@article{MTMT:33859682,
	title = {Clasts derived from rhizocretions in shallow-marine Miocene clastic deposits of northern Hungary: an example of zombie biogenic structures},
	url = {https://m2.mtmt.hu/api/publication/33859682},
	author = {Uchman, Alfred and Dávid, Árpád and Fodor, Rozália},
	doi = {10.7306/gq.1674},
	journal-iso = {GEOL Q},
	journal = {GEOLOGICAL QUARTERLY},
	volume = {67},
	unique-id = {33859682},
	issn = {1641-7291},
	abstract = {Disc-and cy lin dri cal-shaped clasts of fine grained cal car e ous and ferruginous rock, each with a cen tral tun nel, oc cur in shallow ma rine brack ish Mio cene sandy de pos its of the Egyhazasgerge For ma tion in Hun gary. Pre vi ously, these have been in terpreted as enigmatic biogenic (?) structures. After field and laboratory examination and comparisons with sub-recent rhizoclasts in sub soils de vel oped on Qua ter nary fine-grained de pos its in SE Po land, they are re-in ter preted as re de pos ited rhizocretions pos si bly washed out of the co eval con ti nen tal de pos its of the Salgo tarjan Lig nite For ma tion. Most are fragmented and abraded. They are termed rhizoclasts and are pre sented as an ex am ple of zom bie struc tures in her ited from an other en vi ron ment where they played a dif fer ent role. Such rhizoclasts can be con sid ered as an in di ca tor of the source of the clastic ma te rial trans ported from a veg e tated land mass on which mod er ate or poorly drained soils de velop and plant roots pen e trate the fine-grained sub strate. In such soils, iron was mo bi lized, then fixed by ox i da tion, as the wa ter ta ble and ox y gen levels fluctuated.},
	keywords = {Neogene; CONCRETIONS; Palaeosols; redeposition; rhizocretions; clastic deposits},
	year = {2023},
	eissn = {2082-5099}
}

@{MTMT:33351972,
	title = {Rovarok életnyomai késő-oligocén (Egri) korú növénymaradványokon (Wind-féle téglagyár, Eger)},
	url = {https://m2.mtmt.hu/api/publication/33351972},
	author = {Gyökeres, Imre and Dávid, Árpád and Fodor, Rozália},
	booktitle = {25. Magyar Őslénytani Vándorgyűlés, Tótvázsony, 2022 Program, előadáskivonatok, kirándulásvezető},
	unique-id = {33351972},
	year = {2022},
	pages = {15-16}
}

@article{MTMT:33351496,
	title = {NATURAL CASTS OF ENTOBIA FROM THE LATE CAENOZOIC OF SICILY},
	url = {https://m2.mtmt.hu/api/publication/33351496},
	author = {GARILLI, VITTORIO and Dávid, Árpád and DOMINICI, STEFANO},
	doi = {10.54103/2039-4942/15175},
	journal-iso = {RIV IT PALEON STRATIG},
	journal = {RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA},
	volume = {128},
	unique-id = {33351496},
	issn = {0035-6883},
	abstract = {As with other ichnofossils, the study of the ichogenus Entobia Bronn, 1837, attributed to the activity of boring sponges, is useful to understand taphonomic processes and reconstruct paleoenvironments. Here we delineate a diverse Entobia assemblage from Sicily, the first described from this Mediterranean island, based on the discovery of well-preserved natural casts. The studied association is represented by seven ichnotaxa, Entobia cateniformis, E. cateniformis form A, E. geometrica, E. laquea, E. ?megastoma, E. ovula, E. ?paradoxa, which come from the late Caenozoic sites of Altavilla Milicia and Sferracavallo, in north-western Sicily. Aragonitic bivalves, mostly veneroids, served as substrate for the boring organisms responsible of producing these ichnotaxa. Entobia was also found associated with natural casts of the boring Caulostrepsis taeniola, produced by polychaetes. Ichnology and shell-bed taphonomy indicates that investigated deposits formed in conditions of low rate of sedimentation; post depositional processes involved chemical conditions favorable to the preservation of calcite shells.},
	year = {2022},
	eissn = {2039-4942},
	pages = {211-228},
	orcid-numbers = {GARILLI, VITTORIO/0000-0001-8809-4176; DOMINICI, STEFANO/0000-0003-3719-0605}
}

