Fig. 4 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran

Fig. 4 Microfacies of Late Maastrichtian Tarbur Formation. a Bioclastic wacke-/packstone with large benthic foraminifer Loftusia sp. and dasycladale Salpingoporella pasmanica Radoičić (transverse section, arrow and detailed view). Thinsection Rt 177-1. Scale bars: 1.0 mm and 0.3 mm (detail, right below). b Bioclastic wacke-/packstone with large benthic foraminifera (Dicyclina? sp.), and dasycladalean algae Salpingoporella pasmanica Radoičić (arrow) and Salpingoporella? sp. with tilted laterals.