A paleothermometer is a methodology that provides an estimate of the ambient temperature at the time of formation of a natural material. Most paleothermometers are based on empirically-calibrated proxy relationships, such as the tree ring or TEX86 methods. Isotope methods, such as the δ18O method or the clumped-isotope method, are able to provide, at least in theory, direct measurements of temperature.
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| - Paleotermòmetre (ca)
- Paleotermómetro (es)
- Paleothermometer (en)
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| - Un paleotermòmetre és la metodologia per determinar les temperatures dels temps passats fent servir Proxydades que es troben en registres naturals com són els sediments, un nucli de gel, anells d'arbres o TEX86. (ca)
- Un paleotermómetro es un artilugio metodológico para determinar Tº del pasado usando proxy (símil), encontrados en registros naturales tales como sedimentos o muestras de hielo, o anillos de árboles (dendroclimatología). (es)
- A paleothermometer is a methodology that provides an estimate of the ambient temperature at the time of formation of a natural material. Most paleothermometers are based on empirically-calibrated proxy relationships, such as the tree ring or TEX86 methods. Isotope methods, such as the δ18O method or the clumped-isotope method, are able to provide, at least in theory, direct measurements of temperature. (en)
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| - Un paleotermòmetre és la metodologia per determinar les temperatures dels temps passats fent servir Proxydades que es troben en registres naturals com són els sediments, un nucli de gel, anells d'arbres o TEX86. (ca)
- Un paleotermómetro es un artilugio metodológico para determinar Tº del pasado usando proxy (símil), encontrados en registros naturales tales como sedimentos o muestras de hielo, o anillos de árboles (dendroclimatología). (es)
- A paleothermometer is a methodology that provides an estimate of the ambient temperature at the time of formation of a natural material. Most paleothermometers are based on empirically-calibrated proxy relationships, such as the tree ring or TEX86 methods. Isotope methods, such as the δ18O method or the clumped-isotope method, are able to provide, at least in theory, direct measurements of temperature. (en)
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