Palaeolimnology of Lake Hess (Patagonia, Argentina): multi-proxy analyses in short sediment cores.

GUILIZZONI, PIERO , JULIETA MASSAFERRO, ANDREA LAMI, EDUARDO LUIS PIOVANO, SERGIO RIBEIRO GUEVARA, STELLA MARIS FORMICA, ROMINA DAGA ANDREA RIZZO & STEFANO GERLI

HYDROBIOLOGIA

Año: 2008

0018-8158

By contrast with the extensive palaeolimnological studies carried out North America and Europe, relatively few studies have described the anthropogenic and/or climate impacts in Patagonian lakes. We addressed these issues by analysing geochemistry, lithology, pigments and chironomid remains from sediment cores collected from Lake Hess (41° 22´ 20” S, 71° 44´ 0” W) located in the Nahuel Huapi National Park, in northern Patagonia. The aim of this study is to provide a palaeoenvironmental and climate reconstruction of the last ca. three centuries for this cold oligotrophic, quasi-pristine lake which receives melt waters from the Tronador ice cap. Chronology was based on 137Cs and 210Pb measurements of the upper sediments and the inferred sedimentation rate of 23.2 mg cm-2 y-1 (0.148 cm y-1) was consistent with both sets of measurements. The sediment from Lake Hess was rich in tephra deposits particularly evident in the lower part of the cores. Tephras are valuable to use for core correlation and can be traced through peaks in the magnetic susceptibility profiles. Results from the multiproxy analysis in the longest core (83 cm) identify three main phases of change. From the bottom up to 42 cm (ca. A.D.1800), the sediment is composed of light-grey organically rich clays. Both pigments and chironomids suggest variable trends in productivity and precipitation regime. At the end of the Little Ice Age chronozone (1770-1850 A.D.), pigment concentrations were very low. From 42 cm to ca. 25 cm (A.D. 1800-1940), the sedimentary record is composed of alternating black and dark organic-matter rich muds with variable amounts of macrophyte remains. Pigment concentrations and chironomid head capsule counts were also very low. These facies are composed of very fine plastic sediments with some faintly laminated intervals and an organic matter composition gradually decreasing towards the top of the zone. A sharp change occurs at 25 cm (ca.1940 A.D.) showing a strong increase in organic matter content, algal nutrients, and plant pigments together with a change in the chironomid assemblages. This might document a change in the trophic condition of the lake associated with changes in erosion/deposition rates. Although there are records of human impact in the area studied, involving the use of fires, most of the observed chemical and biological changes in Lake Hess sediment sequence were interpreted in terms of climate changes, especially to changes in moisture balance brought about by variations in the strength of the westerlies.