Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
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Oceanic minerals: their origin, nature of their environment, and significanceCovariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age.Ocean dynamics, not dust, have controlled equatorial Pacific productivity over the past 500,000 years.Multicentennial record of Labrador Sea primary productivity and sea-ice variability archived in coralline algal bariumBarium and its Importance as an Indicator of (Paleo)Productivity.Metals content in otoliths of Dicentrarchus labrax from two fish farms of Sicily.Volcanic perturbations of the marine environment in South China preceding the latest Permian mass extinction and their biotic effects.Pelagic barite precipitation at micromolar ambient sulfate.Two modes of change in Southern Ocean productivity over the past million years.Intensified deep Pacific inflow and ventilation in Pleistocene glacial times.Palaeoenvironment and its control on the formation of Miocene marine source rocks in the Qiongdongnan Basin, northern South China Sea.Quantifying export production in the Southern Ocean: Implications for the BaxsproxyAntarctic Zone nutrient conditions during the last two glacial cyclesLate Miocene–early Pleistocene paleoproductivity variations of the Lop Nor in the Tarim Basin and its implications on aridification in Asian InteriorCyclic magnetite dissolution in Pleistocene sediments of the abyssal northwest Pacific Ocean: Evidence for glacial oxygen depletion and carbon trappingReproducibility of Ba/Ca variations recorded by northeast Pacific bamboo coralsA 300 kyr high-resolution aridity record of the North African continentEquatorial Pacific productivity changes near the Eocene-Oligocene boundaryBarium-rich fluids and melts in a subduction environment (La Corea and Sierra del Convento mélanges, eastern Cuba)Centennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early HoloceneNitrogen isotope evidence for water mass denitrification during the Early Toarcian (Jurassic) oceanic anoxic eventPore water geochemistry along continental slopes north of the East Siberian Sea: inference of low methane concentrationsExport productivity and carbonate accumulation in the Pacific Basin at the transition from a greenhouse to icehouse climate (late Eocene to early Oligocene)Remanence acquisition efficiency in biogenic and detrital magnetite and recording of geomagnetic paleointensitySediment size fractionation and focusing in the equatorial Pacific: Effect on230Th normalization and paleoflux measurementsGeochemical evidence for enhanced productivity during S1 sapropel deposition in the eastern MediterraneanStable phytoplankton community structure in the Arabian Sea over the past 200,000 yearsSulphidic Mediterranean surface waters during Pliocene sapropel formationShort-time-scale variability in ventilation and export productivity during the formation of Mediterranean sapropel S1Temporal variability in the northern Arabian Sea oxygen minimum zone (OMZ) during the last 225,000 years
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Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
description
im April 1992 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована у квітні 1992
@uk
name
Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
@en
Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
@nl
type
label
Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
@en
Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
@nl
prefLabel
Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
@en
Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
@nl
P2093
P2860
P356
P1433
P1476
Barium in Deep-Sea Sediment: A Geochemical Proxy for Paleoproductivity
@en
P2093
Erwin Suess
Jack Dymond
Mitch Lyle
P2860
P304
P356
10.1029/92PA00181
P577
1992-04-01T00:00:00Z