identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
03CEF41BFFC5812EFDAB207CEBE3FB73.text	03CEF41BFFC5812EFDAB207CEBE3FB73.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Glis sackdillingensis (Heller 1930)	<div><p>Glis sackdillingensis (Heller, 1930)</p><p>1930 Myxodus sackdillingensis n. sp. – HELLER, p. 281–282, pl. XVI. figs 5a-b, 6.</p><p>1962 Glis sackdillingensis (Heller, 1930) – DEHM, p. 46–47.</p><p>1963 Glis sackdillingensis (Heller, 1930) – KOWALSKI, p. 553–558, fig. 12.</p><p>1986 Glis sackdillingensis (Heller, 1930) – AGUILAR et al., p. 141, fig. 3a-c.</p><p>Description – P 4: Rounded tooth, with five ridges. The first ridge (anteroloph) is isolated, slightly arched anteriorly. The second ridge (protoloph) is long, and joined with the third one (anterior extra ridge) on the central part of the tooth. The fourth and the fifth ridges (metaloph and posteroloph) are isolated.</p><p>M 1: The tooth has rounded square shape and seven ridges. The first and third main ridges (anteroloph and protoloph) are isolated; there is a small, isolated ridge (anterior extra ridge) between the latter two. The fourth ridge is isolated (anterior centraloph), whereas the fifth and seventh ridges (metaloph and posteroloph) are joined on the palatinal side. Between the latter two ridges, there is a small, isolated ridge (posterior extra ridge).</p><p>M 2: Labiopalatinally elongated tooth, with seven ridges. The first ridge (anteroloph) is joins with a small ridge (anterior extra ridge) on the central part of tooth. The third and fourth ridges (protoloph and anterior centraloph) are isolated. The fifth and seventh ridges (metaloph and posteroloph) are joined on the palatinal side. The sixth small ridge (posterior extra ridge) is joined with the seventh ridge on the labial side.</p><p>M 3: Triangular tooth, with eight ridges. The first and third ridges (anteroloph and protoloph) are joined on the palatinal side. The anterior extra ridge (second ridge) is longer than the anterior centraloph (fourth ridge). These former ridges are joined on the palatinal side. The fifth ridge (posterior centraloph) is isolated. The extra ridges (second and sixth ridges) are joined on the labial side. The seventh ridge (metaloph) is small and isolated. The eighth ridge (posteroloph) is also joined the two extra ridges on the labial side.</p><p>P 4: Triangular tooth, with five ridges. The first and the second ridges (anterolophid and metalophid) are joined on both sides. The third ridge (mesolophid) is isolated, whereas the fourth and fifth ridges (posterior extra ridge and posterolophid) are joined on the labial side.</p><p>M 1: Anteriorly elongated, narrowed tooth, with seven ridges. The first, second and third ridges (anterolophid, anterior extra ridge and metalophid) are joined on the labial side. The fourth ridge (centralophid) is short and isolated.</p><p>1</p><p>The fifth, sixth and seventh ridges (mesolophid, posterior extra ridge and posterolophid) are joined on the labial side.</p><p>M 2: Squared tooth, with seven ridges. The first and second ridges (anterolophid and anterior extra ridge) are joined on the labial side. All other ridges are isolated.</p><p>M 3: Shield shaped tooth, which is rounded on the posterior side, with seven ridges. The first, second, third and fourth ridges (anterolophid, anterior extra ridge, metalophid and centralophid) are joined on the labial side. The fifth ridge (mesolophid) is isolated, whereas the sixth and seventh ridges (posterior extra ridge and posterolophid) are joined on the labial side.