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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 trace element ratios in biominerals and proxies from organic molecules.
Common paleothermometers & Overview
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temperature ca mg leaf species proxy ratio coral higher used sr trace element ratios isotopologues isotopes heavy high carbonate error
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Paleothermometer | is a | methodology that provides an estimate of the ambient temperature at the time of formation of a natural material | 0.90 | text |
| drip tips | instance of | shapes and prevalence of features | 0.80 | text |
| Paleothermometer | related to 13C-18O bonds in carbonates | There | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | The | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | Van | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | Hoff | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | Along | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | Carbonate | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | CO32 | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | CO2 | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | The CO2 | 0.60 | section |
| Paleothermometer | related to 13C-18O bonds in carbonates | Thus | 0.60 | section |
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