@article{MTMT:32753540,
	title = {Preliminarily report on rare earth element taphonomy of a Miocene mixed age fossil vertebrate assemblage (Pécs-Danitzpuszta, Mecsek Mts., Hungary): uptake mechanism and possible separation of palaeocommunities},
	url = {https://m2.mtmt.hu/api/publication/32753540},
	author = {Botfalvai, Gábor and Kocsis, László and Szabó, Márton and Király, Edit and Sebe, Krisztina},
	doi = {10.1080/08912963.2022.2049771},
	journal-iso = {HIST BIOL},
	journal = {HISTORICAL BIOLOGY},
	volume = {35},
	unique-id = {32753540},
	issn = {0891-2963},
	year = {2023},
	eissn = {1029-2381},
	pages = {498-517},
	orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036; Kocsis, László/0000-0003-4613-1850; Sebe, Krisztina/0000-0002-4647-2199}
}

@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: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:30759402,
	title = {Thermophilous elements from the late Miocene flora of Pécs-Danitzpuszta (Mecsek Mts, Hungary) – confimed by cuticular analysis},
	url = {https://m2.mtmt.hu/api/publication/30759402},
	author = {Hably, Lilla and Erdei, Boglárka and Sebe, Krisztina},
	doi = {10.17110/StudBot.2019.50.1.9},
	journal-iso = {STUD BOT HUNG},
	journal = {STUDIA BOTANICA HUNGARICA},
	volume = {50},
	unique-id = {30759402},
	issn = {0301-7001},
	abstract = {The late Miocene (Pannonian) flora of Pécs-Danitzpuszta was first studied and published by Hably & Sebe (2016). Recent collections, however, revealed additional foliage remains, some also providing epidermal details. A well-preserved leaf fragment assigned to Laurophyllum based on its micromorphology proves the presence of Lauraceae. A frequent element of European Miocene floras, Laurophyllum pseudoprinceps, is first described from the late Miocene (Pannonian) of Hungary. In addition, a leafl et of Engelhardia orsbergensis is also first reported as a thermophilous element in the Hungarian late Miocene.},
	keywords = {Pannonian Basin; LATE MIOCENE; cuticle; fossil flora and vegetation},
	year = {2019},
	pages = {9-17},
	orcid-numbers = {Erdei, Boglárka/0000-0001-5144-6246; Sebe, Krisztina/0000-0002-4647-2199}
}

@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:3273189,
	title = {The Central Paratethys palaeoceanography: a water circulation model based on microfossil proxies, climate, and changes of depositional environment},
	url = {https://m2.mtmt.hu/api/publication/3273189},
	author = {Kováč, M and Hudáčková, N and Halásová, E and Kováčová, M and Holcová, K and Oszczypko-Clowes, M and Báldi, Katalin and Less, György and Nagymarosy, A and Ruman, A and Klučiar, T and Jamrich, M},
	journal-iso = {ACTA GEOL SLOV},
	journal = {ACTA GEOLOGICA SLOVACA},
	volume = {9},
	unique-id = {3273189},
	issn = {1338-0044},
	year = {2017},
	eissn = {1338-5674},
	pages = {75-114},
	orcid-numbers = {Báldi, Katalin/0000-0002-9154-2045}
}

@article{MTMT:3187838,
	title = {First report on vertebrate coprolites from the Upper Cretaceous (Santonian) Csehbánya Formation of Iharkút, Hungary},
	url = {https://m2.mtmt.hu/api/publication/3187838},
	author = {Segesdi, Martin and Botfalvai, Gábor and Bodor, Emese Réka and Ősi, Attila and Buczkó, Krisztina and Dallos, Zsolt and Tokai, Richárd and Földes, Tamás},
	doi = {10.1016/j.cretres.2017.02.010},
	journal-iso = {CRETACEOUS RES},
	journal = {CRETACEOUS RESEARCH},
	volume = {74},
	unique-id = {3187838},
	issn = {0195-6671},
	abstract = {Abstract More than 2600 coprolites produced by vertebrates have been found in the fluvial lacustrine beds of the Upper Cretaceous (Santonian) Csehbánya Formation, Iharkút, western Hungary. In this study the mineral components, embedded dietary residues of these coprolites were examined and their ecological significance are discussed. The coprolite assemblage, containing mostly small-sized (length between 0.8 and 8.6 cm) specimens, can be ordered into seven different morphotypes, among which the spiral ones might have been produced by fish with spiral intestinal valves. The surface of