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Interstitial water chemistry of Hole 44-392A, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 44-391C, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 44-391B, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 44-391A, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 44-390A, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 44-390, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 44-388A, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
(Table 1) Organic carbon and pyrolysis assay at DSDP Hole 76-534A and 44-391C
Sediment depth is given in mbsf. Pyrolysis was limited to samples with greater than 0.5 wt.% organic carbon. -
Stable isotope ratios of Maestrichtian foraminifera of DSDP Hole 44-390
This dataset has no description
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(Table 3) Stable isotope record of Cretaceous foraminifera from DSDP Hole 44-...
Mid-Cretaceous (Barremian-Turonian) plankton preserved in deep-sea marl, organic-rich shale, and pelagic carbonate hold an important record of how the marine biosphere responded... -
(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. -
(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... -
Compilation of global mid-Miocene opal distribution
This is a virtual data set that comprises several other real data sets. -
Geochemistry and geological ages for organic-rich black shales of the Quatern...
This dataset has no description
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Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes
Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
Strontium and oxygen isotope data for DSDP Hole 44-390A and ODP Leg 171 holes
Differences in regional responses to climate fluctuations are well documented on short time scales (e.g., El Niño-Southern Oscillation), but with the exception of latitudinal... -
Annotated record of the detailed examination of Mn deposits from DSDP Leg 44 ...
The western part of the North Atlantic Ocean holds clues to some of the most intriguing questions in marine geology. But because the geologic problems are many and varied, the... -
(Table 5) Quaternary paleoproductivity of organic carbon in oceans based on D...
By analogy with the present-day ocean, primary productivity of paleoceans can be reconstructed using calculations based on content of organic carbon in sediments and their... -
Depth, age, strontium isotopic ratios and trace elemental ratios of samples f...
Large variations exist between published mid-Cretaceous (late Barremian to early Turonian stages) seawater Sr-isotope stratigraphies; this has resulted in disparate...
