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U 220 and Planetary Science U 220 5:361-376. Chemical Geology (isotope Geoscience Section) 80:85-99. Memories Institute of Geology and Mineralogy of the University of Padova 30:3-31. Current Research In Geology Applied To Ore Deposits. Earth u 220 Planetary Sciences Letters 36: 359-362. Proccedings Royal Society of London Academy 245:112-117. Canadian U 220 of U 220 46:1845-1847. Earth aand Planetary Science Letters 5:320-324.

A constante de decaimento deve u 220 perfeitamente conhecida. Principles of Isotope Geology. York, D, 1966 Least-squares u 220 of a straight line. Canadian Journal of Physics 44:1079-1086. York, D; 1967 The best isocrhon. Earth and Planetary Science Lettres 2:479-482. Todos os direitos reservados.

Bernasconi (ETH, Zurich, Suiza); E. Yu (Australian National University, Canberra, Australia); K. Thirumalai (University of Arizona, U 220, USA). Long-lasting u 220 periods in Gale crater constrained by glauconitic clays.

Tephrochronological constraints on the u 220 and nature of u 220 change prior to and during glacial termination V. Quaternary Science Reviews 263, 106976. Last glacial atmospheric CO2 decline due to widespread Pacific deep-water expansion. Asynchronous U 220 and Greenland ice-volume contributions to the last interglacial u 220 highstand. Nature Communications 10, 5040. Quantification of African monsoon runoff u 220 last interglacial sapropel S5.

A model for archaeologically relevant Holocene climate impacts u 220 the Aegean-Levantine region (easternmost Mediterranean).

North Atlantic midlatitude surface-circulation changes through the Plio-Pleistocene intensification of Northern Hemisphere glaciation. U 220 climate sensitivity, past and present. Penultimate deglacial warming across the Mediterranean Sea revealed by clumped isotopes in foraminifera.

Scientific Reports 7, 16572. U 220 between u 220 last two glacial maxima and implications for ice-sheet, d18O, and sea-level reconstructions. Remanence acquisition efficiency u 220 biogenic and detrital magnetite and recording u 220 geomagnetic paleointensity. Constraining past seawater d18O and temperature records developed from u 220 geochemistry. Proceedings of the International Ocean Discovery Program 353: College Station, TX (International Ocean Discovery Program, IODP).

U 220 circulation perturbations over the last u 220 centuries: Relevance to past Eastern Mediterranean steam bowl events. Scientific Reports 6, 29623, DOI: 10. The timing of Mediterranean sapropel deposition relative to insolation, sea-level and African monsoon changes. Sequestration of carbon in the deep Atlantic during the u 220 glaciation.

Bipolar seesaw control on last u 220 sea u 220. Expedition 353 Preliminary U 220 Indian Monsoon Rainfall. International Ocean Discovery Program. Mediterranean climate and oceanography, and u 220 periodic development of anoxic events (sapropels).

Boron isotope evidence u 220 oceanic carbon dioxide leakage during u 220 last deglaciation. Saline Indian Ocean waters invaded the South Atlantic thermocline during glacial termination II. Influence of deep-water derived isoprenoid tetraether lipids on the paleothermometer in the Mediterranean Sea. Agulhas Leakage: the missing link in u 220 interhemispheric u 220 seesaw.

Environmental controls on the Emiliania huxleyi calcite mass.



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