the coprolites is mostly smooth and desiccation cracks were observed in only one case, suggesting that most of these coprolites were buried in-situ without long-term subaerial exposure. The fine-grained matrix of coprolites contains small holes, partially digested plant and animal residues but no sedimentary particles. CT-scanning was an effective method for revealing embedded dietary residues despite that the coprolites contain a large amount of pyrite. The coprolites contain cuticle remains, coalified seeds, pollen grains and diatoms. Animal residues may be the evidence of predation: mollusk shell and bone fragments, ganoid scales of Lepisosteiformes fish were frequent and one Pycnodontiformes fish tooth was found as well. It is not possible to ascertain the real producer of the coprolites, but, according to these remains, the Lepisosteiformes and Pycnodontiformes fish were included in the producer's prey. Not only the bone- but also the plant-bearing coprolites are highly phosphatic with mineral apatite in their matrix. However, the embedding fluvial sediment has significantly different chemical composition. The high phosphatic content of coprolites and the apatite might be derived from the carnivorous diet. Plant remains in the phosphatic coprolites may imply an omnivore producer or were the result of their incidental ingestion. Rapid burial and the mineral content of the animal nutriment might have been the responsible factors for the good preservation of the excrements.},
	keywords = {EVOLUTION; Chemistry; Canada; ARCHITECTURE; ALBERTA; Bakony Mountains; TEETH; Partially digested animal inclusions; Carnivore coprolites; High phosphorous content; Plant and animal residues; Coprolites; NORTHWESTERN HUNGARY; DINOSAUR COPROLITES},
	year = {2017},
	eissn = {1095-998X},
	pages = {87-99},
	orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036; Bodor, Emese Réka/0000-0003-3894-2506; Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:3022749,
	title = {A late Miocene termophilous flora from Pécs-Danitzpuszta, Mecsek Mts., Hungary},
	url = {https://m2.mtmt.hu/api/publication/3022749},
	author = {Hably, Lilla and Sebe, Krisztina},
	doi = {10.1127/njgpa/2016/0554},
	journal-iso = {NEUES JAHRB GEOL P-A},
	journal = {NEUES JAHRBUCH FÜR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN},
	volume = {279},
	unique-id = {3022749},
	issn = {0077-7749},
	year = {2016},
	eissn = {2363-717X},
	pages = {261-271},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:3411946,
	title = {Dietary and environmental implications of Early Cretaceous predatory dinosaur coprolites from Teruel, Spain},
	url = {https://m2.mtmt.hu/api/publication/3411946},
	author = {Vajda, Violetta and Fernandez, MDP and Villanueva-Amadoz, U and Lehsten, V and Alcala, L},
	doi = {10.1016/j.palaeo.2016.02.036},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {464},
	unique-id = {3411946},
	issn = {0031-0182},
	abstract = {Coprolites from the Early Cretaceous vertebrate bone-bed at Arino in Teruel, Spain, were analyzed geochemically and palynologically. They contain various inclusions, such as small bone fragments, abundant plant remains, pollen, and spores. We attribute the coprolites to carnivorous dinosaurs based partly on their morphology together with the presence of bone fragments, and a high content of calcium phosphate (hydroxylapatite) with calcite. Well-preserved pollen and spore assemblages were identified in all coprolite samples and a slightly poorer assemblage was obtained from the adjacent sediments, both indicating an Early Cretaceous (Albian) age. This shows that the coprolites are in situ and also confirms previous age determinations for the host strata. The depositional environment is interpreted as a continental wetland based on the palynoflora, which includes several hydrophilic taxa, together with sparse occurrences of fresh-water algae, such as Ovoidites, and the absence of marine palynomorphs. Although the coprolites of Arino samples generally are