identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
D36487CDFFF5FFC66493D0C61157FAD2.text	D36487CDFFF5FFC66493D0C61157FAD2.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Palaeocryptonyx hungaricus Janossy 1991	<div><p>†  Palaeocryptonyx hungaricus Jánossy, 1991 (syn: † Eurobambusicola turolicus Zelenkov, 2016)</p><p>Location and age: Beremend 26; Lower Pliocene (MN15).</p><p>Material: a proximal left coracoid fragment (omal part) (Figure 2 /4).</p><p>Dimensions (in mm): coracoid: C—5.5–5.9, D—3.3–3.5, E—3.0–3.2.</p><p>Description: similar to  Gallus bones, quail size.</p><p>Previous records of the taxon—sites and their age: Rátka, Upper Miocene (MN 12–13) (Kessler 2009b)— complete skeleton without skull; Polgárdi 4, 5, Upper Miocene (MN 13) (Jánossy 1991, 1995); Beremend 26, Lower Pliocene (MN 15) (Kessler 2009b), Beremend 17, 18 Lower Pleistocene (Q1) (Jánossy 1992, 1996). Mátraszőlős 3, Middle Miocene (Horváth 2023). Other than the above, no other sites have been reported. Along with other members of the genus, Mlíkovskỳ (2002) assigned  Palaeocryptonyx hungaricus to †  Alectoris donnezani (Depéret, 1892), while Zelenkov (2016) renamed it as Eurobambusicola turolicus.</p><p>This material is not catalogued, it belongs to the Chapel of Reconciliation in Beremend and will be catalogued in their collection.</p></div>	https://treatment.plazi.org/id/D36487CDFFF5FFC66493D0C61157FAD2	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF5FFC66493D3DA1159FDCA.text	D36487CDFFF5FFC66493D3DA1159FDCA.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Pandion pannonicus Kessler 2018	<div><p>†  Pandion pannonicus Kessler, 2018</p><p>Location and age: Máriahalom; Lower Miocene (MN16).</p><p>Material: phalanx ungualis, digit pedis II (Figure 2 /3).</p><p>Dimensions (mm): A—19.3, B—9.9, C—3.50, D—5.20, E—4.8.</p><p>Description: This fossil, like the previously identified bones of †  Pandion pannonicus, is smaller than those of the currently known osprey. The tuberculum extensorium is oblique with a blunt end; the cotyla articularis has an asymmetrical outline; the neck of the tuberculum flexorium is short, the lower part is convex in the middle; the corpus phalangis is wide and curved and the apex phalangis is damaged. The dimensions of the fossil are 80% of those of the extant species. It is similar in size and shape to the holotype example described.</p><p>Comparative material:  Pandion haliaetus (2010.222.1);  Pandion pannonicus Kessler, 2018 (uncatalogued).</p><p>This material is catalogued, number:VER 2021. 72; the bones belong to the collection of the Hungarian Museum of Natural History.</p></div>	https://treatment.plazi.org/id/D36487CDFFF5FFC66493D3DA1159FDCA	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF5FFC76493D6861157FECE.text	D36487CDFFF5FFC76493D6861157FECE.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Palaeortyx Milne-Edwards 1869	<div><p>†  Palaeortyx Milne-Edwards, 1869</p><p>†  Palaeortyx gallica Milne-Edwards, 1869 / syn.  P. intermedia Ballmann, 1969 / †  Coturnix gallica (Milne-Edwards, 1869), (Mlíkovskỳ 2002).</p><p>Location and age: Beremend 38; Lower Pliocene (MN16).</p><p>Material: 1 distal right tarsometatarsus (Figure 2 /5).</p><p>Dimensions (in mm): tarsometatarsus: E—3.5, F—6.7, G—5.0.</p><p>Description: The description was given by Göhlich and Mourer-Chauviré (2005). Within the extinct pheasant species, the  Palaeortyx species are distinct both in size and in anatomical characters.  Palaeortyx gallica is a mediumsized extinct pheasant species within the  Palaeortyx genus. This species is slightly larger in size than  P. brevipes, but much smaller than  P. phasianoides . In  P. gallica, the tarsometatarsus has an anatomical marker that makes it easier to distinguish from other species, but this fossil specimen lacks this marker (fossa parahypotarsalis).