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(Table 1-2) Sample summary and major element contents in DSDP and ODP cherts
Contents are given on volatile free base -
(Data Set S1) Compiled benthic foraminiferal stable isotopic values
d13C_adj: carbon isotopic value adjusted to Cibicidoides equivalent.d18O_adj: oxygen isotopic value adjusted to Cibicidoides equivalent. -
Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
(Table 1) Oxygen and carbon isotopic values of benthic foraminifera from the ...
Stable isotopic data from benthic foraminifera indicate the occurrence of at least three deepwater masses in the late Maastrichtian ocean. Given mean oceanic d18Ow of -1.0 per... -
(Table 2) Location, age of accompanied sediments, chemical and Sr isotopic co...
Strontium isotopic compositions of acetic acid (HOAc) leachate fractions of eight manganese oxide deposits from the modern seafloor, and of twenty-one buried manganese nodules... -
Fossil manganese deposits buried within DSDP/ODP cores, Legs 1-126
Probable in-situ manganese deposits larger than 1 cm in diameter buried in ODP/DSDP cores were selected for study after examining previous descriptions of the manganese deposits... -
Chemical composition of DSDP and ODP cherts
Rare earth element (REE), major, and trace element abundances and relative fractionations in forty nodular cherts sampled by the Deep Sea Drilling Project (DSDP) and Ocean... -
Pacific Neogene carbonate accumulation rates
I have compiled CaCO3 mass accumulation rates (MARs) for the period 0–25 Ma for 144 Deep Sea Drilling Project and Ocean Drilling Program drill sites in the Pacific in order to... -
Isotopic composition of carbon and oxygen from Paleogene deposits of some Pac...
This dataset has no description
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Compilation of global mid-Miocene opal distribution
This is a virtual data set that comprises several other real data sets. -
Revised chronology of Neogene DSDP holes from the World Ocean
After nearly 30 years of growth in geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated. In this... -
Strontium isotope ratios of pore waters and planktonic foraminifera from DSDP...
A detailed record of the strontium-87 to strontium-86 ratio in seawater during the last 100 million years was determined by measuring this ratio in 137 well-preserved and... -
(Table S8) Re-Os analyses of sediment leaches and associated age corrections ...
This dataset has no description
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(Table S3) Calcium carbonate content in ODP Hole 113-690C and DSDP Site 86-577
Sediment depth is given in mbsf. Analysis of ODP Hole 113-690C samples at University of Hawai'i at Manoa, analysis of DSDP Site 86-577 samples at Woods Hole Institute. -
(Table 6) Revised Paleocene age model of DSDP Hole 86-577 in the western equa...
Stratigraphic occurrence of Event/Datum from Monechi (1985, doi:10.2973/dsdp.proc.86.110.1985), Bleil (1985, doi:10.2973/dsdp.proc.86.117.1985) reinterpreted herein, Aubry... -
(Table 5) Age estimates of the Paleocene section of DSDP Hole 86-577 in the w...
This dataset has no description
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(Table 1) 10 Beryllium and CaCO3 at DSDP Holes 86-576B, 86-576, and 86-578
Extension of the 10Be geochronology for deep-sea sediments beyond the limit of late Pliocene age found in published works has been attempted. The results obtained on sediments... -
Isotope measurements from late Paleocene - early Eocene of 5 cores from Atlan...
High-resolution stable carbon isotope records for upper Paleocene - lower Eocene sections at Ocean Drilling Program Sites 1051 and 690 and Deep Sea Drilling Project Sites 550... -
Magnetobiostratigraphy and stable isotope record of Paleocene sediments from ...
Surface and deep water circulation patterns in the eastern Indian Ocean during the Paleocene Epoch are inferred based on an integrated magnetobiostratigraphic and stable isotope... -
Ice-rafted debris flux in the North Pacific from core 86-580
This dataset has no description
