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DOI10.1016/j.palaeo.2019.109398
Volcanism and paleoenvironment of the pula maar complex: A pliocene terrestrial fossil site in Central Europe (Hungary)
Kovács J.; Németh K.; Szabó P.; Kocsis L.; Kereszturi G.; Újvári G.; Vennemann T.
发表日期2020
ISSN0031-0182
卷号537
英文摘要We describe the Late Pliocene paleoenvironment and paleoclimate of the Pula fossil site of the western Pannonian Basin, Hungary, which occurs within a lacustrine succession deposited in a volcanic crater (maar). Radiometric dating of adjacent volcanic bodies hosting the fossil-bearing sedimentary assemblages gives an age of 4.25 ± 0.17 Ma (K–Ar). To date, five, articulated rhinoceros skeletons (Dihoplus sp.) have been recovered, and a few fragmentary remains of artiodactyls and freshwater fishes (Perca sp., Leuciscus sp. and Gobius sp.) are also present. An insect taphocoenosis comprises terrestrial groups that inhabited the former lake margins (Syrphidae, Heteroptera, Chalcidoidea, Tenebrionidae) as well as aquatic insects (Dytiscidae, Baetidae, and Chironomidae). Deciduous broad-leaved, woody plants prevailed in and around the Pula locality (Quercus, Ulmus, Zelkova, Acer, Salicaceae) and are associated with some rare floral elements (Ginkgo, Sassafras) and Buxus. Deposition at the lake bottom seems to have taken place in oxygen-depleted layers, and taphonomic evidence indicates that fossil material underwent minimal (if any) weathering. δ13C values of one rhinoceros tooth suggest that this mammal consumed mixed C3 plants in a wooded environment. The climatic conditions inferred from the reconstructed vegetation and stable oxygen isotope data from the tooth enamel support a Cf-type climate (Köppen classification) with a mean annual temperature of 10–13 °C with some dry periods during the year. Pula is comparable to other maar fossil sites of Pliocene age such as Camp dels Ninots, Spain, and Hajnáčka I, Slovakia. © 2019 Elsevier B.V.
英文关键词Animal fossils; Central europe; Maar; Paleovegetation; Pliocene; Stable isotopes
语种英语
scopus关键词crater; explosive volcanism; fossil record; geographical distribution; oxygen isotope; paleoclimate; paleoenvironment; Pliocene; skeleton; stable isotope; taphonomy; terrestrial environment; tooth; volcanism; Czechoslovakia; Pannonian Basin; Slovakia; Acer; Animalia; Artiodactyla; Baetidae; Buxus; Chalcidoidea; Chironomidae; Dytiscidae; Gobius sp.; Heteroptera; Hexapoda; Leuciscus sp.; Mammalia; Perca; Pisces; Quercus; Rhinoceros; Salicaceae; Sassafras; Syrphidae; Tenebrionidae; Ulmus; Zelkova
来源期刊Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/150746
作者单位Department of Geology and Meteorology, University of Pécs, Ifjúság U. 6, Pécs, H-7624, Hungary; Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Pécs, Hungary; Geosciences, School of Agriculture and Environment, Massey University, Private Bag 11 222, Palmerston North, 4442, New Zealand; Geology Group, Universiti Brunei Darussalam, Darussalam, Brunei Darussalam; Department of Lithospheric Research, University of Vienna, Vienna, Austria; Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budapest, Hungary; Institute of Earth Surface Dynamics, University of Lausanne, Lausanne, Switzerland
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Kovács J.,Németh K.,Szabó P.,et al. Volcanism and paleoenvironment of the pula maar complex: A pliocene terrestrial fossil site in Central Europe (Hungary)[J],2020,537.
APA Kovács J..,Németh K..,Szabó P..,Kocsis L..,Kereszturi G..,...&Vennemann T..(2020).Volcanism and paleoenvironment of the pula maar complex: A pliocene terrestrial fossil site in Central Europe (Hungary).Palaeogeography, Palaeoclimatology, Palaeoecology,537.
MLA Kovács J.,et al."Volcanism and paleoenvironment of the pula maar complex: A pliocene terrestrial fossil site in Central Europe (Hungary)".Palaeogeography, Palaeoclimatology, Palaeoecology 537(2020).
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