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Tropical Pacific late Cenozoic Iodine/Calcium from planktic foraminifera spec...
We apply the Iodine to Calcium (I/Ca) ratio in planktic foraminifera to reconstruct oceanic oxygen across the late Cenozoic. The data includes I/Ca ratios from planktic... -
Plio-Pleistocene planktic foraminifera oxygen and carbon stable isotopes at e...
Stable carbon and oxygen isotope data from two species of planktic foraminifera (Trilobatus sacculifer and Neogloboquadrina dutertrei) are obtained for eastern equatorial... -
Standardized and compiled marine paleoproductivity records across the late Mi...
This dataset represents a compilation of globally distributed paleoproductivity proxy records, mainly derived from low latitudes. It includes standardized and compiled records... -
Smoothed Cenozoic sea-level relative to modern from deep-sea geochemical and ...
We use published Pacific benthic foraminiferal oxygen isotope data and Mg/Ca records to derive a Cenozoic (66 Ma) global mean sea level (GMSL) estimate. This paper is novel in... -
Cenozoic sea-level relative to modern from deep-sea geochemical and continent...
We use published Pacific benthic foraminiferal oxygen isotope data and Mg/Ca records to derive a Cenozoic (66 Ma) global mean sea level (GMSL) estimate. This paper is novel in... -
δ¹⁸O and δ¹³C record of Paragloborotalia siakensis and Dentoglobigerina venez...
Knowledge of the equatorial thermocline is essential for understanding climate changes in the tropical Pacific. Multispecies planktic foraminiferal analyses provide a way to... -
Analysis of the middle Miocene climate transition from different Holes of IOD...
The middle Miocene climate transition (MMCT) is characterized by an abrupt 1‰ increase in benthic foraminiferal oxygen isotopes at ca. 13.8 Ma, marking expansion of the... -
Minor element ratios of Globorotalia tumida and subsurface temperature recons...
The equatorial Pacific thermocline is a critical component in determining the ocean-atmosphere interactions of the tropics. During the Pliocene warm period, the tropical... -
(Table T1) Scanning electron microscope (SEM) analyses of IODP Site 321-U1338
The late Miocene to early Pliocene carbonate-rich sediments recovered at Integrated Ocean Drilling Program (IODP) Site U1338 during the Expedition 320/321 Pacific Equatorial Age... -
Core summary for IODP Hole 321-U1338D
This dataset has no description
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Magnetic remanence from IODP Hole 321-U1338C
Geocode = Depth CSF-A (m) -
Reflectance spectroscopy and colorimetry from IODP Hole 321-U1338C
Geocode = Depth CSF-A (m) -
P-Wave velocity (PWL) from IODP Hole 321-U1338C
Geocode = Depth CSF-A (m) -
Natural gamma radiation from IODP Hole 321-U1338C
Geocode = Depth CSF-A (m) -
Pass-through measurements of magnetic susceptibility from IODP Hole 321-U1338C
Geocode = Depth CSF-A (m) -
Gamma ray attenuation bulk density from IODP Hole 321-U1338C
Geocode = Depth CSF-A (m) -
Core summary for IODP Hole 321-U1338C
This dataset has no description
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Magnetic remanence from IODP Hole 321-U1338B
Geocode = Depth CSF-A (m) -
Reflectance spectroscopy and colorimetry from IODP Hole 321-U1338B
Geocode = Depth CSF-A (m) -
P-Wave velocity (PWL) from IODP Hole 321-U1338B
Geocode = Depth CSF-A (m)
