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Isotopic Fingerprints of Paleoclimates during the Last 30,000 Years in Deep Confined Groundwaters of Southern India

Published online by Cambridge University Press:  20 January 2017

Balbir Singh Sukhija ,
Dontireddy Venkat Reddy  and
Pasupuleti Nagabhushanam
Balbir Singh Sukhija
Affiliation:
National Geophysical Research Institute, Hyderabad, -500 007, India
Dontireddy Venkat Reddy
Affiliation:
National Geophysical Research Institute, Hyderabad, -500 007, India
Pasupuleti Nagabhushanam
Affiliation:
National Geophysical Research Institute, Hyderabad, -500 007, India
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Abstract

Isotopic and geochemical evidence of paleoclimates, especially for the last glaciation, has been obtained from deep confined groundwaters of southern India. The δ13C, δ18O, chloride, and deuterium analyses of groundwaters show distinct excursions inferred to be related to climatic variations. The arid climatic episode associated with the last glaciation (18,000 ± 2000 yr B.P.) is conspicuously identified by signatures of relatively enriched δ13C (−10 to −12‰ PDB) and δ18O (−5.3 to −4.8‰ SMOW) values, and high chloride concentration (80 to 160 mg/l). The transition from an arid to humid period ca. 12,000–8000 yr B.P. is shown by a decreasing trend in the δ13C (−9.5 to −17‰) and δ18O (−4.5 to −6.3‰) contents of groundwaters. The late Holocene (since 4000 yr B.P.), marked by a more humid but unstable climate, is identified by further depletion of δ13C (−13 to −20‰) and δ18O (−5.2 to −6.3‰). Similar variation between δ18O and chloride values in confined groundwaters further demonstrates two distinct climatic excursions (arid and humid) governed by the “amount effect.” This is the first time that isotopic and geochemical signatures related to changing paleoclimates have been identified in the confined groundwaters of the southern Indian landmass.

Keywords

paleoclimatelast glaciationtransitionHoloceneisotopeschlorideamount effectgroundwatersouthern India
Type
Original Articles
Information
Quaternary Research , Volume 50 , Issue 3 , November 1998 , pp. 252 - 260
Copyright
University of Washington