</p><p>1</p><p>Remarks – Two species of the genus Glis have been described from the Pliocene: G.minor Kowalski, 1956 and G.sackdillingensis (Heller, 1930) (KOWALSKI 1956; AGUILAR et al. 1986), whereas several species of the genus have been observed in the Pleistocene: G. sackdillingensis, G. mihevci Aguilar et Michaux, 2011, G. perkoi Aguilar et Michaux, 2011 and the extant G. glis (Linnaeus, 1766) (KOWALSKI 1963; AGUILAR &amp; MICHAUX 2011). A gradual size increase of the molars is observed in Glis from the Pliocene until recently. Morphology has evolved in this time span from primitive forms with transversal crests, synclines open on the lingual side in the upper molars and labial side in lower ones and accessory ridges reduced in P 4 and M 3 (KOWALSKI 1956; JÁNOSSY 1966; AGUILAR &amp; MICHAUX 2011; MANSINO et al. 2013). According to a recently accepted view, the edible dormouse ( G. glis) is descendant of G. sackdillingensis .</p><p>Altogether, 4 P 4, 28 M 1 (9 G. sackdillingensis; 19 G. minor), 13 M 2, 6 M 3, 2 P 4, 16 M 1 (8 G. sackdillingensis; 8 G. minor), 12 M 2 and 10 M 3 teeth of Glis were found in the Somssich Hill 2 samples. In case of G. sackdillingensis M 1, the lengths of teeth vary between 1.7 and 1.95 mm, whereas the lengths of M 1 are 1.68–1.91 mm (Fig. 5). Within the sequence of locality, G. sackdillingensis was found with G. minor in most cases (layers 5, 13, 24, 28, 30–31, 40 and 45). The number of specimens of the latter taxon is usually lower than in the case of G. minor, but in cases of layers 4, 29–31, 36, and 40 G. sackdillingensis is the dominant dormouse in the fauna (Fig. 6; see also Fig. 12).</p></div>	https://treatment.plazi.org/id/03CEF41BFFC5812EFDAB207CEBE3FB73	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.		Plazi	Striczky, L.;Pazonyi, P.	Striczky, L., Pazonyi, P. (2014): Taxonomic study of the dormice (Gliridae, Mammalia) fauna from the late Early Pleistocene Somssich Hill 2 locality (Villány Hills, South Hungary) and its palaeoecological implications. Fragmenta Palaeontologica Hungarica 31: 51-81, DOI: 10.17111/FragmPalHung.2014.31.51, URL: https://doi.org/10.17111/fragmpalhung.2014.31.51
03CEF41BFFC8812EFDAA267EEAD9F886.text	03CEF41BFFC8812EFDAA267EEAD9F886.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Glis minor Kowalski 1956	<div><p>Glis minor Kowalski, 1956</p><p>1956 Glis sackdillingensis minor n. ssp. – KOWALSKI, p. 384–385, pl. IV, fig. 8, text-fig. 2f.</p><p>1959 Glis minor Kowalski, 1956 – KRETZOI, p. 240.</p><p>1963 Glis minor Kowalski, 1956 – KOWALSKI, p. 543–550, fig. 8–10.</p><p>1964 Glis minor Kowalski, 1956 – SULIMSKI, p. 228–229, pl. XIV.</p><p>Description – Since the molar teeth of the two Glis species are not distinguishable based on their morphological characters, description of teeth see above.</p><p>Remarks – In case of G. minor M 1, the lengths of teeth are between 1.45 and 1.6 mm, while the lengths of M 1 are between 1.42 and 1.6 mm (Fig. 5). Within the sequence of locality, G. minor was the dominant dormouse in several layers (layers 2, 5, 12–14, 25–26, 28 and 45). The number of specimens increased particularly in the upper part of sequence.</p><p>Somssich Hill 2 locality was a later occurrence of G. minor, which earlier was only described from Pliocene (Csarnóta 2, Podlesice, Węże) and Early Pleistocene (Osztramos 7) localities (JÁNOSSY 1986; KOWALSKI 1956).</p></div>	https://treatment.plazi.org/id/03CEF41BFFC8812EFDAA267EEAD9F886	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.		Plazi	Striczky, L.;Pazonyi, P.	Striczky, L., Pazonyi, P. (2014): Taxonomic study of the dormice (Gliridae, Mammalia) fauna from the late Early Pleistocene Somssich Hill 2 locality (Villány Hills, South Hungary) and its palaeoecological implications. Fragmenta Palaeontologica Hungarica 31: 51-81, DOI: 10.17111/FragmPalHung.2014.31.51, URL: https://doi.org/10.17111/fragmpalhung.2014.31.51
