A systematic study of the middle-late Miocene rodents and lagomorphs (Mammalia) of Felsőtárkány 3 / 8 and 3 / 10 (Northern Hungary) with stratigraphical relations Author Hír, János Author Kókay, József text Geodiversitas 2010 2010-06-30 32 2 307 329 http://www.bioone.org/doi/abs/10.5252/g2010n2a5 journal article 10.5252/g2010n2a5 1638-9395 4688402 Myoglis meini Baudelot, 1965 MATERIAL EXAMINED. — See Table 8 for data and measurements. DESCRIPTION In the upper molars, the extra ridges between the anteroloph and protoloph are long. The anterior TABLE 9. — Data of the Myoxus vallesiensis (Agustí,1981) find from Felsőtárkány, Hungary. Locality No. inv. MMP Position L W Fig. FT 3/10 2007.121 m 2 1.97 2.0 6M TABLE 10.— Individual data of the Paraglirulus werenfelsi Engesser, 1972 finds from Felsőtárkány, Hungary.

Locality	No. inv. MMP Position		L	W	Fig.
FT 3/10	2007.176	M1	1.18	1.19	6J
FT 3/8	2007.225	M2	1.18	1.27	6K
FT 3/10	2007.89	d4	0.83	0.63
FT 3/10	2007.177	m2	1.36	1.20	6L

extra ridges are connected to the middle part of the anterior centroloph. Th e main ridges are merged in the protocone. In this, the FT 3/10 form differs from Myoglis ucrainicus Nesin & Kowalski, 1997 ( Nesin & Kowalski 1997 ) in which the main ridges of M1-2 are frequently not merged in the protocone region. COMMENTS The morphology of these teeth is similar to that of the material described by Baudelot (1965), Engesser (1972) and Nemetshek & Mörs (2003) as Myoglis meini . This species is already known in three other Felsőtárkány localities, i.e. FT 3/2, FF 2/3 and FF 2/7, as described by Hír (2003 , 2006 ). The material from the borehole Lövölde Square, Budapest , described by Kretzoi (1943) as “ Pentaglis földvárii ” should be included in this species.