paleotemperature

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paleotemperature

[¦pāl·ē·ō′tem·prə·chər]
(geology)
The temperature at which a geologic process took place in ancient past.
The mean climatic temperature at a given time or place in the geologic past.
References in periodicals archive ?
Thermochronological methods; from palaeotemperature constraints to landscape evolution models.
Oxygen isotope and palaeotemperature records from six Greeland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and North GRIP.
Environmentally controlled variation in the structure and mineralogy of Patella granularis shells from the coast of southern Africa: implications for palaeotemperature assessments.
The palaeotemperature data based on the Ca/Mg ratio show the average value between + 15[degrees]C and + 17[degrees]C in the northern Timan section (samples 45/1 and 45/2) and + 19[degrees]C in the Central Urals section (sample 134/1) (Fig.
Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP.
A climatic model of the last glacial/ interglacial transition based on palaeotemperature and palaeohydrological evidence, in Vogel (ed.
Strontium isotope profile of the early Toarcian (Jurassic) oceanic anoxic event, the duration of ammonite biozones, and belemnite palaeotemperatures.