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(Table 4A) Trace element concentrations in high-latitude diatoms
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(Table 1) Two-way time, age and corrected ages of middle Miocene at DSDP site...
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(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma,...
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(Table 3) Percentage of diatom assemblages made up by Nitzschia spp. and Roux...
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(Table 2) Relative abundance of diatoms in middle Pliocene sediments of DSDP ...
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(Table 1) Age model of DSDP Hole 28-266 from the south flank of the Southeast...
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(Table 5) Relative abundance of pollen and spores in mid-Pliocene sediments o...
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(Table 2) Relative abundance of diatoms in mid-Pliocene sediments of DSDP Hol...
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(Table 1) Palynological investigation at DSDP Hole 28-274 north-northeast of ...
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Age model of DSDP Hole 28-267B
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Age model of DSDP Hole 28-266
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Age model of DSDP Hole 28-265
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(Table 2) Geochemistry and acculumation rates of DSDP Hole 28-266
Age based on downhole correlation from Berggren and van Couvering [1972] to Haq [1983] time scale -
Concentration and stable carbon isotopic composition of organic carbon of DSD...
The 7% carbon-13 depletion in cold water phytoplankton provides a striking signal that is traceable in deep-sea cores taken in high latitude regions of the Southern hemisphere.... -
Accumulation rates and Opal of Hole 28-266
This dataset has no description
