Fig. 5From: First record of ostracods from the Upper Ordovician red-coloured marine sandstones of the Tierekeawati Formation in Tarim Basin, NW China: implications on palaeoenvironment and palaeobiogeographyScanning electron micrographs of ostracods (II) from the Arisu red beds of the Tierekeawati Formation in Kalpin area, northwestern Tarim Basin, Northwest China. Scale bar is 100 μm. a Fenxiangia cf. puriformis Jiang, 1995 (Jiang et al. 1995). Left lateral view of complete carapace, 171094, Late Ordovician; b Rectella? cf. proposita Abushik and Sarv 1983. Left lateral view of complete carapace, 171095, Late Ordovician; c Anticostus jolieti (Copeland 1973). Left lateral view of complete carapace, 171096, Late Ordovician; d Bairdia cf. altitumida Wang 2015. Right lateral view of complete carapace, 171097, Late Ordovician; e Bairdia cf. altitumida Wang 2015. Dorsal view of complete carapace, 171098, Late Ordovician; f Bairdia cf. confragosa Jiang, 1995 (Jiang et al. 1995). Right lateral view of complete carapace, 171099, Late Ordovician; g Bairdia sp. Right lateral view of complete carapace, 171100, Late Ordovician; h Steusloffina cf. cuneata (Steusloff 1895). Left lateral view of complete carapace, 171101, Late OrdovicianBack to article page