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This lowstand occurs quasi at the same time as the end of a longer lowstand in the Black Sea.
The freshest waters are then inferred as having occurred between 8.4 and ≤4.4 cal.
ka BP, linked to a connection with the Amu Darya and the melting glaciers on the Pamir Mountains.
This place is situated in Allerod, Frederiksborg, Denmark, its geographical coordinates are 55° 52' 0" North, 12° 23' 0" East and its original name (with diacritics) is Allerød.
See Allerod photos and images from satellite below, explore the aerial photographs of Allerod in Denmark.
During the 20th century, CS water levels have fluctuated rapidly, a hundred times faster than recent global sea level, causing serious environmental and economic damage and adversely affecting oil and gas exploitation, agriculture and fishing as well as causing major risks in areas for storage of nuclear waste. 1B: Location map of the cores and the main inflows to the Caspian Sea. Grey lines are rivers, continuous line for permanent, dashed line for temporary. (For interpretation of the references to colour in this figure legend, the reader is referred to the web version of this article.)The impact of water level changes was especially strong in low-lying areas.
Instrumental records (since 1837) indicate a 3 m change with a sharp drop between 1930 (−26 m) and 1977 (−29 m), followed by a sharp rise until 1995 (−26.5 m) (Leroy et al., 2006 ; USDA, 2013). The horizontal changes were the most pronounced in the north basin with the Volga delta wandering north–south up to 700 km along its riverbed in the last climate cycle (Kroonenberg et al., 1997 ; Tudryn et al., 2013) (C ka BP) of possibly lower than −110 m (Rychagov, 1997 ; Chepalyga, 2007).
Pollen and dinoflagellate cysts have been analysed in a core from the south basin of the Caspian Sea, providing a picture of respectively past vegetation and water salinity for the Late Pleistocene to middle Holocene.