(ostracodes, latest Permian (Changhsingian), taxonomy, stratigraphy, Vardar Zone, Jadar Block, NW Serbia)
PANTIĆ-PRODANOVIĆ(1979) mentioned “Campilian” ostracodes in the vicinity of Valjevo, and KRSTIĆ (1980) reported the ostracode fauna of the same age from the Gučevo Mt.The ostracodes described and illustrated hereinwere foundwith stylolites; 4b,laminated limestones; 5,conodonts; 6,foraminifers; 7,ostracodes; 8,wackestone; 9,packstone; 10,fault.foraminifers, algae, ostracodes, conodonts, holothurian sclerites, crinoids, echinoids, brachiopods, gastropods
gastropods, algae, foraminifers, etc.), and a poor LowerTriassic microfossil association (foraminifers, ostracodes) have been determined.During long-term geological investigations, particularly in NW Serbia, the Serbian
(Lower Triassic, Olenekian, conodonts, ostracodes, pyrite framboid, Jadar Block, North-western Serbia)
published only fewpapers dealing with ostracodes: PANTIĆ-PRODANOVIĆ(1979), KRSTIĆ (1980) and CRASQUIN et al. (2010). Inpaper of PANTIĆ-PRODANOVIĆ (1979), only five species of ostracodes were cited (three in open nomenclature)2011). Paracypris ? krivipotokensis FOREL n. sp.is the first record of Smithian ostracodes on the northMILAN N. SUDAR et al.10Fig. 6. Ostracodes from the Krivi Potok Section, Gučevo Mt., Jadar Block, NW Serbia; middle part
1980. The Lower Triassic ostracodes of Gučevo.Zapisnici Srpskog geološkog društva za 1979 godinu(Vanredni zbor 24. I 1980), 203–208 (in Serbo-Croatian,English summary).LETHIERS, F. 1981. Ostracodes du Dévonien terminal del’Ouest