Pregled bibliografske jedinice broj: 211414
Geochemical and isotopic variations in recent freshwater carbonates in Krka river, Croatia : implication for climate reconstruction.
Geochemical and isotopic variations in recent freshwater carbonates in Krka river, Croatia : implication for climate reconstruction. // VIII Isotope Workshop: extended abstract volume / STRAUCH, Gerhard, WEISE, Stephen M. (ur.).
Leipzig: Leipzig: UFZ Centre for Environmental Research, Department of Hydrogeology, Department of Isotope Hydrology, 2005. str. 161-164 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
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Naslov
Geochemical and isotopic variations in recent freshwater carbonates in Krka river, Croatia : implication for climate reconstruction.
Autori
Lojen, Sonja ; Oudane, Baghdad ; Vokal, Barbara ; Papesch, Wolfgang ; Cukrov, Neven ;
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
VIII Isotope Workshop: extended abstract volume
/ STRAUCH, Gerhard, WEISE, Stephen M. - Leipzig : Leipzig: UFZ Centre for Environmental Research, Department of Hydrogeology, Department of Isotope Hydrology, 2005, 161-164
Skup
VIII Isotope Workshop
Mjesto i datum
Leipzig, Njemačka, 25.06.2005. - 30.06.2005
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
climate reconstruction; Krka river; stable isotops; O; C; tufa
Sažetak
Environmental and climatic changes are potentially recorded in recent terrestrial carbonates, such as speleothems or tufas. Stromatolite-like crusts have been the subject of great interest since they contain mm-size laminae, which are considered to represent annual climatic records. The origin of the light and dark layers has been attributed to seasonal variations in microbial assemblages and their activities, water chemistry and carbonate precipitation rates. In conclusion, both oxygen isotope, as well as geochemical records in the laminar crust to a certain extent reflect the temperature and other environmental conditions during the period of precipitation. However, the exact estimation of the precipitation temperature is not yet possible.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA