Results 21 to 30 of about 25,230 (195)
Origins of high δ18O in 3.7–3.6 Ga crust: A zircon and garnet record in Isua clastic metasedimentary rocks [PDF]
Elevated δ18O is used as a marker for the presence of continents and surficial alteration in the Eoarchean and Hadean. This study establishes a timeline for δ18O enrichment in Eoarchean metasedimentary rocks of the Isua supracrustal belt in Greenland ...
Gauthiez Putallaz, Laure +3 more
core +3 more sources
The climate significance of stalagmite δ18O values from the East Asian monsoon region are still under much debated during the past years. The bone of contention focuses on whether the stalagmite δ18O can reflect the summer monsoon intensity or summer ...
Jianjun Yin
doaj +1 more source
Characterization of spatiotemporal variation of the stable isotopes δ18O and δD in surface water is essential to trace the water cycle, indicate moisture sources, and reconstruct paleoaltimetry.
Ya-Ni Yan +7 more
doaj +1 more source
A novel salinity proxy based on Na incorporation into foraminiferal calcite [PDF]
Salinity and temperature determine seawater density, and differences in both thereby control global thermohaline circulation. Whereas numerous proxies have been calibrated and applied to reconstruct temperature, a direct and independent proxy for ...
Reichart, G.J. +16 more
core +3 more sources
Príspevok syntetizuje dostupné údaje o izotopickom zložení zrážok na území Slovenska (Západné Karpaty). Hodnotí koreláciu hodnôt δ18O v kumulatívnych mesačných zrážkach z rokov 1988-1997 medzi jednotlivými stanicami, vplyv nadmorskej výšky, teploty ...
Holko Ladislav +3 more
doaj +1 more source
The origin of high δ18O zircons: marbles, megacrysts, and metamorphism [PDF]
The oxygen isotope ratios (δ18O) of most igneous zircons range from 5 to 8‰, with 99% of published values from 1345 rocks below 10‰. Metamorphic zircons from quartzite, metapelite, metabasite, and eclogite record δ18O values from 5 to 17‰, with 99% below
J. Valley (23314189) +5 more
core +2 more sources
Modulated orbital cycles in planktonic foraminifera δ18O
Measurements of δ18O on planktonic foraminifera represent an important geological archive. In the study of climate change on orbital time-scales, δ18O is used either as a proxy for temperature change, to construct age models through pattern matching, to ...
Roche, Didier; id_orcid +3 more
core +1 more source
In the East Asian monsoon area, stalagmites generally record lower and higher oxygen isotope (δ18O) levels during warm humid interglacial and cold dry glacial periods, respectively.
Shota Amekawa +8 more
doaj +1 more source
Interpretation of Oxygen Isotopes in Phanerozoic Ophiolites and Sedimentary Rocks
Two reactive transport models were developed to integrally simulate fluxes of oxygen isotopes from hydrothermal alteration of oceanic crust and weathering of continental rocks for a better understanding of the regulation of oxygen isotopes in the ocean ...
Yoshiki Kanzaki
doaj +1 more source
Oxygen isotopic compositions (δ18O) of benthic foraminifer tests are widely used for reconstructing paleoceanographic changes, such as global ice volumes during glacial–interglacial cycles.
Minoru Ikehara +3 more
doaj +1 more source