</p><p>Previous records of the taxon—sites and their age: Grund, Lower Miocene (MN 5) (Göhlich 2003); Litke 2, Lower Miocene (MN 5) (Kessler &amp; Hír 2012); Kőalja 2, Middle Miocene (MN 6) (Kessler &amp; Venczel 2009); Mátraszőlős 1, Middle Miocene (MN 6–8) (Kessler 2009b); Rudabánya, Upper Miocene (MN 9) (Kessler 2009b); Polgárdi, Upper Miocene (MN 13) (Kessler 2009b); Mátraszőlős 3, Middle Miocene (Horváth 2023).</p><p>Comparative material:  Perdix perdix (67.21.1);  Coturnix coturnix (2010.1226.1);  Gallus gallus domesticus (60.12.1);  Alectoris rufa (68.7.1);  Alectoris graeca (2010.1221.1).</p><p>This material is not catalogued, it belongs to the Chapel of Reconciliation in Beremend and will be catalogued in their collection.</p></div>	https://treatment.plazi.org/id/D36487CDFFF5FFC76493D6861157FECE	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF4FFC76493D2B21157FAA6.text	D36487CDFFF4FFC76493D2B21157FAA6.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Tetrao Linnaeus 1758	<div><p>Tetrao Linnaeus, 1758</p><p>†  Tetrao praeurogallus Jánossy, 1969 / †  T. conjugens Jánossy, 1974 / †  T. macropus Jánossy, 1976a</p><p>Location and age: Beremend 38; Lower Pliocene (MN16).</p><p>Material: 1 distal left humerus (Figure 2 /6).</p><p>Dimensions (in mm): humerus: E—10.5, F—18.5, G—10.2.</p><p>Description: In his original diagnosis (Jánossy 1969), Dénes Jánossy described the morphological difference between fossil and modern species only in the proximal epiphysis. The dimensions suggest that the fossil from Beremend may be from a hen.</p><p>Previous records of the taxon—sites and their age: MN15—Csarnóta 2 (Jánossy 1976a, 1979a; Kessler 2009a); Beremend 26 (Kessler 2009a); Q1—Osztramos 7 (Jánossy 1973, 1976a, 1979a); Q2—Méhész 1 (Kretzoi 1975; Jánossy 1976a, 1979a); Nagyharsányhegy 1–4 (Lambrecht 1916, 1933; Jánossy 1976a, 1979a); Q3/I—Hundsheim (Jánossy 1971, 1974, 1976a); Tarkő 10 (Jánossy 1976a, 1979a).</p><p>The earliest European presence of the capercaillie is known from the Early Pliocene at Dorkovo in Bulgaria (MN 14) (Boev 1998), followed by the sites Csarnóta and Beremend in Hungary, and the sites Weze in the Vistula in Poland (MN 15) and Rebielice Królowskie, Ostramos 7 (MN 16) of similar age (Jánossy 1976b; Bocheński 1989; Mlíkovskỳ 2002; Kessler 2009a).</p><p>Comparative material: fossil:  Tetrao praeurogallus Jánossy, 1969 (V.10.374); recent:  Tetrao urogallus (58.37.1).</p><p>This material is not catalogued, it belongs to the Chapel of Reconciliation in Beremend and will be catalogued in their collection.</p></div>	https://treatment.plazi.org/id/D36487CDFFF4FFC76493D2B21157FAA6	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF4FFC46493D6A31159FD02.text	D36487CDFFF4FFC46493D6A31159FD02.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Balearica Brisson 1760	<div><p>Balearica Brisson, 1760</p><p>aff. †  Balearica excelsa (Milne-Edwards, 1868) —syn. †  Grus excelsa Milne-Edwards, 1868, see Mlíkovskỳ, 2002</p><p>Location and age: Máriahalom; Lower Miocene (MN16).</p><p>Material: ungual phalanx (Figure 2 /7).</p><p>Dimensions (in mm): A—10.2, B—5.2.</p><p>Description: Characteristic crane ungual (distal pedal phalanx), which shows a characteristic sulcus along the side of the ungual in addition to the flattened ventral face. The fossil bone is more robust than the recent species, but this discovered bone is not from the  Grus genus. The tuberculum extensorium protrudes, the cotyla articularis is more concave laterally. The tuberculum flexorum is bluntly protruding.</p><p>One species of the genus has been described so far in Hungary, †  Balearica excelsa (Milne-Edwards 1868), from the Late Oligocene of Máriahalom (MP25), which was identified from a claw bone (phal. 2 dig. I) (collected by Zoltán Evanics, in the collection of the Department of Palaeontology of ELTE). Dimensions of the claw: length of the claw bone 11–12 mm, length of the distal part of the joint 4.16 mm, including the cotyla articularis 5.74 mm, thickness 2.78 mm. The shape of the claw bone, with its sulcus, is characteristic and its size corresponds to that of a recurrent crane (Kessler 2013a).