@article{MTMT:34745482,
	title = {A global compilation of diatom silica oxygen isotope records from lake sediment - trends and implications for climate reconstruction},
	url = {https://m2.mtmt.hu/api/publication/34745482},
	author = {Meister, P. and Alexandre, A. and Bailey, H. and Barker, P. and Biskaborn, B.K. and Broadman, E. and Cartier, R. and Chapligin, B. and Couapel, M. and Dean, J.R. and Diekmann, B. and Harding, P. and Henderson, A.C.G. and Hernandez, A. and Herzschuh, U. and Kostrova, S.S. and Lacey, J. and Leng, M.J. and Lücke, A. and MacKay, A.W. and Magyari, Enikő Katalin and Narancic, B. and Porchier, C. and Rosqvist, G. and Shemesh, A. and Sonzogni, C. and Swann, G.E.A. and Sylvestre, F. and Meyer, H.},
	doi = {10.5194/cp-20-363-2024},
	journal-iso = {CLIM PAST},
	journal = {CLIMATE OF THE PAST},
	volume = {20},
	unique-id = {34745482},
	issn = {1814-9324},
	year = {2024},
	eissn = {1814-9332},
	pages = {363-392},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937}
}

@article{MTMT:34189703,
	title = {Ferussina petofiana sp. n. (Gastropoda, Caenogastropoda, Cyclophoridae), the oldest representative of its subfamily from the Late Cretaceous of Romania},
	url = {https://m2.mtmt.hu/api/publication/34189703},
	author = {Páll-Gergely, Barna and Magyar, János and Csiki-Sava, Zoltán and Botfalvai, Gábor},
	doi = {10.17109/AZH.69.4.337.2023},
	journal-iso = {ACTA ZOOLOG ACAD SCI HUNG},
	journal = {ACTA ZOOLOGICA ACADEMIAE SCIENTIARUM HUNGARICAE},
	volume = {69},
	unique-id = {34189703},
	issn = {1217-8837},
	abstract = {The terrestrial gastropod Ferussina petofiana Páll-Gergely sp. n. is described from uppermost Cretaceous (Maastrichtian) deposits from the Haţeg Basin, Romania. It represents the first properly diagnosed and described snail taxon from these deposits, despite numerous earlier reports of gastropod occurrences. This new species is characterized by a depressed, mostly smooth shell, three spiral carinae on the ventral side (inside the umbilicus), and an upward-turning aperture. The last feature characterizes two European fossil snail genera, the cyclophoroidean Ferussina, and the stylommatophoran Strophostomella. The new species is classified in the former group due to its nearly circular aperture, and the presence of conspicuous spiral carinae. In contrast, the aperture of most stylommatophoran genera (including Strophostomella) is semilunar, and if raised sculptural elements are present, they are mostly radially oriented. The identification of this new taxon in the uppermost Cretaceous of Romania represents an important range extension for the genus Ferussina, and adds it to the brief list of European clades that appear to have survived the mass extinction event at the Cretaceous-Paleogene boundary.},
	year = {2023},
	eissn = {2064-2474},
	pages = {337-352},
	orcid-numbers = {Páll-Gergely, Barna/0000-0002-6167-7221; Botfalvai, Gábor/0000-0002-5479-9036}
}

@{MTMT:34139745,
	title = {Stand scale palynology helps to reveal the role of forest exploitation and climate change in the current distribution of Fagus sylvatica in the NE Pannonian Basin (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/34139745},
	author = {Ofosu-Brakoh, Abigail Amponsaah and Réka, Csorba R. and Bede-Fazekas, Ákos and Standovár, Tibor and Pató, Zsuzsanna Anna and Magyari, Enikő Katalin},
	booktitle = {Natural Hazards and Climate Change - conference and workshop for identifying and tackling challenges together},
	unique-id = {34139745},
	year = {2023},
	pages = {18},
	orcid-numbers = {Bede-Fazekas, Ákos/0000-0002-2905-338X; Standovár, Tibor/0000-0002-4686-3456; Pató, Zsuzsanna Anna/0000-0003-2135-824X; Magyari, Enikő Katalin/0000-0002-2844-8937}
}