@article{MTMT:32833540,
	title = {Nodulichnus hungaricus igen. et isp. nov. from the Early Miocene of North Hungary},
	url = {https://m2.mtmt.hu/api/publication/32833540},
	author = {Fodor, Rozália and Dávid, Árpád},
	doi = {10.14241/asgp.2022.06},
	journal-iso = {ANN SOC GEOL POL},
	journal = {ANNALES SOCIETATIS GEOLOGORUM POLONIAE},
	volume = {92},
	unique-id = {32833540},
	issn = {0208-9068},
	year = {2022},
	eissn = {0208-9068}
}

@{MTMT:33351198,
	title = {A rája lakomája-Piscichnus waitemata a bükki kora-miocénből},
	url = {https://m2.mtmt.hu/api/publication/33351198},
	author = {Dávid, Árpád and Fodor, Rozália},
	booktitle = {24. Magyar Őslénytani Vándorgyűlés, Program, előadáskivonatok, kirándulásvezető},
	unique-id = {33351198},
	year = {2021},
	pages = {9-10}
}

@article{MTMT:31924603,
	title = {Diverse bioerosion structures in lower Pliocene deposits from a volcanic oceanic island: Baía de Nossa Senhora section, Santa Maria Island, Azores (central North Atlantic)},
	url = {https://m2.mtmt.hu/api/publication/31924603},
	author = {Dávid, Árpád and Uchman, Alfred and Ramalho, Ricardo S. and Madeira, José and Melo, Carlos S. and Madeira, Patrícia and Rebelo, Ana Cristina and Berning, Björn and Johnson, Markes E. and Ávila, Sérgio P.},
	doi = {10.1016/j.palaeo.2021.110284},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {569},
	unique-id = {31924603},
	issn = {0031-0182},
	abstract = {Pliocene body fossils from Santa Maria Island, Azores, have been studied for decades, but only more recently have ichnofossils received their due attention. Calcareous Pliocene deposits from the Baia de Nossa Senhora section contain numerous, diverse, well-preserved natural casts of invertebrate borings. The study of this type of fossils adds to knowledge on the dispersal of benthic faunas across oceans to volcanic oceanic islands. The borings belong to seven ichnogenera and twenty-two ichnotaxa at the ichnospecies level with more than half pertaining to Entobia, which is produced by clionaid sponges. Other borings found were produced by bivalves (Gastrochaenolites), polychaete worms (Caulostrepsis and Maeandropolydora), sipunculid worms (Trypanites), phoronid worms (Talpina) and ctenostome bryozoans (Iramena). The occurrence, ichnogeny, distribution and preservational state of the borings suggest that the bearing bioclasts have been exposed for several years on the sea floor. The borings derive from different bathymetric zones on the shelf, and their formation took place during several bioerosional phases. The association of borings belongs to the Entobia ichnofacies, which is typical of carbonate rocky shores, and shows close similarity to those described from the Paratethys, Mediterranean and partly the eastern Atlantic regions. This fits the idea that most of the Neogene shallow-water marine fauna in the Azores is biogeographically related to the eastern Atlantic shores.},
	keywords = {hard substrate; Bioerosion; trace fossils; Ichnology; Geosites},
	year = {2021},
	eissn = {1872-616X}
}

@{MTMT:31924735,
	title = {Adalékok a mecseki középső-miocén paleoichnológiájához (Hetvehely, vasúti bevágás)},
	url = {https://m2.mtmt.hu/api/publication/31924735},
	author = {Fodor, Rozália and Dávid, Árpád},
	booktitle = {23. Magyar Őslénytani Vándorgyűlés},
	unique-id = {31924735},
	year = {2020},
	pages = {12}
}

