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doi:10.2204/iodp.proc.342.204.2016
Data report: relative abundance of benthic foraminiferal morphotypes across the Eocene/Oligocene and
Oligocene/Miocene boundaries (IODP Expedition 342 Site U1406, North Atlantic)1
Kazuyoshi Moriya2 and Oliver Friedrich3
Abstract
Relative abundances of five benthic foraminiferal morphotype groups (i.e., agglutinated, elongated, planispiral, tapered, and trochospiral) from the late Paleocene to early Miocene at Site U1406 (Integrated Ocean Drilling Program Expedition 342) are reported. Benthic foraminiferal tests from Site U1406 are generally very well preserved and occur abundantly from the late Eocene through middle Oligocene; they are less abundant for the remainder of the studied interval. Among the five morphotypes identified in this study, tapered and trochospiral forms are the dominant groups. Thereby, tapered morphotypes show increasing abundances at and above the Eocene/Oligocene and Oligocene/Miocene boundaries. Agglutinated and planispiral morphotypes are minor components throughout the studied interval. Relative abundances of the elongated morphotype abruptly increase during the lower Eocene. This increase can be correlated to a distinct decrease in carbonate content between lithostratigraphic Units III and IV.
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