@article{MTMT:34112863,
	title = {Geochemical investigation of the mixed Máriahalom vertebrate fauna at the Paleogene–Neogene boundary in the Central Paratethys: environmental conditions and age constrain},
	url = {https://m2.mtmt.hu/api/publication/34112863},
	author = {Kocsis, László and Rabi, Márton and Ulianov, Alex and Cipriani, Anna and Farkas, Izabella M. and Botfalvai, Gábor},
	doi = {10.1186/s13358-023-00281-7},
	journal-iso = {SWISS J PALAEON},
	journal = {SWISS JOURNAL OF PALAEONTOLOGY},
	volume = {142},
	unique-id = {34112863},
	issn = {1664-2376},
	abstract = {The fossil vertebrate fauna of Máriahalom contains remains from a wide range of ecologies including terrestrial and aquatic mammals, crocodiles, sharks, and rays among others. All these were found mixed in mollusc-rich, shallow water, coastal deposits. The aim of the study is to trace the origin of the fossils using their rare earth element (REE) content and their respective ecology with stable oxygen isotopic compositions. In addition, marine vertebrates and calcareous marine fossils were analysed for their Sr isotope composition to provide a new age estimate for the locality. The REE content and their distribution in the fossils indicate similar early diagenetic environments and possible contemporaneous fossilization for the entire vertebrate assemblage. Reworked fossils of significantly different age can be excluded. The enamel/enameloid-derived phosphate oxygen isotope composition of selected fossil taxa fit well with previously inferred habitats that include marine, brackish, and terrestrial environments. Notably, the stem-pinniped Potamotherium valletoni is best interpreted as freshwater dweller instead of marine, consistent with the sedimentology of other occurrences. Our novel 87 Sr/ 86 Sr data suggest an Aquitanian age (21.4 ± 0.5 Ma) for the Máriahalom site that is younger than the previously proposed Late Oligocene age based on biostratigraphy (MP28–30 European Mammal Paleogene Reference Levels). An Aquitanian age raises the possibility that the index fossil taxon, the anthracothere mammal Microbunodon minimum , may have vanished earlier in Western Europe than in the Central Paratethys region.},
	year = {2023},
	eissn = {1664-2384},
	orcid-numbers = {Kocsis, László/0000-0003-4613-1850; Botfalvai, Gábor/0000-0002-5479-9036}
}

