T157 Combined Ecological and Geologic Perspectives in Modern Terrestrial Ecosystems
Tuesday, 30 October 2007
1:30 PM - 5:30 PM
ORGANIC MATTER AND STABLE ISOTOPIC RECORD IN NAINITAL LAKE SEDIMENTS IN KUMAUN HIMALAYAS, INDIA
Paper number: T157-8
Program: Technical Sessions
Time: 3:15 PM – 3:30 PM
Authors
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Joyanto RouthStockholm University, Stockholm, N/A
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Govind J. ChakrapaniIndian Institute of Technology, Roorkee, N/A
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Bhishma KumarNational Institute of Hydrology, Roorkee, N/A
Abstract
We retrieved a 45 cm long core from the deepest part of the lake and sliced it at 2 cm intervals. Elemental concentrations of C, N, and S and their ratios (C/N, C/S), isotopic signature, and specific biomarkers (n-alkanes and pigments) were measured in the sedimentary organic matter. 210Pb dating in the core represents an age of ca. 85 years, and a sedimentation rate of about 5.0 mm/yr. TOC in sediments range from 2-5%, total N is 0.2-0.5%, and S is 13-25 mg/g. The low (11-15) C/N ratio coupled with low values for Carbon Preference Index (1-3) and Terrestrial Aquatic Ratio (0.3-2.9) indicate the dominance of algal derived matter in these sediments. The ä13C and ä15N values in sedimentary organic matter are -26.1‰ to -28.8‰ and 3.8‰ to 8.6‰, respectively. The lake shows nutrient deficient conditions, which favors cyanobacterial fixation. This is consistent with the high (1 to 4 mmol/g) concentration of different cyanobacterial pigments. Sulfate reduction is prevalent in the sediments, and ä34S ranges from 1 to 3‰. The main source of sulfate is from an underground spring and regional lithology. Sediment characteristics in the mid-section of the core suggests higher anthropogenic input (mainly from agricultural activities; 1950-80s), which affects the trophic state of the lake. Preventive measures adopted in recent years (e.g., aeration) have affected the sediments and ongoing biogeochemical processes in the lake.