“…Relatively low lake levels can further be identified by horizons enriched in molluscs, which are confined to the photic zone because they are feeding on algae (Sapozhnikov et al, 2009). They can therefore be used for tracing either later regressive or early transgressive phases (Fig.…”
Section: Lithofacies: a Tool For Tracing The Lake-level Historymentioning
“…Relatively low lake levels can further be identified by horizons enriched in molluscs, which are confined to the photic zone because they are feeding on algae (Sapozhnikov et al, 2009). They can therefore be used for tracing either later regressive or early transgressive phases (Fig.…”
Section: Lithofacies: a Tool For Tracing The Lake-level Historymentioning
“…3). Diatoms that are generally considered to be oligohalobous (C. placentula, N. fonticola) and are frequently used as indicators of low salinity presently occur in the Aral Sea at salinities exceeding 100 ‰ (saPozhnikov et al 2009). Therefore, their abundance may be controlled by factors other than salinity.…”
Section: Diatom Assemblage Changesmentioning
confidence: 99%
“…The salinity range of this species is wide, e.g. its reported optimum varies from saPozhnikov et al 2009). High abundances of Navicula digitoradiata (GreGory) ralfs (Fig.…”
Section: Diatom Assemblage Changesmentioning
confidence: 99%
“…This species is mainly abundant when the sediment contains a very high diatom concentration that point to a relatively low dissolution rate of the frustules within the water column. Although A. octonarius is a marine diatom it was a dominant species in the Aral Sea in 1960(mirabdullayev et al 2004). saPozhnikov et al (2009 pointed to the dependence of diatom assemblage composition on water depth.…”
Section: Interpretation Of the Diatom Recordmentioning
confidence: 99%
“…1 to more than 100 ‰ (saPozhnikov et al 2009) in the Western Basin. At least from 1853 until 1961, the Aral Sea had been a relatively stable water body with secular variations of the water level less than 3 m (kawabata et al 1997).…”
This study assesses changes in the environmental conditions in Chernyshov Bay (northern part of Aral Sea Western Basin) during the last ~2 ky from geochemical and diatom analyses of sediment core C2/2004. Comparison of fossil assemblages with the contemporary distribution of diatoms in the Aral Sea suggests that considerable changes occurred in water level as well as salinity. Deposits with high diatom concentrations and dominance of the marine species Actinocyclus octonarius ehrenberG are interpreted as periods of high water level, whereas replacement by Tryblionella compressa (bailey) boyer is considered to indicate lake level fall. On the other hand sediments with low diatom concentration represent higher freshwater input and therefore salinity decrease. This interpretation is supported by estimates of siliciclastic and chemogenic sediment components. A chronology of major lake stages is derived and roughly agrees with recent findings from other studies.
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