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(Table 2) Stable isotope ratios of Uvigerina sp. and planktonic foraminifera ...
This dataset has no description
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(Table 3) Rare earth and trace element contents in DSDP and ODP cherts
This dataset has no description
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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 -
(Table 1) Estimated age for the last occurrence of Globoquadrina dehiscens
Ages were transfered to the timscale of Berggren et al. (1995) -
(Table 2) Planktonic foraminiferal datum levels and paleoclimatic events of D...
This dataset has no description
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(Tab. 14) Distribution of benthic foraminifera in Lower Cretaceous sediments ...
A = abundant, C = common, R = rare, - = absent. Samples 32-307-8-CC, 32-307-9-CC, 32-307-12-CC no microfossils -
(Tab. 13) Distribution of benthic foraminifera in Lower Cretaceous sediments ...
A = abundant, C = common, R = rare, - = absent. Sample 32-306-1-CC contaminated with quaternary foraminifera, samples 32-306-6-CC, 32-306-10-1,64-66, 32-306-10-CC, 32-306-12-CC,... -
(Tab. 12) Distribution of benthic foraminifera in Lower Cretaceous sediments ...
A = abundant, C = common, R = rare, - = absent. -
(Tab. 11) Distribution of benthic foraminifera in Lower Cretaceous sediments ...
A = abundant, C = common, R = rare, - = absent. Lithology: nannofossil chalk and chert. Samples 32-304-3-CC, 32-304-7-CC, 32-304-8-CC, 32-304-12-1,25 no microfossils -
(Tab. 10) Distribution of benthic foraminifera in Lower Cretaceous sediments ...
A = abundant, C = common, R = rare, - = absent. Lithology: multicoloured pelagic claystone and chert. Sample 32-303A-3-CC no microfossils -
(Table 2) Geochemistry and acculumation rates of DSDP Hole 32-310
Age based on nannofossil biostratigraphy by Worsley for this study, documented in Chaboudy (1984) -
(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. -
Annotated record of the detailed examination of Mn deposits from DSDP Leg 32 ...
The northwestern Pacific Ocean is the largest expanse of old oceanic lithosphere, and so the principal theme of Leg 32 set by the Pacific Advisory Panel was the late Mesozoic... -
(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 1) Stabile isotopes at DSDP Leg 55 Holes
Deep sea drilling on four seamounts in the Emperor Seamount chain revealed that Paleogene shallow-water carbonate sediments of the "bryozoan-algal" facies crown the basalt... -
(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... -
(Table 1) Stable oxygen isotope ratios of benthic foraminifera from Pacific O...
The thermal structure of the Pacific Ocean between water depths of about 1 and 4.5 kilometers is estimated from the oxygen isotopic ratio of benthonic foraminifera from... -
Major- and trace-element analyses of cherts, porcellanites, oozes, and clays ...
Analyses of 42 Cretaceous rock samples from Deep Sea Drilling Project (DSDP) Leg 32, in the northern Pacific, show that chert and porcellanite are enriched in Fe, Mn, P, Cu, Ba,... -
Geochemical analyses of chert nodules and beds from deep-sea sediments (Table 1)
Concentrations of Fe, Mg, Ca, Sr, Mn, Zn, and other heavy metals were analyzed by atomic absorption spectrometry in 27 chert samples from the Pacific deep sea, 17 chert samples... -
(Table 3) Aeolian component of North Pacific pelagic sediments
Isolation and analysis of the eolian component of late Cenozoic pelagic sediments from the North Pacific provides direct information concerning changes in atmospheric...
