@article{MTMT:31955461,
	title = {‘X’ marks the spot! Sedimentological, geochemical and palaeontological investigations of Upper Cretaceous (Maastrichtian) vertebrate fossil localities from the Vălioara valley (Densuş-Ciula Formation, Hațeg Basin, Romania)},
	url = {https://m2.mtmt.hu/api/publication/31955461},
	author = {Botfalvai, Gábor and Csiki-Sava, Z and Kocsis, L and Albert, Gáspár and Magyar, János and Bodor, Emese Réka and Ţabără, D and Ulyanov, A and Makádi, László},
	doi = {10.1016/j.cretres.2021.104781},
	journal-iso = {CRETACEOUS RES},
	journal = {CRETACEOUS RESEARCH},
	volume = {123},
	unique-id = {31955461},
	issn = {0195-6671},
	year = {2021},
	eissn = {1095-998X},
	orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036; Csiki-Sava, Z/0000-0001-7144-0327; Albert, Gáspár/0000-0002-1723-8328; Magyar, János/0000-0002-2072-0174; Bodor, Emese Réka/0000-0003-3894-2506; Ulyanov, A/0000-0001-7047-6862; Makádi, László/0000-0001-6829-0241}
}

@article{MTMT:32533253,
	title = {Sarmatian and Pannonian mollusks from Pécs-Danitzpuszta, southern Hungary: a unique local faunal succession},
	url = {https://m2.mtmt.hu/api/publication/32533253},
	author = {Botka, Dániel Bálint and Rofrics, N and Katona, Lajos Tamás and Magyar, Imre},
	doi = {10.23928/foldt.kozl.2021.151.4.335},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {151},
	unique-id = {32533253},
	issn = {0015-542X},
	year = {2021},
	eissn = {2559-902X},
	pages = {335-361},
	orcid-numbers = {Botka, Dániel Bálint/0000-0002-6627-4640}
}

@article{MTMT:32525530,
	title = {An exceptional surface occurrence: the middle to upper Miocene succession of Pécs-Danitzpuszta (SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/32525530},
	author = {Sebe, Krisztina and Konrád, Gyula and Sztanó, Orsolya},
	doi = {10.23928/foldt.kozl.2021.151.3.235},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {151},
	unique-id = {32525530},
	issn = {0015-542X},
	year = {2021},
	eissn = {2559-902X},
	pages = {235-252},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:32525556,
	title = {A diverse Miocene fish assemblage (Chondrichthyes and Osteichthyes) from the Pécs-Danitzpuszta sand pit (Mecsek Mts, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/32525556},
	author = {Szabó, M and Kocsis, L and Bosnakoff, M and Sebe, Krisztina},
	doi = {10.23928/foldt.kozl.2021.151.4.363},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {151},
	unique-id = {32525556},
	issn = {0015-542X},
	year = {2021},
	eissn = {2559-902X},
	pages = {363-409},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:32290175,
	title = {Szórványleletek a Magyar Természettudományi Múzeum gyűjteményében: Óriásszalamandra, †Andrias scheuchzeri (Holl, 1831) farokcsigolyák a késő-miocén pannon pécs-danitzpusztai (Magyarország) ősgerinces lelőhelyről (Caudata: Amphibia: Cryptobranchidae)},
	url = {https://m2.mtmt.hu/api/publication/32290175},
	author = {Szentesi, Zoltán},
	doi = {10.53019/AnnlsMusHistNatHung.2021.113.11},
	journal-iso = {ANNLS MUS HIST-NAT HUNG},
	journal = {ANNALES MUSEI HISTORICO-NATURALIS HUNGARICI},
	volume = {113},
	unique-id = {32290175},
	issn = {0521-4726},
	year = {2021},
	pages = {11-23},
	orcid-numbers = {Szentesi, Zoltán/0000-0002-7019-5478}
}

@article{MTMT:32525536,
	title = {Various marginal marine environments in the Central Paratethys: Late Badenian and Sarmatian (middle Miocene) marine and non-marine microfossils from Pécs-Danitzpuszta, southern Hungary},
	url = {https://m2.mtmt.hu/api/publication/32525536},
	author = {Szuromi-Korecz, Andrea and Magyar, Imre and Sztanó, Orsolya and Beliczainé Csoma, Vivien and Botka, Dániel Bálint and Sebe, Krisztina and Tóth, Emőke},
	doi = {10.23928/foldt.kozl.2021.151.3.275},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {151},
	unique-id = {32525536},
	issn = {0015-542X},
	year = {2021},
	eissn = {2559-902X},
	pages = {275-305},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653; Beliczainé Csoma, Vivien/0000-0002-2593-5537; Botka, Dániel Bálint/0000-0002-6627-4640; Sebe, Krisztina/0000-0002-4647-2199; Tóth, Emőke/0000-0002-1733-7828}
}