dominated by pollen produced by Taxodiaceae (cypress) and Cheirolepidiaceae (a family of extinct conifers), the sediment samples have a slightly higher relative abundance of fern spores. The distribution of major organic components varies between the coprolite and sediment samples, which is manifest by the considerably higher charcoal percentage within the coprolites. The high quantities of charcoal might be explained by a ground-dwelling species, feeding on smaller vertebrates that complemented its diet with plant material from a paleoenvironment were wild fires were a part of the ecosystem. The state of preservation of the spores and pollen is also more detailed in the coprolites, suggesting that encasement in calcium phosphate may inhibit degradation of sporopollenin. (C) 2016 The Authors. Published by Elsevier B.V.},
	keywords = {POLLEN; PRESERVATION; Cretaceous; charcoal; DEPOSITS; records; palynology; USA; coprolite; EXCRETA; NORTHEASTERN; ESCUCHA FORMATION; RED COLOBUS MONKEYS; Wild fires; Teruel},
	year = {2016},
	eissn = {1872-616X},
	pages = {134-142}
}

@article{MTMT:2174694,
	title = {A legmagasabban fekvő mecseki pannon-tavi üledékek helyzete és kora},
	url = {https://m2.mtmt.hu/api/publication/2174694},
	author = {Sebe, Krisztina and Konrád, Gyula and Magyar, Imre},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {143},
	unique-id = {2174694},
	issn = {0015-542X},
	year = {2013},
	eissn = {2559-902X},
	pages = {67-72},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1354802,
	title = {Fiatal tektonikai jelenségek új észlelései a Nyugati-Mecsekben és környezetében},
	url = {https://m2.mtmt.hu/api/publication/1354802},
	author = {Konrád, Gyula and Sebe, Krisztina},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1354802},
	issn = {0015-542X},
	abstract = {Exposures of Neogene and Quaternary age were investigated along the main structural zones of the Western Mecsek
		Mts. (SW Hungary) in order to study post-Miocene tectonic activity, with an aim of supplementing studies on the longterm
		stability of the region. Field observations showed that young movements affected only the mountain fronts and the
		foreland. From the 24 studied exposures, those with impacts of tectonic activity were located along the major fault zones
		of the Western Mecsek Mts. and prove tectonic/seismic events occurring as late as the Late Pleistocene along the
		Mecsekalja Dislocation Zone and probably the Hetvehely–Magyarszék Fault. On the contrary, no impact of neotectonic
		activity was found within the Western Mecsek Anticline, indicating that this area behaved as a single solid block during
		post-Miocene movements. Since the Karpatian age, 5 tectonic phases could be distinguished. From these – somewhat
		opposing previous research – transtension seems typical for the Karpatian along the Hetvehely–Magyarszék Fault. The
		Early Pannonian transtensional stress field did not cease to exist at the beginning of the Late Pannonian. Tectonic
		inversion started only within the first half of the Late Pannonian and can be considered active up to present day in the
		major part of the area.
		
		A munka során a Nyugat-Mecsek fő szerkezeti vonalainak környezetében feltárt neogén és kvarter képződményeket
		vizsgáltuk fiatal (posztpannóniai) tektonikai aktivitás nyomai után kutatva, elsősorban a terület hosszú távú
		stabilitásának megítéléséhez. A terepi megfigyelések alapján a fiatal mozgások csak a hegységperemet és az előteret
		érintették. A vizsgált 24 feltárásból a fiatal tektonikával érintettek a Nyugat-Mecsek meghatározó szerkezeti vonalai
		mentén helyezkednek el, és még a késő-pleisztocénben is szerkezeti mozgásokat, illetve szeizmikus aktivitást
		bizonyítanak a Mecsekalja-öv és valószínűleg a Hetvehely–magyarszéki-törés mentén. Ezzel ellentétben a Nyugatmecseki-
		antiklinális területén belül neotektonikára utaló jeleket nem észleltünk, ez alapján a pannóniai–negyedidőszaki
		mozgások során a Nyugat-Mecsek egységes tömbként viselkedhetett.
