Influence of precipitation, landscape and hydrogeomorphic lake features on pelagic allochthonous indicators in two connected ultraoligotrophic lakes of North Patagonia

• DOI: 10.1016/j.scitotenv.2012.03.085
• Publication Date: 2012-05-02T11:09:05Z
• Authors: Claudia Queimaliños; Mariana Reissig; María del Carmen ...; Marina Arcagni; Sergio Ribeiro Gu...; Linda Campbell; Carolina Soto Cár...; Raúl Rapacioli; María Arribére
• Keywords: Chlorophyll; Ultraoligotrophic Lakes; Food Chain; Rain; Argentina; Environment; 01 natural sciences; Zooplankton; Water Color; Allochthony; https://purl.org/becyt/ford/1.5; https://purl.org/becyt/ford/1.6; Snow; Animals; Organic Chemicals; https://purl.org/becyt/ford/1; Hydrogeomorphic Features; 0105 earth and related environmental sciences; Carbon Isotopes; Chlorophyll A; 15. Life on land; North Patagonia; Zooplankton Isotopic Carbon Signatures; Lakes; 13. Climate action; Seasons

We investigated the terrestrial influence on two chained deep ultraoligotrophic lakes of North Patagonia (Argentina) through the seasonal analysis of two pelagic allochthonous indicators: i) water color, as a proxy of allochthonous dissolved organic matter in lakes; and ii) the color to chlorophyll a ratio (Color:Chla), as an indicator of the relationship between allochthonous and autochthonous carbon pools. We also evaluated the potential transfer pathways of the allochthonous dissolved organic matter into the pelagic food webs of these deep lakes, including the natural zooplankton δ(13)C in the analysis. The dynamics of the allochthonous indicators were related to the precipitation regime, water level fluctuations, and hydrogeomorphic and catchment features of lakes Moreno East and Moreno West. The water color (absorbance at 440 nm) was extremely low (<0.28 m(-1)) in both lakes regardless of the season. However, precipitation and snowmelt regimes drove the increase and decrease of water color, respectively. A significant positive relationship between the zooplankton bulk δ(13)C with the water color would suggest an input of allochthonous organic carbon into the pelagic consumers. The incorporation of the dissolved allochthonous material into higher trophic levels is likely favored by the bacterivorous behavior of planktonic organisms, mixotrophic flagellates and ciliates, which dominate the pelagic food webs of these Patagonian lakes. Morphometric aspects, mainly the higher water residence time, led to lower values of allochthony in Moreno East compared to Moreno West, probably accentuated by its upper position in the lake chain. Overall, our results suggest that these allochthonous signals can bring insight into the magnitude of the interaction between terrestrial environments and lake ecosystems, even in extremely clear and ultraoligotrophic systems, such as the Andean Patagonian lakes.