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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 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) -
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) 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... -
Isotopic composition of carbon and oxygen from Paleogene deposits of some Pac...
This dataset has no description
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(Table 1) Average aluminium accumulation rate at 40 DSDP Sites for the time i...
A six-fold increase in the rate of accumulation of Al in north and central Atlantic and Pacific Ocean sediments indicates vastly increased denudation of the continents during... -
(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... -
Stable carbon and oxygen isotope composition of Recent, Tertiary and Cretaceo...
Oxygen isotope analyses of Tertiary and Cretaceous planktic foraminifera indicate that species have been stratified with respect to depth in the water column at least since...