Development and application of an electrical conductivity transfer function, using diatoms from lakes in the Urals, Russia
Author:
Funder
Russian Science Foundation
State Contract
Publisher
Springer Science and Business Media LLC
Subject
Earth-Surface Processes,Aquatic Science
Link
http://link.springer.com/content/pdf/10.1007/s10933-019-00106-z.pdf
Reference60 articles.
1. Andreeva MA (1973) Ozera Srednego i Juzhnogo Urala (Middle and Southern Urals lakes). Southern Urals Books Press, Chelyabinsk (in Russian)
2. Appleby PG, Oldfield F (1978) The calculation of lead–210 dates assuming a constant rate of supply of the unsupported lead–210 to the sediment. CATENA 5:1–8. https://doi.org/10.1016/S0341-8162(78)80002-2
3. Birks HJB (1998) Numerical tools in palaeolimnology—progress, potentialities, and problems. J Paleolimnol 20:307–332. https://doi.org/10.1023/A:1008038808690
4. Birks HJB, Line JM, Juggins S, Stephenson AC, ter Braak CJF (1990) Diatoms and pH reconstruction. Philos Trans R Soc Lond B Biol Sci 327:263–278. https://doi.org/10.1098/rstb.1990.0062
5. Blaauw M, Christen AJ (2011) Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Anal 6(3):457–474. https://doi.org/10.1214/11-BA618
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