</p><p>Since cranes are represented in the fossil bird fauna of Europe only from Eocene and Late Miocene strata, the find can be compared with only one known species, a fossil species described from the Early Miocene in France (Saunt-Gérand-le-Puy, MN2). Originally described as  Grus excelsa by Milne-Edwards, 1868, the species was placed in  Balearica by Mlíkovský (2002). It is also known in France, from Artenay (Lower Miocene, MN4) and Sansan (Middle Miocene, MN6). Mlíkovský (2002) also synonymised  Balearica excelsa with  Grus miocaenicus Grigorescu &amp; Kessler, 1977, described from the Middle Miocene of Dobrudzsa, Romania.</p><p>Distribution: Early Miocene (MN2a) of Saint-Gérand-le-Puy, France (Milne-Edwards 1869 –1871; Cracraft 1973; Cheneval 2000); early Miocene (MN4) of Artenay, France; and middle Miocene (MN6) of Sansan, France (Cheneval 2000).</p><p>This material is catalogued, number VER 2021. 73; the bones belong to the collection of the Hungarian Museum of Natural History.</p></div>	https://treatment.plazi.org/id/D36487CDFFF4FFC46493D6A31159FD02	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF7FFC56493D09F1157FECE.text	D36487CDFFF7FFC56493D09F1157FECE.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Cuculus csarnotanus Janossy 1979	<div><p>†  Cuculus csarnotanus Jánossy, 1979 (in Jánossy 1979b)</p><p>Location and age: Beremend 26; Lower Pliocene (MN15).</p><p>Material: 1 complete left tarsometatarsus (Figure 2 /8).</p><p>Dimensions (in mm): tarsometatarsus: A—14.1, C—4.0, D—3.7, E—2.0, F—4.3, G—2.4.</p><p>Previous records of the taxon—sites and their age: the fossil species was originally described from a distal epiphysis of a humerus (MTM. Vt.80) smaller in size but morphologically similar to the European cuckoo from the Early Pliocene (MN 15) site Csarnóta 2, near Beremend (Jánossy 1979b).</p><p>A distal ulna (MÁFI V.09.341.1) from the Late Miocene of Polgárdi 4 (MN 13), and a distal humerus (MTM V.2009.51.1) from the Late Pliocene of Beremend 15 (MN 16), the holotype, were described as †  Cuculus pannonicus Kessler, 2010 (Kessler 2010, 2013a). Nikita Zelenkov wrote in a 2017 article that “This ulna cannot be referred to a cuckoo, since its tuberculum carpale is set strongly aside relative to the shaft and the proximal apex of its condylus ventralis [is] shifted ventrally; in these characters and general outline, this bone is similar to those of  Charadriiformes ”, p. 210. Therefore, he identified it as  Scolopacidae fam. indet. (Zelenkov 2017).</p><p>The size of the characteristic cuckoo skeletal parts exceeds that of the recent species and far exceeds that of the fossil species from Csarnóta, but no tarsometatarsus occurs among any of the materials. A specimen of this family is already known from the Middle Miocene of Mátraszőlős 1, from where it was identified as  Cuculidae gen. et sp., based on unidentified material of  Passeriformes indet. from Gál et al. (1999; this fossil was identified in 1998), which was not further defined.</p><p>The genus is unknown from the Neogene of Europe. The earliest fossil species assigned to the taxon is  Chambicuculus pusillus Mourer-Chauviré et al., 2013, which dates from the late Early to early Middle Eocene in Tunisia. This very small bird is known from several isolated tarsometatarsi as well as a referred coracoid and femur (Mourer-Chauviré et al. 2013, 2016). These bones show a close resemblance to the corresponding elements of extant species of  Cuculiformes, with the tarsometatarsus bearing a large accessory trochlea for the fourth toe (Mayr 2022).