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Orue-Etxebarria, X., Pujalte, V., Bernaola, G., Apellaniz, E., Baceta, J.I., Payros, A., Nu?ez-Betelu, K., Serra-Kiel, J. and Tosquella, J. (2001) Did the Late Paleocene Thermal Maximum Affect the Evolution of Larger Foraminifers? Evidence from Calcareous Plankton of the Campo Section (Pyrenees, Spain). Marine Micropaleontology, 41, 45-71. http://dx.doi.org/10.1016/S0377-8398(00)00052-9

has been cited by the following article:

• TITLE: Larger Benthic Foraminifera from the Paleocene Sediments in the Chehel-Kaman Formation, North-Eastern Iran

  AUTHORS: Batool Rivandi, Seyed Mohammad Ali Moosavizadeh

  KEYWORDS: Chehel-Kaman, Kopet-Dagh, Foraminifera, Paleocene, Ranikothalia sindensis Partial Zone

  JOURNAL NAME: Open Journal of Geology, Vol.5 No.4, April 27, 2015

  ABSTRACT: This study is the micropaleontological investigation of the Chehel-Kaman Formation of Paleocene age from Kopet-Dagh basin, NE of Iran. Thirty three species of diagnostic benthic foraminifers belonging to generaMiscellanea,Operculina,Lockhartia,Rotalia,Akbarina,Pseudocuvillerina,Smoutina,Davisina,Idalina,Valvulina,Laffitteina,andRanikothaliaare recorded based on detailed petrographic analysis. The rocks are entirely shallow marine in rigin with biotic assemblages confirming Chehel-Kaman Limestone of the Paleocene age. The analyses of benthic foraminifers suggest that the deposition of the Paleogene sequence occurs in warm and shallow marine environments. In this paperRanikothalia sindensispartial zone was reported in association withMiscellanea miscella,M. juliettaeandM. yvettae.