Permian fusulinids from the Koryak Terrane, northeastern Russia, and their paleobiogeographic affinity

Middle-Late Permian (Murgabian-Djulfian) foraminifers of the northern Maku area (western Azerbaijan, Iran

“…pusilla Skinner, 1969 Figure Davydov et al, 1996), but it belongs yet to Dunbarula by the septal folding relatively intense at the poles and the deviation of juvenarium. Our material is relatively similar to D. pusilla, from the Midian of Turkey, but this one shows a stronger septal folding.…”

The Changhsingian foraminiferal fauna of a Neotethyan seamount: the Gyanyima Limestone along the Yarlung‐Zangbo Suture in southern Tibet, China

“…Thus, the occurrence of Parareichelina is considered to be a marker of their links. However, as summarized by Nestell and Nestell (2006), Parareichelina is also known from several localities in the Tethys and Panthalassa, including the northwestern Caucasus (Miklukho-Maklay, 1954;Pronina-Nestell and Nestell, 2001), Sikhote-Alin (Sosnina, 1965), the Koryak area of eastern Siberia (Davydov et al, 1996), the Himalayas (Ladakh) (Lys et al, 1980), South China (Sheng, 1963) and northern California (Stevens et al, 1991). The occurrence of Parareichelina from the Gyanyima section marks the southernmost margin of its palaeogeographic distribution.…”

The marine Permian of East and Northeast Asia: an overview of biostratigraphy, palaeobiogeography and palaeogeographical implications

“…1). Davydov et al (1999) reported a highly diverse fusulinoidean fauna, represented by more than 65 species in 30 genera, from 12 separate limestone blocks (or olistostromes), all of which belong to the Ekonay Terrane (Sokolov, 1990). The diverse fusulinoidean fauna has been divided into five stratigraphic assemblages, respectively, representing the Asselian, Yakhotashian (or Artinskian), Bololrian (or Kungurian), Kubergandian (Roadian) and Midian (late Capitanian).…”