@article{MTMT:31618797,
	title = {Geochemical analyses suggest stratigraphic origin and late Miocene age of reworked vertebrate remains from Penanjong Beach in Brunei Darussalam (Borneo).},
	url = {https://m2.mtmt.hu/api/publication/31618797},
	author = {Kocsis, László and Botfalvai, Gábor and Qamarina, Qahirah and Razak, Hazirah and Király, Edit and Lugli, Federico and Wings, Oliver and Lambertz, Markus and Raven, Han and Briguglio, Antonino and Rabi, Márton},
	doi = {10.1080/08912963.2020.1819999},
	journal-iso = {HIST BIOL},
	journal = {HISTORICAL BIOLOGY},
	volume = {33},
	unique-id = {31618797},
	issn = {0891-2963},
	year = {2020},
	eissn = {1029-2381},
	pages = {2627-2638},
	orcid-numbers = {Kocsis, László/0000-0003-4613-1850; Botfalvai, Gábor/0000-0002-5479-9036; Wings, Oliver/0000-0002-6482-6683; Raven, Han/0000-0002-5305-0795}
}

@article{MTMT:30994641,
	title = {Giant salamander from the Miocene of the Mecsek mountains (Pécs-Danitzpuszta, southwestern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/30994641},
	author = {Szentesi, Zoltán and Sebe, Krisztina and Szabó, Márton},
	doi = {10.1007/s12542-019-00499-2},
	journal-iso = {PALAEONTOL Z},
	journal = {PALAEONTOLOGISCHE ZEITSCHRIFT},
	volume = {94},
	unique-id = {30994641},
	issn = {0031-0220},
	year = {2020},
	eissn = {1867-6812},
	pages = {353-366},
	orcid-numbers = {Szentesi, Zoltán/0000-0002-7019-5478; Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:30738709,
	title = {Interplay of sediment supply and lake-level changes on the margin of an intrabasinal basement high in the Late Miocene Lake Pannon (Mecsek Mts., Hungary)},
	url = {https://m2.mtmt.hu/api/publication/30738709},
	author = {Budai, Soma and Sebe, Krisztina and Nagy, Gábor and Magyar, Imre and Sztanó, Orsolya},
	doi = {10.1007/s00531-019-01745-3},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {108},
	unique-id = {30738709},
	issn = {1437-3254},
	year = {2019},
	eissn = {1437-3262},
	pages = {2001-2019},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:30379885,
	title = {Miocene syn-rift lacustrine sediments in the Mecsek Mts. (SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/30379885},
	author = {Sebe, Krisztina and Selmeczi, Ildikó and Szuromi-Korecz, Andrea and Hably, Lilla and Kovács, Ádám and Benkó, Zsolt},
	doi = {10.1007/s00015-018-0336-1},
	journal-iso = {SWISS J GEOSCI},
	journal = {SWISS JOURNAL OF GEOSCIENCES},
	volume = {112},
	unique-id = {30379885},
	issn = {1661-8726},
	year = {2019},
	eissn = {1661-8734},
	pages = {83-100},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:3189083,
	title = {Gradual changes in upwelled seawater conditions (redox, pH) from the late Cretaceous through early Paleogene at the northwest coast of Africa: Negative Ce anomaly trend recorded in fossil bio-apatite},
	url = {https://m2.mtmt.hu/api/publication/3189083},
	author = {Kocsis, László and Gheerbrant, E and Mouflih, M and Cappetta, H and Ulianov, A and Chiaradia, M and Bardet, N},
	doi = {10.1016/j.chemgeo.2015.12.001},
	journal-iso = {CHEM GEOL},
	journal = {CHEMICAL GEOLOGY},
	volume = {421},
	unique-id = {3189083},
	issn = {0009-2541},
	abstract = {Marine vertebrate fossils from late Cretaceous-early Paleogene shallow marine phosphorites of Morocco were investigated for their trace element compositions and neodymium isotopic ratios in order to constrain marine and depositional conditions. The various analyzed fossils are separated into two groups with different geochemical compositions: (1) shark tooth enameloid with generally lower Cu, Ba, rare earth elements (REEs) and U, and higher Na, Zn and Sr concentrations than (2) dentine, bone, and coprolites. These differences are related to the originally different structures of these fossils. All the fossils revealed very similar shale-normalized REE patterns, with negative Ce anomaly and heavy REE enrichment mimicking the REE pattern of modern oxic-seawater. The results therefore suggest REE uptake by the fossils from an early diagenetic pore fluid that was dominated by seawater. Importantly, the Ce anomaly does not vary among the different types of fossil remains and the values are very similar in a given layer. Moreover, a step-wise shift towards lower Ce/Ce* values from older to younger beds is apparent. Nd isotope analyses across the phosphorite succession yielded minor variation with an average εNd(t) value of -6.2±0.4 (n=12) indicating no major changes in the REE source during the studied interval. The relatively radiogenic values reflect Tethyan connection and/or important contribution of a mafic Nd source from weathering in the region. The age-related trend in the Ce anomaly is interpreted to be due to changes in redox and/or pH conditions of the upwelling seawater on the shallow shelf areas. The driving force of these changes was probably an extended global oceanic circulation, especially enhanced connection and water exchange between the North and South Atlantic. © 2015 Elsevier B.V.},
	keywords = {Seawater; Vertebrata; ISOTOPES; Trace Elements; Uranium; Atlantic Ocean; Tethys; Cretaceous; Rare earth elements; Geochemistry; Paleogene; tooth; Strontium; cerium; marine sediment; fossil record; Rare earths; Phosphate minerals; shark; Chondrichthyes; rare earth element; paleoceanography; ATLANTIC; Exploratory geochemistry; MOROCCO; phosphorite; Ce anomalies; Phosphate deposits; Shark teeth; Ce anomaly},
	year = {2016},
	eissn = {1872-6836},
	pages = {44-54}
}