@article{MTMT:34105792,
	title = {Erdő- és fahatár változás a Déli-Kárpátokban a késő glaciális és kora holocén gyors felmelegedési hullámai idején: korai erdőexpanzió és a fiatal driász lehűlés csillapított hatása},
	url = {https://m2.mtmt.hu/api/publication/34105792},
	author = {Darabos, Gabriella and Magyari, Enikő Katalin and Szabó, Zoltán and Lisztes-Szabó, Zsuzsa and Veres, D and Haliuc, A and Reitmeyer, B and Pálfi, Ivett},
	doi = {10.23928/foldt.kozl.2023.153.2.143},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {153},
	unique-id = {34105792},
	issn = {0015-542X},
	abstract = {A Páreng-hegységcsoportban (Munții Parâng, Déli-Kárpátok) lévő magashegyi tó (Latorica-tó, Iezerul Latorița, 1530 m) üledékének késő glaciális és kora holocén korú szakaszán növényi makrofosszília és pollen analitikai elemzéseket végeztünk, hogy megállapítsuk a fahatár, az erdőhatár és a szubalpi vegetáció éghajlatváltozásra adott válaszreakcióit. A Latorica-tó vízgyűjtőjén és partján 15 510–14 765 kal. BP évek (Grönlandi 2-es oxigénizotóp fázis (GS-2) vége) között a gleccserek visszahúzódása nyomán nem volt, vagy csak ritka növényborítás lehetett, tehát a fahatár valószínűleg a tó alatt húzódott. Az ezt követő GI-1 fázisban (kormodellünk alapján 14 765–13 340 kal. BP évek között) bekövetkező felmelegedés hatására a tó körül kialakuló fahatár ökoton zónában törpefenyő, lucfenyő és szálanként vörösfenyő (Pinus mugo–Picea abies–Larix decidua) keveredésével jellemezhető, boreális nyílt erdő expanzióját rekonstruáltuk. A fahatár fokozatosan magasabbra húzódott, majd a GI-1 végén (13 340–12 930 kal BP évek közt) nagy intenzitású erdőtűz következhetett be a tó körül, annak vízgyűjtőjére is kiterjedve. A fiatal driász lehűlés a jelenlegi kormodell szerint 12 930 és 11 995 kal. BP évek között a tó szerves anyag produkciójának csökkenéséhez vezetett, ugyanakkor a lehűlés csak kis mértékben hatott a tó menti vegetációra. A legjelentősebb változás a havasi cirbolyafenyő (Pinus cembra) megjelenése és előretörése volt ebben az időszakban. A kora holocénben (11 995–11 300 kal. BP évek közt) a fa- és erdőhatár folyamatosan emelkedhetett, az erdőszerkezet zárult és tovább diverzifikálódott a molyhos nyír (Betula pubescens) megjelenésével: luc- (P. abies), vörösfenyő (L. decidua) és törpefenyő (P. mugo) alkotta nyílt, de a késő glaciálisnál zártabb erdők uralták a tó körüli tájat. Eredményeink alapján elmondhatjuk, hogy a késő glaciális erdőexpanzió gyorsasága közeli refúgiális populációkra utal a fenyőfélék esetében, valamint eredményeink megerősítik a Déli-Kárpátok Retyezát vonulatában kapott eredményeket, miszerint a fiatal driász lehűlés a vegetációs időszak hőösszegét csak kis mértékben csökkentette ebben a régióban (szemben Nyugat-Európával). Az éghajlatváltozás kompetíciós előnybe hozta a Déli-Kárpátok szubalpin zónájában a havasi cirbolyafenyőt (P. cembra), mely ekkor terjedt el a fahatár ökoton zónában. A kora holocén felmelegedés során a mainál kontinentálisabb klímán a vörösfenyő széles körben elterjedt a Déli-Kárpátokban a szubalpin zónában.},
	year = {2023},
	eissn = {2559-902X},
	pages = {143-163},
	orcid-numbers = {Darabos, Gabriella/0000-0001-8070-5630; Magyari, Enikő Katalin/0000-0002-2844-8937; Lisztes-Szabó, Zsuzsa/0000-0002-6322-8542; Veres, D/0000-0003-3932-577X; Haliuc, A/0000-0002-5681-8210; Pálfi, Ivett/0000-0001-9814-3410}
}

@article{MTMT:33786764,
	title = {Multi‐disciplinary study of a late Pleistocene woolly rhinoceros found in the Pannonian Basin and implications for the contemporaneous palaeoenvironment},
	url = {https://m2.mtmt.hu/api/publication/33786764},
	author = {Gasparik, Mihály and Major, István and Lisztes-Szabó, Zsuzsa and Magyari, Enikő Katalin and Szabó, Bence and Pandolfi, Luca and Borel, Antony and Futó, István and Horváth, Anikó and Kiss, Gabriella Ilona and Molnár, Mihály and Csík, Attila and Markó, András},
	doi = {10.1002/jqs.3533},
	journal-iso = {J QUATERNARY SCI},
	journal = {JOURNAL OF QUATERNARY SCIENCE},
	volume = {38},
	unique-id = {33786764},
	issn = {0267-8179},
	year = {2023},
	eissn = {1099-1417},
	pages = {1159-1170},
	orcid-numbers = {Major, István/0000-0003-4675-9875; Lisztes-Szabó, Zsuzsa/0000-0002-6322-8542; Magyari, Enikő Katalin/0000-0002-2844-8937; Csík, Attila/0000-0002-8173-9653; Markó, András/0000-0002-7556-0091}
}

