Abstract
This paper presents a multi-proxy climate record of an 11 m long core collected in Lago Puyehue (southern Chile, 40°S) and extending back to 18,000 cal yr BP. The multi-proxy analyses include sedimentology, mineralogy, grain size, geochemistry, loss-on-ignition, magnetic susceptibility and radiocarbon dating. Results demonstrate that sediment grain size is positively correlated with the biogenic sediment content and can be used as a proxy for lake paleoproductivity. On the other hand, the magnetic susceptibility signal is correlated with the aluminium and titanium concentrations and can be used as a proxy for the terrigenous supply.
Original language | English |
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Pages (from-to) | 179-195 |
Number of pages | 17 |
Journal | Journal of Paleolimnology |
Volume | 39 |
Publication status | Published - 2008 |
Keywords
- Paleoclimate
- Lake record