@inproceedings{MTMT:2906290,
	title = {Neogene stratigraphy in the Mecsek region. Hetvehely, Badenian rocky shore and fossiliferous shorface sand},
	url = {https://m2.mtmt.hu/api/publication/2906290},
	author = {Sebe, Krisztina and Csillag, Gábor and Dulai, Alfréd and Gasparik, Mihály and Magyar, Imre and Selmeczi, Ildikó and Szabó, Márton and Sztanó, Orsolya and Szuromi-Korecz, A},
	booktitle = {Neogene of the Paratethyan Region: 6th Workshop on the Neogene of Central and South-Eastern Europe. An RCMNS Interim Colloquium},
	unique-id = {2906290},
	year = {2015},
	pages = {102-124},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Sztanó, Orsolya/0000-0003-0786-3653}
}

@CONFERENCE{MTMT:3189500,
	title = {Kovácsszénájai-tó. Középső-miocén, badeni Pécsszabolcsi Mészkő Formáció, szarmata Kozárdi Mészkő Formáció.},
	url = {https://m2.mtmt.hu/api/publication/3189500},
	author = {Konrád, Gy and Dulai, Alfréd},
	booktitle = {16. Magyar Őslénytani Vándorgyűlés, Orfű},
	unique-id = {3189500},
	year = {2013},
	pages = {50-52}
}

@article{MTMT:3189093,
	title = {Protracted diagenetic alteration of REE contents in fossil bioapatites: Direct evidence from Lu-Hf isotope systematics},
	url = {https://m2.mtmt.hu/api/publication/3189093},
	author = {Kocsis, László and Trueman, CN and Palmer, MR},
	doi = {10.1016/j.gca.2010.08.007},
	journal-iso = {GEOCHIM COSMOCHIM AC},
	journal = {GEOCHIMICA ET COSMOCHIMICA ACTA},
	volume = {74},
	unique-id = {3189093},
	issn = {0016-7037},
	abstract = {Fossil bones and teeth are potentially important repository for geochemical proxy data and a target for radiometric dating. The concentration of many trace elements in bones and teeth increases by orders of magnitude after death and it is this diagenetic incorporation that forms the basis for several areas of geochemical study. The use of bones and teeth in this context relies on two assumptions: first, that target metal ions are incorporated rapidly after death, reflecting a known environmental signal, and second, that after early incorporation, the bone or tooth remains as an essentially closed system, resistant to later diagenetic change. A wide literature has developed exploring these assumptions, but relatively little direct evidence has been used to assess the long-term diagenetic stability of trace elements within bones and teeth. In this study, we use the Lu-Hf isotope system to show that bones and teeth of Cretaceous and Triassic age from both terrestrial and marine settings experience continued, long-term diagenetic change, most likely through gradual addition of trace elements. Modelling suggests that diagenetic addition after initial recrystallisation may account for >50% of the total REE content in the sampled bones, the extent depending on initial uptake conditions. Tooth enamel and enameloid may be more resistant to late diagenetic changes, but dentine is probably altered to the same extent as bone. These results have significant implications for the use of bones and teeth as hosts of chronological, palaeoceanographic, palaeoenvironmental and taphonomic information, particularly in Mesozoic and Palaeozoic contexts. © 2010 Elsevier Ltd.},
	keywords = {trace element; Bone; Cretaceous; tooth; Isotopic composition; apatite; Lutetium; fossil; Triassic; Hafnium; rare earth element; diagenesis},
	year = {2010},
	eissn = {1872-9533},
	pages = {6077-6092}
}