@{MTMT:33746513,
	title = {Őskörnyezeti változások a Csomád-hegycsoportban az utolsó glaciálisban},
	url = {https://m2.mtmt.hu/api/publication/33746513},
	author = {Magyari, Enikő Katalin and Vincze, Ildikó and Tóth, Mónika and Hubay, Katalin and Daniel, Veres and Aritina, Hialiuc and Molnár, Mihály and Jakab, Gusztáv and Braun, Mihály and Frank, Schabitz and Máthé, István and Buczkó, Krisztina},
	booktitle = {A Kárpátok legfiatalabb tűzhányója, a Csomád. Vulkánosság, őskörnyezet, ember és táj.},
	unique-id = {33746513},
	year = {2023},
	pages = {143-156},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Jakab, Gusztáv/0000-0002-2569-5967}
}

@article{MTMT:32087364,
	title = {Social Context of Late Medieval and Early Modern Deforestation Periods in the Apuseni Mountains (Romania) based on an Integrated Evaluation of Historical and Paleobotanical Records},
	url = {https://m2.mtmt.hu/api/publication/32087364},
	author = {Jakab, Gusztáv and Pál, Ilona and Silye, Lóránd and Sümegi, Pál and Tóth, A and Sümegi, B and Frink, József Pál and Magyari, Enikő Katalin and Kern, Zoltán and Benkő, Elek},
	doi = {10.1080/14614103.2021.1942744},
	journal-iso = {ENVIRON ARCHAEOL},
	journal = {ENVIRONMENTAL ARCHAEOLOGY},
	volume = {28},
	unique-id = {32087364},
	issn = {1461-4103},
	year = {2023},
	eissn = {1749-6314},
	pages = {345-366},
	orcid-numbers = {Jakab, Gusztáv/0000-0002-2569-5967; Silye, Lóránd/0000-0001-7306-6041; Sümegi, Pál/0000-0003-1755-4440; Magyari, Enikő Katalin/0000-0002-2844-8937; Kern, Zoltán/0000-0003-4900-2587}
}

@CONFERENCE{MTMT:33709032,
	title = {Use of diatoms for disentangling of climate and tectonic forcing in the development of the last volcanic lake of Carpathians during the Last Glacial Maximum and deglaciation (Lake St. Anne, Romania)},
	url = {https://m2.mtmt.hu/api/publication/33709032},
	author = {Buczkó, Krisztina and Korponai, János and Veres, D. and Karátson, Dávid and Magyari, Enikő Katalin},
	booktitle = {Lagos, Memorias del Territorio},
	unique-id = {33709032},
	year = {2022},
	pages = {108-108},
	orcid-numbers = {Korponai, János/0000-0003-0211-192X; Karátson, Dávid/0000-0003-0386-1239; Magyari, Enikő Katalin/0000-0002-2844-8937}
}

@article{MTMT:33623827,
	title = {First record of Gomphonema lacunicola Patrick et Freese (Bacillariophyta) from the Pâreng Mts (Southern Carpathians, Romania)},
	url = {https://m2.mtmt.hu/api/publication/33623827},
	author = {Buczkó, Krisztina and Kövér, Csilla and Magyari, Enikő Katalin and Szabó, Zoltán and Korponai, János},
	doi = {10.17110/StudBot.2022.53.1.51},
	journal-iso = {STUD BOT HUNG},
	journal = {STUDIA BOTANICA HUNGARICA},
	volume = {53},
	unique-id = {33623827},
	issn = {0301-7001},
	abstract = {Here we report and document the occurrence of the diatom Gomphonema lacunicola Patrick et Freese 1961 from the Pâreng Mts of the Carpathian Mountains, Romania. This observation was made within the framework of a systematic sampling campaign and analyses that were conducted in the Southern Carpathians, covering 40 mountain lakes for discovering the cladoceran fauna and diatom flora of this region between 2012 and 2014. G. lacunicola was found only in one of the 40 lakes, namely in Lake Câlcescu, where it was extremely rare, but the characteristic feature of the lake promoted the presence of the species. Lake Câlcescu is a subalpine lake, located 1,934 m a.s.l. This is the first record of this diatom species in Romania.},
	keywords = {Carpathian Mountains; Romania; Gomphonema; diatom taxonomy; Cryptic project; Pâreng Mts},
	year = {2022},
	pages = {51-58},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Korponai, János/0000-0003-0211-192X}
}