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Thermal conductivity of IODP Hole 318-U1355A
Geocode = Depth CSF-A (m) -
Reflectance spectroscopy and colorimetry from IODP Hole 318-U1355A
Geocode = Depth CSF-A (m) -
P-Wave velocity (PWL) from IODP Hole 318-U1355A
Geocode = Depth CSF-A (m) -
Natural gamma radiation from IODP Hole 318-U1355A
Geocode = Depth CSF-A (m) -
Point measurements of magnetic susceptibility from IODP Hole 318-U1355A
Geocode = Depth CSF-A (m) -
Pass-through measurements of magnetic susceptibility from IODP Hole 318-U1355A
Geocode = Depth CSF-A (m) -
Core summary for IODP Hole 318-U1355A
This dataset has no description
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XRD raw data from IODP Exp318
This dataset has no description
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Palynological counts from the Oligocene-Miocene of IODP Site 318-U1356, Wilke...
Palynological counts from IODP Leg 318 Hole U1356A, Cores 95R-11R, and the lithological facies as observed in Salabarnada et al., CP 2018. Reworked dinocysts (as by Bijl et al.,... -
Major, trace element and XRF data for sediments and fish tooth samples, from ...
Fossil fish teeth from pelagic open ocean settings are considered a robust archive for preserving the neodymium (Nd) isotopic composition of ancient seawater. However, using... -
Sporomorphs and quantitative analysis of the Eocene record from IODP Hole 318...
The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was characterized by an expansion of near-tropical vegetation belts into the... -
Pollen and spores, calculated temperature and precipitation of IODP Hole 318-...
The warmest global climates of the past 65 million years occurred during the early Eocene epoch (about 55 to 48 million years ago), when the Equator-to-pole temperature... -
Global shallow sediment diagenesis survey results based on all available IODP...
Global shallow sediment diagenesis survey results based on all available IODP sediment core images.