03CEF41BFFC9812FFDB922CAEA50FDFF.text	03CEF41BFFC9812FFDB922CAEA50FDFF.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Muscardinus Kaup 1829	<div><p>Genus Muscardinus Kaup, 1829</p><p>Remarks – One Muscardinus species was found in the material of Somssich Hill 2 locality. This species was not recognized by JÁNOSSY (1990), only Muscardinus sp. was mentioned in his preliminary list.</p></div>	https://treatment.plazi.org/id/03CEF41BFFC9812FFDB922CAEA50FDFF	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.		Plazi	Striczky, L.;Pazonyi, P.	Striczky, L., Pazonyi, P. (2014): Taxonomic study of the dormice (Gliridae, Mammalia) fauna from the late Early Pleistocene Somssich Hill 2 locality (Villány Hills, South Hungary) and its palaeoecological implications. Fragmenta Palaeontologica Hungarica 31: 51-81, DOI: 10.17111/FragmPalHung.2014.31.51, URL: https://doi.org/10.17111/fragmpalhung.2014.31.51
03CEF41BFFC9812BFDA5210BEDD3FBCE.text	03CEF41BFFC9812BFDA5210BEDD3FBCE.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Muscardinus dacicus Kormos 1930	<div><p>Muscardinus dacicus Kormos, 1930</p><p>1930 Muscardinus dacicus n. sp. – KORMOS, p. 243–244.</p><p>1963 Muscardinus aff. dacicus Kormos, 1930 – KOWALSKI, p. 543, fig. 6.</p><p>1993 Muscardinus dacicus Kormos, 1930 – DAOUD, p. 214–219, fig. 22.</p><p>2000 Muscardinus cf. dacicus Kormos, 1930 – MARCHETTI et al., p. 101, fig. 6/41.</p><p>Description – M 1: The tooth is markedly brachyodont, with five ridges. The first mesial ridge (protoloph) is oblique, the second one (posterior centraloph) is longer, sinuous, oblique, and extending along the palatinal side. The first ridge is very wide apart from the second one. The second, fourth (metaloph), and fifth (posteroloph) ridges are joined on palatinal side with the endoloph. The third one (posterior extra ridge) is shorter, and isolated on both sides (morphotype 1), or sinuous, and joined on palatinal side to the endoloph (morphotype 2).</p><p>M 2: The tooth is squared, with seven parallel, linear ridges. All ridges are joined on palatinal side with the endoloph. The third ridge (anterior extra ridge) is interrupted in the central part of the tooth. This ridge and the fourth one (anterior centraloph) are joined on labial side. The metacone is absent.</p><p>M 1: The tooth is long with six almost parallel main ridges, which are narrow especially in the anterior part. All ridges are isolated from each other. These characters are corresponding with morphotype 8 of recent M. avellanarius .</p><p>M 2: The tooth has six enamel ridges. The ridges are slightly arched anteriorly. The first, second, third and fourth ridges are isolated from each other. The fifth and sixth ridges (posterior extra ridge and posterolophid) are joined on lingual side (morphotype 1), or on both sides (morphotype 2).</p><p>Remarks – Altogether, 2 M 1, 1 M 2, 6 M 1, and 4 M 2 teeth of M. dacicus were found in the Somssich Hill 2 samples. Our material was compared with an Early Pleistocene dormouse, M. dacicus (Kormos, 1930), and recent M. avellanarius (Linnaeus, 1758) . These species are very similar, and László Kordos (March 2013, pers. comm.) suggested, that M. dacicus could plausibly correspond with the extant species. In order to verify this idea, recent M. avellanarius material was also analysed.</p><p>Eight morphotypes were determined by M 1 morphology of M. avellanarius, and these ones were compared with M. dacicus specimens from six Early and Middle Pleistocene localities: Betfia 2, 10, 13 (TERZEA &amp; JURCSÁK 1967; TERZEA 1973), Osztramos 7, Kövesvárad (JÁNOSSY 1986) (Fig. 7a, b).