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K. Takahashi and H. Okada, “The Paleoceanography for the Last 30.000 Years in the Southeastern Indian Ocean by Means of Calcareous Nannofossils,” Marine Micropaleontology, Vol. 40, No. 1-2, 2000, pp. 83-103. doi:10.1016/S0377-8398(00)00033-5

has been cited by the following article:

• TITLE: Miocene to Pliocene Paleoceanography of the Western Equatorial Pacific Ocean Based on Calcareous Nannofossils, ODP Hole 805B

  AUTHORS: Meutia Farida, Ryo Imai, Tokiyuki Sato

  KEYWORDS: Paleoceanography; Calcareous Nannofossils; Discoaster; Reticulofenestra; Nutricline; Thermocline

  JOURNAL NAME: Open Journal of Geology, Vol.2 No.2, April 25, 2012

  ABSTRACT: We describe in detail the Miocene to Quaternary paleoceanography of the western equatorial Pacific Ocean based on calcareous nannofossils of Hole 805B. The relative abundance of Discoaster which lived in the lower photic zone under the stable sea with nutricline and thermocline, decreased step by step at NN5/NN6 and NN10/NN11 boundaries. Al- though the size of Reticulofenestra which is strongly influenced by nutrient, increased five times throughout the section, it drastically decreased in NN4-5 zone, NN10, NN12, and in NN15/NN16 boundary. On the basis of the relationship between Discoaster abundance and Reticulofenestra size change, collapse of the stability of the sea surface in the west- ern equatorial Pacific Ocean progressed step by step throughout the Miocene to Quaternary.