Pál Müller

Universität Hamburg

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Imre Magyar

Hungarian National Museum

Miklós Lantos

Mining and Geological Survey of Hungary

Alfréd Dulai

Hungarian Natural History Museum

Gábor Csillag

Institute for Geological and Geochemical Research

Dana H. Geary

University of Wisconsin–Madison

ÁT

Ágnes Tóth‐Makk

Mining and Geological Survey of Hungary

Orsolya Sztanó

Eötvös Loránd University

E. Juhász

Total (France)

Pierre Moissette

National and Kapodistrian University of Athens

László Fodor

Eötvös Loránd University

Cooperative Institutions

Eötvös Loránd University

Mining and Geological Survey of Hungary

Centre National de la Recherche Scientifique

Institute of Paleoprimatology Human Paleontology Evolution and Paleoenvironments

Pázmány Péter Catholic University

Hungarian Academy of Sciences

Natural History Museum

Geological Institute

University of Sydney

Ludwig-Maximilians-Universität München

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A szél hatása a késő-neogén–negyedidőszaki üledékképződésre és a domborzat alakulására a Magyar-középhegységben és előterében = The effect of the wind on the late Neogene and Quaternary sedimentation and morphological evolution of the Hungarian Central Range and of its foreland

Pál Müller Gáspár Albert Gábor Csillag Ándrás Horányi Erzsébet Horváth

Legfontosabb kutatasi eredmenyeink: az eolikus uledekek es felszinek elterjedesenek es koranak meghatarozasa, megayardangok es plato helyzetű eolikus kepződmenyek leirasa, valamint a deflacio meghatarozo szerepenek kimutatasa a Dunantul mai domborzatanak, igy a zalai es somogyi un. meridionalis volgyrendszer kialakitasaban is. A szelmarta kőzetfelszinek kozmogen 10Be izotopos korat a melysegprofilok menti mintavetelezesi modszer alkalmazasaval sikerult meghataroznunk. Ezt a modszert korabban szelcsiszolta kőzetfelszineken meg nem alkalmaztak; elsőkent sikerult 1,5 millio eves szelcsiszolta sziklafelszint datalnunk Europaban. A Tapolcai- es Kali-medencek negyedidőszaki deflacios alacsonyodasi rataja 40-75 m/My volt, ugyanakkor a kipreparalodo kvarcittombok csupan 2-4 m-t pusztulnak evmillionkent. A kulonboző koru szelmarta felszineken mert szelkarc iranyok megfeleltek a mai ENy-ias szeliranynak. Ezzel igazoltuk az allandonak tekinthető uralkodo szeliranyt a negyedidőszak soran. Az OSL kormeghatarozassal 8-80 ezer eves uledekeket sikerult datalnunk a Vertes kornyezeteben. Az uledekanyag szemcseit a betemetődes előtt nem erte elegendő feny ahhoz, hogy a lumineszcens szignal teljesen lenullazodjon. Ezt valoszinűleg a rovid szallitasi tavolsag okozhatta. Ezzel magyarazhato, hogy a vizsgalt uledekek eseteben a geomorfologia es a korabbi koradatok tukreben tobbnyire a centralis OSL kor adja meg a betemetődes korat. | Our most important results are: determination of the distribution and age of aeolian landforms and sediments and description of megayardangs and aeolian formations in plateau position. We demonstrated that deflation played a definitive role in the formation of the topography of Transdanubia and in the development of the radial valley system of Zala and Somogy countries. Age and denudation rate of the wind-abraded rock surfaces was determined using in situ produced 10Be depth profiles. This was the first application of this method on wind-polished rock surfaces, and the first time when a 1.5 million years old wind-abraded surface was dated in Europe. Quaternary deflational surface lowering of the Tapolca and Kal Basins was 40-75 m/My, while denudation rate of the cemented quartzite rock surfaces was only 2-4 m/My. We proved long term stability of north-westerly winds by the measurement of the direction of wind striations rock surfaces of different age. OSL ages of aeolian sediments in the Vertes foreland were 8-80 ky old. The sediments were not exposed to sunlight for enough time to anneal completely the luminescence signal, most probably because of the short distance of transportation. This is the reason why the central OSL ages provide the age of sedimentation, considering the geomorphology and previous age data as well.