</p><p>Outside the Carpathian Basin, the recent species is known from the Lower Pleistocene of Spain (Quibas, Q1) and the Czech Republic (Stránská scale, Q2). Thus, the Carpathian Basin material is unique from this age in Europe. The order  Cuculiformes is possibly represented from the Eocene through the species †  Parvicuculus minor Harrison &amp; Walker, 1977, which was described from a tarsometatarsus from the Burnham-on-Crouch (MP 8–9, London Clay) site in England (Harrison &amp; Walker 1977; Harrison 1982) and from the Condé-en Brie (MP 8–9) site in France (Mayr &amp; Mourer Chauviré 2005). Apart from these, only North American and European Pleistocene-age fossils are known.</p><p>Comparative material:  Cuculus canorus (2010.418.1).</p><p>This material is not catalogued, it belongs to the Chapel of Reconciliation in Beremend and will be catalogued in their collection.</p></div>	https://treatment.plazi.org/id/D36487CDFFF7FFC56493D09F1157FECE	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF6FFC56493D1C31121FB6E.text	D36487CDFFF6FFC56493D1C31121FB6E.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Surnia robusta Janossy 1977	<div><p>†  Surnia robusta Jánossy, 1977</p><p>Location and age: Beremend 38; Lower Pliocene (MN16).</p><p>Material: 1 distal right tarsometatarsus (Figure 2 /9).</p><p>Dimensions (in mm): E—8.3, F—11.5, G—9.2.</p><p>Description: In particular, the tarsometatarsus varies between owl species. Morphological differences are mostly found in the distal epiphysis. In this case, the diaphysis is rather short and stout and the trochlea metatarsi II is clublike.</p><p>Previous records of the taxon—sites and their age: Known from the Upper Miocene of the Carpathian Basin (MN 13)—Polgárdi 4, 5 (Hungary) (Kessler 2010); MN16—Ostramos 7, Beremend 4, Villány 3 (all in Hungary) (Jánossy 1977); Q1–2—Nagyharsányhegy 1–4, Somssich hill 2 (all in Hungary) (Jánossy 1977, 1982, 1983, 1986; Kessler 2017).</p><p>Comparative material:  Asio otus (2010.502.1);  Asio flammeus (2010.487.1);  Aegolius funereus (2010.1624.1);  Surnia ulula (2010.1640.1).</p><p>This material is catalogued number: B.38.2020.07.07; and belongs to the Chapel of Reconciliation in Beremend.</p></div>	https://treatment.plazi.org/id/D36487CDFFF6FFC56493D1C31121FB6E	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF6FFCA6493D57B1157FD02.text	D36487CDFFF6FFCA6493D57B1157FD02.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Corvus harkanyensis Kessler 2010	<div><p>†  Corvus harkanyensis Kessler, 2010</p><p>Location and age: Beremend 26; Lower Pliocene (MN15).</p><p>Material: 1 distal left humerus (Figure 2 /10), 1 proximal right scapula (Figure 2 /11).</p><p>Dimensions (in mm): humerus: F—13.3, G—5.5; scapula: B—5.8, C—5.1/4.2.</p><p>Previous records of the taxon—sites and their age: The holotype is from the  Upper Pliocene (MN15–16) of Csarnóta 2, with humerus dimensions: E—4.9, F—11.5, G—5.9, H—6.2. The dimensions of the modern species  Corvus monedula are: humerus E—4.1–4.6, F—9.4–11.1, G—5.4–6.1, H—5.5–6.46. It was described as a species of crow of the size of a corvid species, in which the condylus ventralis on the distal epiphysis of the humerus is not ovate but rounded; the epicondylus ventralis is much wider and more iron-shaped; the processus flexorius is more prominent; processus supracondylaris dorsalis and epicondylus dorsalis lack the concave indentation present in the jackdaw (Kessler 2010). The scapula is heavily damaged, but has crow-like features and its dimensions are similar to those of the jackdaw.</p><p>It takes its name from the nearby town of Harkány. This fossil species, with the characteristics and size of a modern jackdaw, may have been the ancestor of the present form of  Corvus in the Carpathian Basin.