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Extractions and analyses of reactive phosphorus in the Bering Sea from IODP H...
To reconstruct the cycling of reactive phosphorus (P) in the Bering Sea, a P speciation record covering the last ~ 4 Ma was generated from sediments recovered during Integrated... -
(Table II, page 668-669) Distribution of elements between minerals soluble in...
Attempts to classify pelagic sediments have been based either on appearance and composition, or on the ultimate origin of the components. In particular it appears feasible to... -
Late Pliocene and early Pleistocene rock-magnetic record of IODP Site 306-U13...
Knowledge of the evolution of North Atlantic Deep Water (NADW) is key to understanding the past evolution of the climatic system. We developed a new rock-magnetic method to... -
Micro-granulometry of sedimentary dykes, Kathmandu basin, Nepal, supplement t...
Soft-sediment deformation structures have been analyzed at six sites of the Kathmandu valley. Microgranulometric study (this Supplement and Fig. 3B of Mugnier et al.,... -
(Table A1) Isotopic ratios of Sr, Nd, and Pb for sediments in ODP Leg 138 sit...
The provenance of eolian dust supplied to deep-sea sediments has the potential to offer insights into changes in past atmospheric circulation. Specifically, measuring temporal... -
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,...