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(Table DR3) Foraminiferal oxygen and carbon isotope data for DSDP Site 62-463
Benthic foraminifera include species of Nuttalides and Gavelinella. All other species listed are planktic foraminifera. All other species listed are planktic foraminifera.... -
(Table 1) Concentrations of platinum-group elements and rhenium in sediments ...
Concentrations are given for dry sediments. -
(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 3, part d) Trace element contents in chert and associated host sedimen...
This dataset has no description
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(Table 1, part d) Major element contents in chert and associated host sedimen...
This dataset has no description
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(Tab. 15) Distribution of benthic foraminifera in Lower Cretaceous sediments ...
A = abundant, C = common, R = rare, - = absent. Samples 62-463-71-3,53-55, 62-463-79-1,34-35 radiolarians, samples 62-463-59-2, 62-463-59-CC, 62-463-70-1,41-42,... -
(Table 2) Geochemistry and acculumation rates of DSDP Hole 62-463
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. -
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 DR1) Biogenic silica and chert in the Pacific Ocean, DSDP and ODP data
Evidence for the dissolution of biogenic silica at the base of pelagic sections supports the hypothesis that much of the chert formed in the Pacific derives from the dissolution... -
Trace element abundance, and Sr and Nd isotope ratios of dust samples in the ...
Eolian dust preserved in deep-sea sediment cores provides a valuable indicator of past atmospheric circulation and continental paleoclimate. In order to identify the provenance... -
(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... -
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... -
Benthic foraminiferal number of specimens in Cretaceous samples of various DS...
Benthic foraminifera from 24 DSDP/ODP sites were investigated to assess their global horizontal and vertical distribution in the deep-sea environment at the end of the... -
Chemistry and accumulation rates of Jurassic to early Cretaceous sediments fr...
Sedimentation in the central Pacific during the Jurassic and Early Cretaceous was dominated by abundant biogenic silica. A synthesis of the stratigraphy, lithology, petrology,... -
Chemical composition of bottom sediments and rocks from DSDP Holes 3-14 throu...
Data on analyses of chemical composition of DSDP samples of bottom sediments and rocks carried out in P.P. Shirshov Institute of Oceanology are reported. Basal sediments and... -
Paleoelevations in the Pacific Ocean 35 million years ago
Data from deep sea drilling, linear magnetic anomalies and bathymetric measurements together with age and morphometric characteristics of seamounts have been used to construct a...