@article{MTMT:31924598,
	title = {Pliocene-Pleistocene stratigraphic paleobiology at Altavilla Milicia (Palermo, Sicily): tectonic, climatic and eustatic forcing},
	url = {https://m2.mtmt.hu/api/publication/31924598},
	author = {Stefano, Dominici and Marco, Benvenuti and Vittorio, Garilli and Alfred, Uchman and Francesco, Pollina and Dávid, Árpád},
	journal-iso = {B SOC PALEONTOL ITAL},
	journal = {BOLLETTINO DELLA SOCIETA PALEONTOLOGICA ITALIANA},
	volume = {59},
	unique-id = {31924598},
	issn = {0375-7633},
	abstract = {The integration of sedimentary facies analysis, ichnology and benthic mollusc quantitative paleoecology allowed interpretation of factors that have controlled the deposition of the alluvial to marine succession outcropping in Northwestern Sicily (Southern Italy) at Altavilla Milicia, near Palermo (Imerese Basin). Two main marine units are recognised, labelled CNM and ALT, separated by an angular unconformity and formed by elementary depositional sequences (CNM1-4, ALT1-5). The succession was subdivided by means of calcareous nannoplankton biostratigraphy into upper Pliocene (Piacenzian: CNM1-4 and ALT1-4) and lower Pleistocene (Gelasian, ALT4-5), covering the onset of the Quaternary glaciation. The main asset of the succession is driven by tectonic compression and accommodation by transpressional faults, a regime that led to a change in the direction of fluvial sediment delivery, from axial (mid-Piacenzian: CNM), to transverse with respect to the basin elongation (upper Piacenzian-Gelasian: ALT). High-frequency eustatic changes drove the formation of elementary depositional sequences, the building blocks of CNM and ALT. During the late Piacenzian, a phase of gradual passage from the mid-Piacenzian warm period to the Quaternary glaciation, bioclastic production was still high, characterising the maximum flooding intervals of the two composite depositional sequences CNM and ALT. Mixed carbonate-siliciclastic lithosomes of both CNM and ALT show a good correlation with shallow marine shell-rich detrital carbonates of Northern and Southern Italy and with Mediterranean deep-water sapropel clusters, suggesting common climatic forcing. Some tropical species thought to disappear from the Mediterranean at around 3.0
		Ma, including Pecten bosniasckii, Macrochlamys latissima, Spondylus crassicosta, Lucina orbicularis, Isognomon maxillatus, Crassatina concentrica, Gastrana lacunosa, Callista italica, Circomphalus foliaceolamellosus and Persististrombus coronatus, are present in the upper Piacenzian of Sicily (top of the MN16a Zone and the MN16b/17 Zone of calcareous nannofossil biostratigraphy). More data are needed to reconstruct the geographic dimension in the disappearance of the Mediterranean Pliocene macrobenthos with tropical affinities.},
	keywords = {climate change; Mediterranean Sea; Calcareous nannoplankton; Ichnology; Mollusca; Facies analyses},
	year = {2020},
	pages = {57-83}
}

@CONFERENCE{MTMT:31924693,
	title = {Trace fossils as indicators of Quaternary environmental changes at Weereewa (Lake George), NSW, Australia},
	url = {https://m2.mtmt.hu/api/publication/31924693},
	author = {Eva, Papp and Rozalia, Fodor and Dávid, Árpád and Alex, Franke and Brad, Pillans and Sue, Rule and Brad, Opdyke},
	booktitle = {Abstract Book},
	unique-id = {31924693},
	year = {2019},
	pages = {72}
}

@CONFERENCE{MTMT:31924647,
	title = {A Walk in the Gyrolithes Heaven (Ichnology of an Early Miocene Age Sand-pit, Tardona Hills, North-Hungary)},
	url = {https://m2.mtmt.hu/api/publication/31924647},
	author = {Fodor, Rozália and Dávid, Árpád},
	booktitle = {15th International Ichnofabric Workshop},
	unique-id = {31924647},
	year = {2019},
	pages = {12-13}
}