MINERAL COMPOSITION OF SABAKTY LAKE SEDIMENTS a 294 cm
sediment profile of the Lake Sabakty, with the objectives of
understanding the geochemical
Late Holocene climate and environmental changes in Kamchatka inferred from the subfossil chironomid record chironomid record of TYL
sediments and late
Holocene events reconstructed from other sites and other proxies
Late Holocene climate and environmental changes in Kamchatka inferred from the subfossil chironomid record chironomid record of TYL
sediments and late
Holocene events reconstructed from other sites and other proxies
Control of wind strength and frequency in the Aral Sea basin during the late HoloceneChanging content of detrital input in laminated
sediments traced by XRF scanning and microfacies