@article{MTMT:151966,
	title = {Geochemical study of vertebrate fossils from the Upper Cretaceous (Santonian) Csehbánya Formation (Hungary): Evidence for a freshwater habitat of mosasaurs and pycnodont fish},
	url = {https://m2.mtmt.hu/api/publication/151966},
	author = {Kocsis, László and Ősi, Attila and Vennemann, T and Trueman, CN and Palmer, MR},
	doi = {10.1016/j.palaeo.2009.07.009},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {280},
	unique-id = {151966},
	issn = {0031-0182},
	year = {2009},
	eissn = {1872-616X},
	pages = {532-542},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:1368433,
	title = {Badenian evolution of the Central Paratethys Sea: paleogeography, climate and eustatic sea-level changes},
	url = {https://m2.mtmt.hu/api/publication/1368433},
	author = {Kovac, M and Andreyeva-Grigorovich, A and Bajraktarevic, Z and Brzobohaty, R and Filipescu, S and Fodor, László and Harzhauser, M and Nagymarosy, András and Oszczypko, N and Pavelic, D and Rogl, F and Saftic, B and Sliva, L and Studencka, B},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {58},
	unique-id = {1368433},
	issn = {1335-0552},
	abstract = {The Miocene Central Paratethys Sea covered wide areas of the Pannonian Basin System, bordered by the mountain chains of the Alps, Carpathians and Dinarides. The epicontinental sea spread not only in the back-arc basin area, but flooded even the Alpine-Carpathian Foredeep, situated along the front of gradually uplifting mountains. The Early Badenian (early Langhian) transgressions from the Mediterranean toward the Central Paratethys realm, via Slovenia and northern Croatia (Transtethyan Trench Corridor or Trans Dinaride Corridor) flooded the Pannonian Basin and continued along straits in the Carpathian Chain into the Carpathian Foredeep. The isolation of eastern parts of the Central Paratethys at the end of this period (late Langhian) resulted in the “Middle Badenian” salinity crisis. Thick evaporite sediments, above all halite and gypsum were deposited in the Transcarpathian Basin, Transylvanian Basin and Carpathian Foredeep. During the Late Badenian (early Serravallian), the latest full marine flooding covered the whole back-arc basin and a great part of the foredeep. The main problem is to create a model of sea connections during that time, because some authors consider the western Transtethyan Trench Corridor (Trans Dinaride Corridor) closed and there is no evidence to prove a supposed strait towards the Eastern Mediterranean. A proposed possibility is a connection towards the Konkian Sea of the Eastern Paratethys. The Badenian climate of the Central Paratethys realm can be characterized as fairly uniform, reflecting the stable subtropical conditions of the Miocene Climatic Optimum. No considerable changes in terrestrial ecosystems were documented. Nevertheless, evolution of steep landscape associated with rapid uplift of the East Alpine and Western Carpathian mountain chains (including high stratovolcanoes) caused development of vertical zonation of dry land and consequently close occurrence of different vegetation zones in a relatively small distance during this time. In the Central Paratethys Sea a slight N-S climatic gradient seems to be expressed already from the Early Badenian, but a biogeographic differentiation between basins in the North and South starts to become more prominent first during the Late Badenian, when a moderate cooling of the seawater can also be documented. The Late Badenian sea-level highstand coincides with the appearance of stress factors such as stratification of the water column and hypoxic conditions at the basin bottom in the whole area. Taking into account all bioevents and changes of paleogeography in the Central Paratethys realm, we can very roughly correlate the Early (and “Middle”) Badenian with the eustatic sea-level changes of TB 2.3, TB 2.4 or Bur5/Lan1, Lan2/Ser1 and the Late Badenian with TB 2.5 or Ser2 cycles (sensu Haq et al. 1988; Hardenbol et al. 1998). Generally, we can assign the Early Badenian transgressions to be controlled by both, tectonics (induced mainly by back-arc basin rifting) and eustacy, followed by forced regression. The Late Badenian transgression and regression were dominantly controlled by sea-level changes inside the Central Paratethys realm.},
	keywords = {climate; Pannonian Basin; Miocene; Tectonics; Western Carpathians; Badenian; Middle Miocene; Sequence stratigraphy; Sequence stratigraphy; paleogeography; STRUCTURAL EVOLUTION; CENTRAL PARATETHYS; TRANSYLVANIAN BASIN ROMANIA; GRUND FORMATION; FORMATION MOLASSE BASIN; NORTHERN CARPATHIAN FOREDEEP; CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY},
	year = {2007},
	eissn = {1336-8052},
	pages = {579-606},
	orcid-numbers = {Fodor, László/0000-0002-0606-4414}
}