		A kárpáti korszak óta öt tektonikai fázis volt elkülöníthető a területen. Ezek közül – a korábbi vizsgálati
		eredményekkel szemben – a kárpáti korszakra jellemzőnek tűnik a transztenzió a Hetvehely–magyarszéki-törés
		mentén. A kora-pannóniai transztenziós feszültségtér a Mecsekalja-öv mentén még a késő-pannóniai elején is
		fennállt. Az inverzió a késő-pannóniai első felében kezdődött és a terület legnagyobb részén máig aktívnak
		tekinthető.},
	year = {2010},
	eissn = {2559-902X},
	pages = {135-161},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1782867,
	title = {Neogene flora and vegetation development of the Pannonian domain in relation to palaeoclimate and palaeogeography},
	url = {https://m2.mtmt.hu/api/publication/1782867},
	author = {Erdei, Boglárka and Hably, Lilla and Kázmér, Miklós and Utescher, T and Bruch, AA},
	doi = {10.1016/j.palaeo.2007.03.036},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {253},
	unique-id = {1782867},
	issn = {0031-0182},
	abstract = {A survey of the Neogene flora and vegetation pattern of the Pannonian domain based on selected fossil plant assemblages is given. The paper aims to reveal the complex interrelation of tectonic-palaeogeographic evolution, climate, flora and vegetation development through the Neogene of the Pannonian domain. Flora and vegetation patterns are based on well-documented and studied fossil plant assemblages (macrofloras, primarily leaves). There are time intervals well-represented in the fossil record, e.g. the Pannonian or the Sarmatian and others with relatively few localities, e.g. the Badenian. A general but slow cooling trend is definitely observable after the Early Miocene as reflected by both quantitative climate reconstructions and floristic change, i.e. decrease of diversity, slow disappearance of thermophilous and exotic elements, as well as decrease in the variety of vegetation types. A significant decline of coldest month temperatures (as compared to warmest month temperatures) must have played a defining role in forming flora and vegetation through the Neogene. As compared to climate estimates for the Middle/Late Miocene fossil floras, warmer climate conditions are indicated by the Ipolytarnoc flora and vegetation comprising an extremely high number of thermophilous taxa as well as complex vegetation structure. The Early and Middle Miocene fossil assemblages bear a significant relevance to the tectonic pattern of the Pannonian domain. A transitional character in both flora and vegetation is indicated by the Karpatian Magyaregregy locality. Knowledge of the Badenian flora and vegetation is limited to the Middle Badenian Nogradszakal assemblage indicating cooler climate conditions which contrasts with global climate change. In contrast to the relatively poor azonal vegetation of Nogradszakal and most Pannonian localities, the more diverse Sarmatian and Pliocene floras display a strong relation to each other - attributable to palaeogeographic constraints. (C) 2007 Elsevier B.V. All rights reserved.},
	keywords = {EVOLUTION; RECONSTRUCTION; Hungary; Germany; Neogene; Miocene; Tectonics; Tertiary; FORESTS; palaeogeography; MA; CENTRAL PARATETHYS; Pannonian domain; palaeoclimate; fossil flora and vegetation},
	year = {2007},
	eissn = {1872-616X},
	pages = {115-140},
	orcid-numbers = {Erdei, Boglárka/0000-0001-5144-6246; Kázmér, Miklós/0000-0003-1092-1316}
}

@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}
}