Paleotemperature proxies

Lauritzen S-E (1993) Natural errvirorrmental change in karst The qrratemary record. Catena Supp 25 21-40 Lauritzen S-E (1995) High-resolution paleotemperature proxy record for the last interglaciation based on Norwegian speleothems. Quat Res 43 133-146... [Pg.456]

Figure 17. Plot of Li isotopic composition vs. temperature of growth for synthetic calcite crystallized from a solution containing Li from L-SVEC (Marriott et al. 2004). The results are most consistent with temperature not being a significant control on mass fractionation of Li during crystallization from aqueous solution, thus essentially eliminating Li isotopes as a paleotemperature proxy in marine carbonates.

$Figure 17. Plot of Li isotopic composition vs. temperature of growth for synthetic calcite crystallized from a solution containing Li from L-SVEC (Marriott et al. 2004). The results are most consistent with temperature not being a significant control on mass fractionation of Li during crystallization from aqueous solution, thus essentially eliminating Li isotopes as a paleotemperature proxy in marine carbonates.$

Cohen A., Layne G., Hart S., and Lobel P. (2001) Kinetic control of skeletal Sr/Ca in a symbiotic coral implications for the paleotemperature proxy. Paleoceanography V16(N1), 20-26. [Pg.3233]

Lauritzen, S.-E., 1995, High-Resolution Paleotemperature Proxy Record for the Last Interglaciation Based on Norwegian Speleothems, Quaternary Research, 43 133-146. [Pg.302]

Hastings, D. W., Russell, A. D. Emerson, S. R. 1998. Foraminiferal magnesium in Globigerinoides sacculifer as a paleotemperature proxy. Paleoceanography, 13, 161-169. [Pg.70]

Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...