Кл.слова (ненормированные):
biogeochemistry -- halogen -- Holocene -- paleoclimate -- peatland -- proxy climate record
Аннотация: Na, Br, Cs, Ca, Mg, Ba, Cl and Br distribution along the profile of peatland in the process of peat accumulation is regulated by the climatic fluctuation during Holocene. The possibility of using this information for paleoclimate reconstruction has been shown. In all probability it can be considered as the biochemical migration of alkali-earth and alkaline metals in the process of peat formation reflects mainly climatic fluctuations, connected with temperature, and halogens - with moistening factor.
Scopus
Держатели документа:
Institute of Forest, Siberian Branch RAS, Novosibirsk, Russian Federation
Inst. of Chem. Kinetics/Combustion, Siberian Branch RAS, Novosibirsk, Russian Federation
United Institute of Nuclear Studies, Moscow, Russian Federation
Доп.точки доступа:
Efremova, T.T.; Efremov, S.P.; Kutzenogy, K.P.; Peresedov, V.F.