@article{MTMT:1763182,
	title = {Badenian (Middle Miocene) basin development in SW Hungary: subsidence history based on quantitative paleobathymetry of foraminifera},
	url = {https://m2.mtmt.hu/api/publication/1763182},
	author = {Báldi, Katalin and Benkovics, L and Sztanó, Orsolya},
	doi = {10.1007/s005310100226},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {91},
	unique-id = {1763182},
	issn = {1437-3254},
	abstract = {A quantitative paleobathymetric study of Badenian foraminifera was carried out from Tekeres-1 and Tengelic-2 boreholes, north of the Mecsek Mts., SW Hungary. Paleobathymetric data, based on plankton/benthos ratio provided input for the analysis of the subsidence history. The biostratigraphic framework is mainly provided by calcareous nannoplankton (zones NN5-NN7). Changes in sedimentation rates are also considered, partly calculated from number of benthos per unit sediment, and partly estimated from the changes of lithofacies. Relative sea-level changes are calculated from changes of paleowater depth and coeval sedimentary thickness. The result is examined as the sum of accommodation space created by subsidence and eustasy. In that period of time eustatic changes were about an order of magnitude smaller than changes created by movements of the basin floor. According to our model in early Badenian (up to the half of NN5 nannozone) a very rapid transtension-related subsidence of about 500 m occurred. This was interrupted by a short period of uplift of minor magnitude at about the first third of NN5 zone; thereafter, subsidence continued and the basin floor reached its deepest position. Still within the NN5 nannozone (Early Badenian) a significant uplift occurred, terminating the life of the deep basin. The Late Badenian (NN6) is characterized by a relatively small rate of subsidence and presumably quiet tectonism. During this period bathymetric changes are thought to be controlled primarily by eustatic changes. The first uplift - only interrupting subsidence - is regarded as the result of the change of the local stress field because of convergence along the curvature of strike slip faults. The second uplift, which stopped the subsidence of the basin floor is thought to be of a regional character and is attributed to the compression generated between Tisza and Alcapa tectonic units.},
	keywords = {MODEL; foraminifera; Pannonian Basin; Badenian; paleobathymetry; basin analysis},
	year = {2002},
	eissn = {1437-3262},
	pages = {490-504},
	orcid-numbers = {Báldi, Katalin/0000-0002-9154-2045; Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:1890263,
	title = {Paleogeographic evolution of the Late Miocene Lake Pannon in Central Europe},
	url = {https://m2.mtmt.hu/api/publication/1890263},
	author = {Magyar, Imre and Geary, DH and Muller, P},
	doi = {10.1016/S0031-0182(98)00155-2},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {147},
	unique-id = {1890263},
	issn = {0031-0182},
	abstract = {The paleogeographic evolution of Lake Pannon within the Pannonian basin is reconstructed with eight maps, ranging from the Middle Miocene to the Early Pliocene. The maps are based on the distribution of selected biozones and specific fossils, and on complementary sedimentological and seismic information. Our reconstruction shows that the history of Lake Pannon can be divided into three distinct intervals: an initial stage with low water level, which resulted in isolation from the sea at about 12 Ma and might have led to temporary fragmentation of the lake; an interval of gradual transgression lasting until ca. 9.5 Ma; and a long late interval of shrinkage and infilling of sediments that persisted into the Early Pliocene. The deep subbasins of the lake formed during the transgressive interval, in more basinward locations than the deep basins of the preceding Sarmatian age. The southern shoreline, running parallel with the Sava and Danube rivers along the northern foot of the Dinarides, changed very Little during the Lifetime of the lake, while the northern shoreline underwent profound changes. (C) 1999 Elsevier Science B.V. All rights reserved.},
	keywords = {BASIN; Pannonian Basin; Neogene; Lakes; paleogeography; Paratethys; biogeography},
	year = {1999},
	eissn = {1872-616X},
	pages = {151-167}
}