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- W2046559938 abstract "The principle of isotope thermometry is that isotope ratios are temperature dependent. It is proposed that isotopic ratios in bio-organic material may have independent temperature coefficients, so that, by measuring ratios for several elements, e.g., hydrogen, carbon, and oxygen, it may be possible to show that a temperature change occurred. Assuming that cellulose is formed almost at equilibrium, temperature coefficients for C, H, and O are computed and found to be of measurable size. The coefficients computed for 13C/12C and D/H agree with measured values. Thus indications are that temperature changes in past climates can be measured in old tree rings by using this principle of multiple thermometers." @default.
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- W2046559938 date "1972-08-10" @default.
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- W2046559938 title "Multiple thermometry in paleoclimate and historic climate" @default.
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- W2046559938 doi "https://doi.org/10.1029/jb077i023p04310" @default.
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