiosperms, but no conifers. The prevailing foliage is preserved without cuticles. Noteworthy are records of Daphnogene cinnamomifolia, Laurophyllum cf. acutimontanum, Platanus neptuni, Sloanea artocarpites, Carya fragiliformis / C. quadrangula, Alnus rhenana, Trigonobalanopsis rhamnoides, Eotrigonobalanus furcinervis and cf. Quercus sp. Several foliage specimens of dicots could not be identified to species level, i.e., Leguminophyllum sp., Pungiphyllum cf. cruciatum and Dicotylophyllum sp. div. The fossil plant assemblage of Ludvíkovice corresponds to zonal mesophytic vegetation accompanied by riparian elements. This is corroborated by the Integrated Plant Record vegetation analysis, which reconstructs a zonal broad-leaved evergreen forest similar to the living broad-leaved evergreen sclerophyllous forest from Southern Hunan and Northern Guangxi in SE China. The vegetation thrived under a humid climate characterized by average values of MAT (14.6–24.1 °C), WMMT (24.7–28.3 °C), CMMT (2.2–18.8 °C) and MAP (979–1724 mm). The fossil flora of Ludvíkovice is similar in composition to the floras of Markvartice, Veselíčko, also from the Oligocene Děčín Formation of the České středohoří Mts. and the Hrazený hill.

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