</p><p>On the basis of the fossil material and 50 M 1 of recent M. avellanarius, the middle part of this tooth (between the second and fifth ridges) is steady, while its anterior and posterior parts are very various (Table 2, Fig. 7).</p><p>Morphotype 1: The first and second ridges are isolated, whereas the fifth and sixth ones join on the labial side.</p><p>Morphotype 2: All ridges are isolated.</p><p>Morphotype 3: The first and second ridges join on the labial side, whereas the fifth and sixth ones isolated.</p><p>Morphotype 4: The first and second ridges are isolated, whereas the fifth and sixth ones join on both sides.</p><p>Morphotype 5: The first and second ridges join on the lingual side, whereas the fifth and sixth ones join on the labial side.</p><p>Morphotype 6: The first and second ridges are isolated, whereas the fifth and sixth ones join on the lingual side.</p><p>Morphotype 7: The first and second ridges join on the labial side, and the fifth and sixth ones join on the labial side, too.</p><p>Morphotype 8: The first and second ridges join on the labial side, whereas the fifth and sixth ones join on both sides.</p><p>All M. dacicus specimens corresponded with some morphotype of M. avellanarius . M. dacicus specimens of Osztramos 7 corresponded with morphotypes 1, 2, 3 (Fig. 7a), all specimens from Betfia localities (2, 10, 13) paralleled with morphotype 6, specimen of Kövesvárad corresponded with morphotype 5, whereas all specimens of Somssich Hill 2 paralleled with morphotype 8. According to these results, morphologically M. dacicus M 1 is very similar to recent M. avellanarius (Fig. 7b). Therefore, it is conceivable that the Early Pleistocene M. dacicus was not a separate species, but a morphotype of the recent M. avellanarius . However, in order to prove this hypothesis, more morphological and metric analysis is required on all teeth of both species.</p><p>Within the sequence of the Somssich Hill 2 locality, M. dacicus (Fig. 8) was less abundant, than Glis sackdillingensis or G. minor . Generally, it appeared with Glis (layers 4, 28–30 and 45), but at layer 15 M. dacicus was the only dormouse.</p></div>	https://treatment.plazi.org/id/03CEF41BFFC9812BFDA5210BEDD3FBCE	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.		Plazi	Striczky, L.;Pazonyi, P.	Striczky, L., Pazonyi, P. (2014): Taxonomic study of the dormice (Gliridae, Mammalia) fauna from the late Early Pleistocene Somssich Hill 2 locality (Villány Hills, South Hungary) and its palaeoecological implications. Fragmenta Palaeontologica Hungarica 31: 51-81, DOI: 10.17111/FragmPalHung.2014.31.51, URL: https://doi.org/10.17111/fragmpalhung.2014.31.51
03CEF41BFFCD812BFDB327FAEB3CFAC7.text	03CEF41BFFCD812BFDB327FAEB3CFAC7.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Dryomimus Kretzoi 1959	<div><p>Genus Dryomimus Kretzoi, 1959</p><p>Remarks – One Dryomimus species, D. eliomyoides Kretzoi, 1959, was identified from the locality. The name alludes to the transitional morphology of teeth of the aforementioned taxon between recent Dryomys and Eliomys species, although ridges appear on the occlusal surface too, similarly to Glis (DAAMS &amp; DE BRUIJN 1995) .</p></div>	https://treatment.plazi.org/id/03CEF41BFFCD812BFDB327FAEB3CFAC7	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.		Plazi	Striczky, L.;Pazonyi, P.	Striczky, L., Pazonyi, P. (2014): Taxonomic study of the dormice (Gliridae, Mammalia) fauna from the late Early Pleistocene Somssich Hill 2 locality (Villány Hills, South Hungary) and its palaeoecological implications. Fragmenta Palaeontologica Hungarica 31: 51-81, DOI: 10.17111/FragmPalHung.2014.31.51, URL: https://doi.org/10.17111/fragmpalhung.2014.31.51
