4.0 Article

Middle Miocene to Pleistocene planktonic foraminiferal biostratigraphy in the eastern equatorial Pacific Ocean

Journal

PALEONTOLOGICAL RESEARCH
Volume 17, Issue 1, Pages 91-109

Publisher

PALAEONTOLOGICAL SOC JAPAN
DOI: 10.2517/1342-8144-17.1.91

Keywords

biostratigraphy; equatorial Pacific; IODP Exp 321; Middle Miocene to Pleistocene; planktonic foraminifera

Categories

Funding

  1. Integrated Ocean Drilling Program [330IODP]
  2. Japan Drilling Earth Science Consortium
  3. Center for Deep Earth Exploration
  4. CDEX
  5. Japan Society for the Promotion of Science [23740377]
  6. Grants-in-Aid for Scientific Research [23740377] Funding Source: KAKEN
  7. Natural Environment Research Council [NE/G014817/1, NE/G014817/2] Funding Source: researchfish
  8. NERC [NE/G014817/2, NE/G014817/1] Funding Source: UKRI

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We present a detailed dataset of planktonic foraminiferal biohorizons to enhance a biostratigraphy for the eastern equatorial Pacific. Middle Miocene to Pleistocene planktonic foraminiferal biostratigraphy is established using 269 samples from Cores 1H to 40H recovered from Integrated Ocean Drilling Program (IODP) Hole U1338B. In addition to the onboard study of Hole U1338A, a total of 60 biohorizons are recognized with three grades of reliability. Generally, these biohorizons are in agreement with each other and consistent with shipboard magnetostratigraphy, except for several discrepancies that may be caused by ecological diachronous processes. The studied sequence can be correlated with Zone M7 to Subzone PT1b. However, we cannot detect Miocene zones M6, M10, and M12 in this sequence because of discrepancies in some zonal marker biohorizons.

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