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ACME ACTION PAD F28B DRIVER
During Expeditions andcalcareous nannofossils, planktonic and benthic foraminifers, diatoms, and ostracods were studied in core catcher samples. Samples from acme action pad f28b sections were examined when a more refined age determination was necessary and when time permitted. Biostratigraphic events, mainly the first appearance datum FAD or base and last appearance datum LAD or top of the age-diagnostic species are tied to the geomagnetic polarity timescale GPTS of Gradstein et al. Calcareous nannofossil, diatom, and planktonic foraminiferal acme action pad f28b and scaled ages.
Calcareous nannofossil zonation was based on the schemes of Okada and Bukry and Martini Calibrated ages for bioevents are from Gradstein et al. The timescale of Gradstein et al. In this study, the subdivision of these geologic time acme action pad f28b was mostly based on recognition of these nannofossil bioevents. Table T2. Calcareous nannofossil events and scaled ages.
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Several species of the genus Gephyrocapsawhich are commonly used as Pleistocene biostratigraphic markers, often show a great range of variation in sizes acme action pad f28b other morphological features, causing problems in identification e. Size-defined morphological groups of this genus Young, ; Maiorano and Marino, ; Lourens et al. We acme action pad f28b Reticulofenestra asanoi from the similarly sized Pseudoemiliania lacunosa by the absence of slits on the shield Su, The LAD of Sphenolithus spp. Species concepts for other taxa mainly follow those of Perch-Nielsen and Bown Calcareous nannofossil samples were prepared using standard smear slide techniques.
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For samples from sandy sediments, suspended aliquots of acme action pad f28b raw sample were analyzed. A Hitachi TM tabletop scanning electron microscope SEM was used to confirm the presence of small forms such as Emiliania huxleyian important marker for the latest Pleistocene—Holocene. Preservation of nannofossils was defined as follows:. The planktonic foraminiferal zonation schemes of Blowand Berggren et acme action pad f28b. We also adopted the use of the LAD 0. The FAD of G. The age for the LAD of Globorotalia mutlicamerata 2. Table T3. Planktonic foraminiferal events and scaled ages.
Taxonomic concepts for Neogene and Paleogene taxa acme action pad f28b follow those of Kennett and Srinivasan and Bolli and Saunders Planktonic foraminifer species distribution and range charts are presented in each site chapter. Taxonomic assignments for benthic foraminifers follow Loeblich and TappanKaminski and Gradsteinand Holbourn et al. Paleodepth estimates were based on selected benthic foraminiferal taxa noted and described by van Morkhoven et al.
Sample preparation for foraminifer identification uses the same techniques for both planktonic and benthic foraminifers. Consolidated or lithified samples acme action pad f28b cut in pieces and crushed to pea size, to which a hydrogen peroxide solution was added. Some samples were rewashed by additional disaggregation with the hydrogen peroxide solution.
To avoid contamination of foraminifers between samples, the sieves were thoroughly cleaned between samples, placed into a sonicator for at least 15 min, and then carefully checked. In addition, mudline or hole top samples were acme action pad f28b from selected sites and analyzed for planktonic acme action pad f28b benthic foraminifers and ostracods. Selected microfossil specimens were also examined and imaged using the shipboard SEM. The total abundance of planktonic foraminifers was reported using the following categories:. Relative abundances were reported using the following categories:. Preservation of planktonic foraminifer assemblages was recorded using the following categories:.
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Ostracods were studied at selected sites when time was available. Sample preparation for ostracod examination and illustration followed the same techniques as for foraminifers. Ostracod taxonomic assignments follow Yang et al. Abundance of ostracods was noted using the following definitions:.
Ostracod preservation was estimated using the following definitions:. The taxonomy for diatoms studied during Expeditions and is taken largely from BurckleAkibaAkiba and YanagisawaBaldauf and IwaiBarron,and Barron et al.
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