03CEF41BFFCD8135FD9926E3EA47FD5F.text	03CEF41BFFCD8135FD9926E3EA47FD5F.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Dryomimus eliomyoides Kretzoi 1959	<div><p>Dryomimus eliomyoides Kretzoi, 1959</p><p>1959 Dryomimus eliomyoides n. g. n. sp. – KRETZOI, p. 240.</p><p>Description – P 4: Brachyodont, oval shaped tooth, which is prolated sideward. The paracone and the metacone emerge markedly on the labial side. The occlusal surface of the tooth is concave, with six main ridges. All ridges are joined on palatinal side with the endoloph, and are slightly arched anteriorly. The second and third ridges (protoloph and anterior centraloph) as well as the fourth and the fifth ridges (posterior centraloph and metaloph) are joined on the labial side. The anterior and posterior extra ridges are absent.</p><p>M 1: Rounded, oval shaped tooth, which is bigger than P 4. The occlusal surface is similar to P 4, but the ridges are more linear than in the case of the former one.</p><p>M 2: Angled oval shaped tooth, which is smaller than M 1. The occlusal surface is similar to the above mentioned ones, but the ridges are slightly arched posteriorly.</p><p>M 1: The shape of the tooth is oval, which has anterior, oblique orientation. There are five, anteriorly arched ridges on the occlusal surface. The first and the second ridges (anterolophid and metalophid) are joined on both sides, whereas the third ridge (centralophid) is joined only on the labial side to the former ones. Fourth and fifth ridges (mesolophid and posterolophid) are joined on the labial side, and compose a “U” shape.</p><p>M 2: The tooth is elongated anteriorly; the posterior end is firmly arched. There are six, anteriorly arched ridges on the occlusal surface. The first and the second ridges (anterolophid and metalophid) are joined on both sides, whereas the third ridge (centralophid) is joined only on the labial side to the former ones. Fourth and sixth ridges (mesolophid and posterolophid) are joined on the labial side. Fifth ridge (posterior extra ridge) is isolated between the former ones.</p><p>Remarks – Generally four or five ridges are found on the teeth. These ridges, mainly on the labial side, but sometimes on both sides, join. The unique markings of occlusal surface (“U” shapes) were evolved by connection of third and fourth or fourth and fifth ridges. Size of teeth is similar to Glis sackdillingensis (KRETZOI 1959) .</p><p>Altogether, 1 P 4, 2 M 1, 2 M 2, 1 M 1, and 1 M 2 teeth of D. eliomyoides were found from the Somssich Hill 2 locality (Fig. 9). It is the latest occurrence of Dryomimus eliomyoides, which was earlier described only from Pliocene (Csarnóta 2: JÁNOSSY 1986; Calta (Ankara): SEN et al. 1998; Kastoria 1: KOUFOS 2001) and Early Pleistocene (Osztramos 7, Villány 3: JÁNOSSY 1986; Tourkovounia 1: KOUFOS 2001) localities. Although, D. eliomyoides was the most infrequent dormice at the locality, this species appeared also in such layers where other glirids were absent (layers 19, 42, 44). This result maybe indicates that D. eliomyoides preferred different environment than the other dormice.</p></div>	https://treatment.plazi.org/id/03CEF41BFFCD8135FD9926E3EA47FD5F	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.		Plazi	Striczky, L.;Pazonyi, P.	Striczky, L., Pazonyi, P. (2014): Taxonomic study of the dormice (Gliridae, Mammalia) fauna from the late Early Pleistocene Somssich Hill 2 locality (Villány Hills, South Hungary) and its palaeoecological implications. Fragmenta Palaeontologica Hungarica 31: 51-81, DOI: 10.17111/FragmPalHung.2014.31.51, URL: https://doi.org/10.17111/fragmpalhung.2014.31.51