</p><p>A small-sized  Corvus species is known from the Upper Pliocene ( Corvus cf. monedula: Văršec Bulgaria, MN17 (Boev 2000), which is the only small-sized species of the genus from the recent avifauna of Europe (although presently renamed as  Coloeus monedula). From the Early Pleistocene of the Stránská scale in the Czech Republic,  Corvus moravicus Mlíkovsk ỳ, 1995 was described as an extinct taxon, but this species was later revised by the author himself and the material was assigned to the modern jackdaw ( C. monedula Linnaeus, 1758) (Mlíkovskỳ 2002). The latter species has also been identified from several Lower, Middle and Upper Pleistocene sites (Jánossy 1979a,b; Gál 2002). Apart from the species of  Corvidae mentioned above, only Miocene finds from North America have been described; Olson and Rasmussen (2001) reported the taxon  Corvus aff. ossifragus Wilson, 1812 from the Lee Creek Mine site, based on a tibiotarsus.</p><p>Comparative material:  Corvus monedula (61.9.1);  Pica pica (58.I.17);  Garrulus glandarius (48.VIII.24);  Nucifraga caryocatactes (71.10.27).</p><p>This material is not catalogued, it belongs to the Chapel of Reconciliation in Beremend and will be catalogued in their collection.</p></div>	https://treatment.plazi.org/id/D36487CDFFF6FFCA6493D57B1157FD02	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF9FFCA6493D00F1362FAA6.text	D36487CDFFF9FFCA6493D00F1362FAA6.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Muscicapidae Fleming 1822	<div><p>Muscicapidae gen. et sp. indet.</p><p>Location and age: Beremend 26; Lower Pliocene (MN15).</p><p>Material: 1 ungual phalanx (Figure 3 /1).</p><p>Dimensions (in mm): ungual phalanx: A—3.9, B—1.9.</p><p>Description: the direction and the form of the tuberculum extensorium is straight and blunt; the form of the cotyla articularis is weakly concave; the shape of the tuberculum flexorium is concave and the concavity of the margo plantaris is strongly arched symmetrically. The form of the apex is missing.</p><p>Previous records of the taxon—sites and their age: Outside the Carpathian Basin, the family is only known from the late Pliocene by  Ficedula sp. from Montoussé 5 in France (Clot et al. 1976), and from the Pleistocene by  Oenanthe cf. oenanthe from Hundsheim in Austria the extant species (Tyrberg 1998); MN13—Polgárdi 5 (Kessler 2010); MN15—Csarnóta 2; Beremend 26 (Kessler 2010), as a preliminary indication of  Oenanthe cf. oenanthe .</p><p>Comparative material:  Oenanthe oenanthe (2010.1816.1).</p></div>	https://treatment.plazi.org/id/D36487CDFFF9FFCA6493D00F1362FAA6	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
D36487CDFFF8FFC86493D6331299FE22.text	D36487CDFFF8FFC86493D6331299FE22.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Aves	<div><p>Aves indet.</p><p>Location and age: Beremend 26; Lower Pliocene (MN15)</p><p>Material: 1 radius proximal fragment (Figure 3 /4)</p><p>Dimensions (in mm): radius: C—3.1, D—1.9, E—1.6.</p><p>Description: This proximal radius cannot be identified to species, but judging by its size and character, may belong to a species of a songbird.</p><p>Location and age: Egyházasdengeleg, Late Miocene (MN 12–13)</p><p>Material:1 ungual phalanx (from Egyházasdengeleg) (Figure 3 /5)</p><p>Dimensions (in mm): ungual phalanx: A—7.7, B—5.0, C—3.0.</p><p>Location and age: Hidas, Middle Miocene (MN 7–8)</p><p>Material: pedal phalanx II.1(Figure 3 /6).</p><p>Dimensions (in mm): phalanges pedis: A—10.9, C—3.4, E—1.6, F—2.8, G—1.9, F—4.5, G—1.5.</p><p>Location and age: Alsótelekes; Late Miocene (MN 12–13).</p><p>Material: part ungual phalanx (Figure 3 /7)</p><p>Dimensions (in mm): A—11.7, B—5.1.</p><p>Location and age: Alsótelekes; Late Miocene (MN 12–13)</p><p>Material: partial manal phalanx proximalis digiti majoris (Figure 3 /8)</p><p>Dimensions (in mm): A—ca. 25.0, E—7.2.</p></div>	https://treatment.plazi.org/id/D36487CDFFF8FFC86493D6331299FE22	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Horváth, Ida	Horváth, Ida (2025): New records of fossil bird bones from the Neogene in Hungary. Zootaxa 5627 (2): 327-342, DOI: 10.11646/zootaxa.5627.2.5, URL: https://doi.org/10.11646/zootaxa.5627.2.5