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Climatically driven sedimentary cycles in the Late Miocene sediments of the Pannonian Basin, Hungary

Tectonophysics (1997)

E. Juhász Lóránt Kovács Pál Müller Ágnes Tóth‐Makk Laura Phillips

Milankovitch cycles

Pannonian Basin

Neogene

Climate oscillation

10.1016/s0040-1951(97)00222-9

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Citations (41)

Ancient Lake Pannon and its endemic molluscan fauna (Central Europe; mio-pliocene)

Advances in ecological research/Advances in Ecological Research (2000)

Dana H. Geary Imre Magyar Pál Müller

Endemism

10.1016/s0065-2504(00)31025-x

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ORBITAL CYCLICITY AND ASTRONOMICAL CALIBRATION OF THE UPPER MIOCENE CONTINENTAL SUCCESSION CORED AT THE IHAROSBERÉNY-I WELL SITE, WESTERN PANNONIAN BASIN, HUNGARY

SEPM (Society for Sedimentary Geology) eBooks (2004)

Marco Sacchi Pál Müller

This volume is derived from an SEPM international workshop entitled Multidisciplinary Approach to Cyclostratigraphy, organized by the editors in May 2001 and held in Sorrento (Naples, Italy). In the Introduction we offer a brief history of how concepts of orbital cyclicity and its effects on the Earth evolved, an appraisal of the present state of research, and an overview of the papers in this volume. The main body of the volume consists of the contributed studies. These include a paper on conceptual and pragmatic approaches to stratification cycles by one of the pioneers of cyclostratigraphy, Walther Schwarzacher, who, in the 1940s, discovered the hierarchical expression of orbital cycles in rocks. The other contributions are specific studies of cyclic sequences, extending from the Quaternary back to the Triassic, covering the range from continental deposits to the deep sea, and employing a wide variety of techniques for extracting and processing the information.

Pannonian Basin

10.2110/pec.04.81.0275

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Late Eocene coral-associated decapods (Crustacea) from Hungary

Pál Müller J.S.H. Collins

Fifty-eight species of fossil crabs are recorded and figured from Facies 4, a coral-bearing limestone, of the Szepvolgy Formation (Late Eocene, Priabonian) of Hungary. The following 18 genera, 1 subgenus and 35 species are new: Dardanus curtimanus, Pagurus latidactylus, Diogenes longimanus, Paguristes oligotuberculatus, Galathea (Acanthogalathea subgen. nov.) parva, Protomunida pentacantha, Longoporcellana denticulata gen. nov., Polyonyx arcuatus, Petrolisthes ? striatissimus, Ovocarcinus elongatus gen. nov., Dromilites fossata, Dromilites subglobosa, Kromtitis pentagonalis, Cymonomus primitivus, Ovamene franciae gen. nov., Ethusa evae, Gemmacarcinus fossatus gen. nov., Nanomaja simplex gen. nov., Mesolambrus declinatus gen. nov., Actaeites lobatus gen. nov., Paraxanthosia budensis gen. nov., Pilumnomimus planidentatus, Priabonocarcinus gallicus gen. nov., Prochlorodius ellipticus gen. nov., Sculptoplax rigida gen. nov., Eomaldivia pannonica gen. nov., Eomaldivia trispinosa, Budapanopeus denticulatus gen. nov., Panopeus granulineatus, Branchioplax sulcata, Caprocancer altus gen. nov., Corallicarcinus planus gen. nov., Daragrapsus trispinosus gen. nov., Eoplax minima gen. nov., and Palaeograpsus bittneri. Another new genus, Lobogalenopsis gen. nov., is introduced to accommodate a previously described species and eight species in as many genera are described, but not named.

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Anomura

Hermit crab

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Iterative changes in Lake PannonMelanopsisreflect a recurrent theme in gastropod morphological evolution

Paleobiology (2002)

Dana H. Geary Andrew W. Staley Pál Müller Imre Magyar

Iterative evolutionary changes are of special interest because they imply that the recurring morphological changes had a cause that also repeated itself and might therefore be possible to uncover. We describe a set of iterative morphological changes in melanopsid gastropods from the ancient, long-lived Lake Pannon. First in the Pannonian Age, and again in the Pontian Age approximately three million years later, a smooth-shelled ancestor gave rise to a shouldered descendant. In both cases, the morphological change was probably coincident with a shift from habitats just outside the lake (e.g., rivers and streams) to habitats within the lake itself. Many other convergent examples exist in which a smooth-shelled river dweller is closely related to a shouldered and/or ribbed lacustrine snail. The frequency of this type of morphological change suggests that it has an adaptive basis; response to differing predators or hydrodynamic conditions seem the most plausible explanations, but the functional nature of these morphological changes remains unknown.

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10.1666/0094-8373(2002)028<0208:icilpm>2.0.co;2

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Citations (35)

Lower Pliocene Decapod crustaceans from the Southwestern Iberian Peninsula (Guadalquivir basin, Sevilla, Spain)

Geobios (1998)

Eduardo Mayoral Pál Müller Fernando Muñiz Guinea

Peninsula

10.1016/s0016-6995(98)80122-8

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