A new occurrence of classic “Árpád-type” mollusk fauna from the Upper Miocene of Kozármisleny, southern Hungary
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Abstract
A classic but very rare “Árpád-type” mollusk assemblage, representing the endemic fauna of the Late Miocene–Early Pliocene Lake Pannon, was discovered in Kozármisleny (near Pécs, southern Hungary). The fossils were collected from silt layers deposited in the shallow sublittoral zone of Lake Pannon, and exposed by an 8–10 m high road cut. The assemblage contained some very rare species, including the type species of genus Lymnocardium, L. haueri (M. Hörnes). Palynological investigations from the same layers failed to yield age-diagnostic dinoflagellates, and pointed to strongly freshened water and warm, subtropical climate.
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References
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BRUSINA, S. (1884): Die Fauna der Congerienschichten von Agram in Kroatien. – Beiträge zur Geologie und Paläontologie Österreich-Ungarns und Orients, Vol. 3, 125–187.
GEARY, D.H., MAGYAR, I. & MÜLLER, P. (2000): Ancient Lake Pannon and its Endemic Molluscan Fauna (Central Europe; Mio-Pliocene).– In: ROSSITER, A. & KAWANABE, H. (eds.): Ancient Lakes: Biodiversity, Ecology, and Evolution. Advances in Ecological Research 3, 463–482.
GEARY, D.H., HUNT, G., MAGYAR, I. & SCHREIBER, H. (2010): The paradox of gradualism: phyletic evolution in two lineages of lymnocardiid bivalves (Lake Pannon, central Europe).–Paleobiology, Vol. 36, 592–614. doi: 10.1666/08065.1
HÖRNES, M. (1862): Die fossilen Mollusken des tertiaer-Beckens von Wien.–Conchifera (Acephala), Vol. 2, 1–479.
KONERT, M. & VANDENBERGHE, J. (1997): Comparison of laser grain-size analysis with pipette and sieve analysis, a solution for the underestimation of the clay fraction.–Sedimentology, Vol. 44, 523–535. doi: 10.1046/j.1365-3091.1997.d01-38.x
KOVÁCS, J. (2008): Grain-size analysis of the Neogene red clay formation in the Pannonian Basin.–Int. J. Earth Sci., Vol. 97, 171–178. doi: 10.1007/s00531-006-0150-2
MÜLLER, P., GEARY, D.H. & MAGYAR, I. (1999): The endemic molluscs of the Late Miocene Lake Pannon: their origin, evolution, and family-level taxonomy.–Lethaia, Vol. 32, 47–60. doi: 10.1111/j.1502-3931.1999.tb00580.x
SEBE, K., CSILLAG, G. & KONRÁD, G. (2008): The role of neotectonics in fluvial landscape development in the Western Mecsek Mountains and related foreland basins (SE Transdanubia, Hungary).–Geomorphology, Vol. 102, 55–67. doi: 10.1016/j.geomorph.2007.05.018
SEBE, K., KONRÁD, G. & MAGYAR, I. (2013): A legmagasabban fekvő mecseki pannon-tavi üledékek helyzete és kora.–Földt. Közl., Vol. 143, 445–468.
STEVANOVIĆ, P.M. (1951): Pontische Stufe im engeren Sinne - obere Congerienschichten Serbiens und der angrenzenden Gebiete. 361 pp. Serbische Akademie der Wissenschaften, Sonderausgabe 187, Mathematisch-Naturwissenschaftliche Klasse No. 2, Beograd.
SZÓNOKY, M., DOBOS-HORTOBÁGYI, E., GULYÁS, S., MÜLLER, P., SZUROMI-KORECZ, A., GEARY, D.H. & MAGYAR, I. (1999): Árpád, a classic locality of Lake Pannon bivalves.–Acta Geol. Hung., Vol. 42, 89–108.