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Paleothermometer information


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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Paleothermometer

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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...

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TEX86

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TEX86 is an organic paleothermometer based upon the membrane lipids of mesophilic marine Nitrososphaerota (formerly "Thaumarchaeota", "Marine Group 1 Crenarchaeota")...

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Marine isotope stages

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is unaffected) Timeline of glaciation Geologic temperature record Paleothermometer Anthropocene Marine terrace Ice core Pettitt and White date MIS3 as...

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Glycerol dialkyl glycerol tetraether

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history. Some structural forms of GDGT form the basis for the TEX86 paleothermometer. Isoprenoid GDGTs, now known to be synthesized by many archaeal classes...

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Crenarchaeol

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hundreds of millions of years in the environment. It is part of the TEX86 paleothermometer, a temperature proxy for sea surface temperatures that has been used...

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Glossary of climate change

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circulation The global density-driven circulation of the oceans. TEX-86 A paleothermometer based on the composition of membrane lipids of the marine picoplankton...

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Younger Dryas

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powerful paleothermometer for the quantitative reconstruction of past continental climates.[page needed] The application of alkenone paleothermometers to high-resolution...

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Index of climate change articles

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Thermal Maximum - Paleoclimate Modelling Intercomparison Project - Paleothermometer - Parameterization - Planetary engineering - Peak oil - Phenology -...

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Marine Isotope Stage 5

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Summer Monsoon (ISM) declined in overall intensity. Meltwater pulse 1A Paleothermometer Proxy (climate) Timeline of glaciation Medley, S. Elizabeth (2011)...

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Paleoclimatology

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geological past Paleoceanography – Study of the oceans in the geologic past Paleothermometer – Study of ancient temperatures Paleohydrology – Study of hydrology...

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Magnesite

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(2006-03-15). "13C–18O bonds in carbonate minerals: A new kind of paleothermometer". Geochimica et Cosmochimica Acta. 70 (6): 1439–1456. Bibcode:2006GeCoA...

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Isotopologue

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Prosenjit, et al. "13C–18O bonds in carbonate minerals: A new kind of paleothermometer". Geochimica et Cosmochimica Acta 70.6 (2006): 1439–1456. Young E....

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Mono Lake

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RP (2001). "Ikaite, CaCO3· 6H2O: Cold comfort for glendonites as paleothermometers". American Mineralogist. 86 (11–12): 1530–1533. Bibcode:2001AmMin...

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Conodont

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widely used in biostratigraphy. Conodont elements are also used as paleothermometers, a proxy for thermal alteration in the host rock, because under higher...

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Clumped isotopes

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16O2−) are not completely standardized between labs. δ18O δ15N δ13C Paleothermometer Isotopic signature Isotope analysis Isotope geochemistry Isotopic labeling...

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Thermal history of Earth

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Geologic temperature record List of periods and events in climate history Paleothermometer Radiative forcing Timeline of glaciation Olson, P. (24 October 2013)...

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Marine Isotope Stage 11

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absence of anthropogenic forcing.[citation needed] Meltwater pulse 1A Paleothermometer Proxy (climate) Timeline of glaciation Lisiecki,Lorraine E.; Raymo...

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Amorphous calcium carbonate

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proxies. For example, the calibrations of the clumped 13C-18O carbonate paleothermometer and understanding the origins and evolution of skeletal structures...

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Cool tropics paradox

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temperature around 4–5° warmer than today's. The magnesium/calcium paleothermometer is a recently developed alternative to the δ18O method, and avoids...

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Equilibrium fractionation

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isotope effects) forms the basis of the most widely used isotopic paleothermometers (or climate proxies): D/H and 18O/16O records from ice cores, and...

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Aradhna Tripati

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of its use in the field. She helped develop a technique known as a "paleothermometer," which allows scientists to measure past temperatures by analyzing...

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Reference materials for stable isotope analysis

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John M. (2006). "13C–18O bonds in carbonate minerals: A new kind of paleothermometer". Geochimica et Cosmochimica Acta. 70 (6): 1439–1456. Bibcode:2006GeCoA...

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