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doi:10.2204/iodp.proc.329.202.2015
Data report: radiolarian occurrences at IODP Expedition 329 Site U13711
Giuseppe Cortese2 and Carlos A. Alvarez Zarikian3
Abstract
In this report we present a radiolarian biostratigraphy for the uppermost 108 m recovered during Expedition 329 at Integrated Ocean Drilling Program Site U1371.
This interval of clay-bearing diatom ooze contains well-preserved remains of siliceous microfossils. Below 108 meters below seafloor (mbsf), the sediment lithology changes to zeolitic clay, which does not contain any biosiliceous material.
Twenty-eight radiolarian marker species, used as age-indicative taxa in both middle- and high-latitude radiolarian biozonation schemes, have been recognized at this location and allow age control for the uppermost ~100 m of the cored section, with an estimated age of 8.2 Ma at 101.4 mbsf. These results match well those from a parallel study based on diatom biostratigraphy.
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