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References

Agrawal, D.P. (1985). Climate and Geology of Kashmir: The Last 4 million years. Today and Tomorrow's Printers and Publisher, New Delhi.p. 1–12Google Scholar
Allison, G.B., and Hughes, M.W. (1978). The use of environmental chloride and tritium to estimate total recharge to an unconfined aquifer. Australian Journal of Soil Research 16, 181–195.CrossRefGoogle Scholar
Bath, A.H., Edmunds, W.M., and Andrews, J.N. (1979). Paleoclimatic trends deduced from the hydrochemistry of a Triassic sandstone aquifer, United Kingdom. “Isotope Hydrology 1978”. International Atomic Energy Agency, Vienna.p. 545–568Google Scholar
Clesceri, L.S., Greenberg, A.E., and Trussel, R.R. (1989). Standard Methods for the Examination of Water and Waste Water. American Public Health Association, Washington.p. 4-67–4-75Google Scholar
Craig, H. (1961). Standards of reporting concentrations of deuterium and oxygen-18 in natural water. Science 133, 1833–1834.Google Scholar
Deines, P. (1980). The isotopic composition of reduced organic carbon.Fritz, P., Ch. Fontes, J. Handbook of Environmental Geochemistry I: The Terrestrial Environment A Elsevier, Amsterdam/New York.329–406.Google Scholar
Edmunds, W.M., and Walton, N.R.G. (1980). A geochemical and isotopic approach to recharge evaluation in a semi-arid zone: Past and present. Proceedings of Symposium on Arid Zone Hydrology Investigations with Isotope Techniques, International Atomic Energy Agency, Vienna.p. 47–68Google Scholar
Fontes, J.Ch. (1981). Paleowaters.Gat, J.R., Gonfiantini, R. Stable Isotope Hydrology: Deuterium and Oxygen-18 in the Water Cycle 273–302.Google Scholar
Fontes, J. Ch (1983). Dating of groundwater, Guide Book on Nuclear Techniques in Hydrology. 285, 317., International Atomic Energy Agency, Vienna.Google Scholar
Gasse, F., Ledee, V., Massault, M., and Fontes, J. (1989). Water level fluctuations of lake Tanganyika in phase with oceanic changes during last glaciation and deglaciation. Nature 342, 57–59.CrossRefGoogle Scholar
Gasse, F., Tehet, R., Durand, A., Gilbert, E., and Fontes, J. (1990). The arid–humid transition in the Sahara and the Sahel during the last glaciation. Nature 346, 141–146.CrossRefGoogle Scholar
Geyh, M. A (1980). Interpretation of environmental isotopic groundwater data: Arid and semi-arid zones. In, Arid Zone Hydrology: Investigations with Isotope Techniques, 31, 46, 6–9., Nov. 1978, International Atomic Energy AgencyGoogle Scholar
Geyh, M.A., and Schleicher, H. (1990). Absolute Age Determination—Physical and Chemical Dating Methods and Their Application. Springer- Verlag, Berlin.Google Scholar
Gupta, C. P., Thangarajan, M., Gurunadha Rao, V. V. S., Sarma, M. R. K., Ramachandra, Y. M., Singh, V. S., and Sankaran, S (1986). Regional groundwater modelling studies in Neyveli Basin. Tamil Nadu.Google Scholar
Haynes, C.V., Eyles, C.H., Pavish, L.A., Ritchie, J.C., and Rybak, M. (1989). Holocene palaeoecology of the Eastern Sahara: Selima Oasis. Quaternary Science Reviews 8, 109–136.CrossRefGoogle Scholar
Heaton, T.H.E., Talma, A.S., and Vogel, J.Ch. (1983). Origin and history of nitrate in confined groundwater in the Western Kalahari. Journal of Hydrology 64, 232–262.Google Scholar
Hem, J. D (1985). Study and interpretation of the chemical characteristics of natural waters. 263 Google Scholar
Jordan, D. G., and Fisher, D. W (1977). Relation of bulk precipitation and evapotranspiration to water quality and water resources.Google Scholar
Kale, V.S., and Rajaguru, S.N. (1987). Late Quaternary alluvial history of the northwestern Deccan upland region. Nature 325, 612–614.CrossRefGoogle Scholar
Kelly, E.F., Amundson, R.G., Marino, M.D., and DeNiro, M.J. (1991). Stable isotope ratios of carbon in phytoliths as a qualitative method of monitoring vegetation and climate change. Quaternary Research 35, 222–233.CrossRefGoogle Scholar
Krishnamurthy, R.V., DeNiro, J.M., and Pant, R.K. (1982). Isotope evidence for Pleistocene climatic changes in Kashmir, India. Nature 298, 640–641.CrossRefGoogle Scholar
Ledru, M-P. (1993). Late Quaternary environmental and climatic changes in central Brazil. Quaternary Research 39, 90–98.Google Scholar
Phillips, F.M., Tansey, M.K., and Peters, L.A. (1989). An isotopic investigation of groundwater in the central Sanjuan Basin, New Mexico: Carbon-14 dating as a basis for numerical flow modeling. Water Resources Research 25, 2259–2273.CrossRefGoogle Scholar
Rozanski, K., Arans-Aragnas, L., and Gonfiantini, R. (1992). Relation between long term trends of oxygen-18 isotope composition of precipitation and climate. Science 258, 981–985.CrossRefGoogle ScholarPubMed
Said, R. (1993). The River Nile: Geology, Hydrology, and Utilization. Pergamon Press, Oxford.Google Scholar
Sarkar, A., Bhattacharya, S.K., and Sarin, M.M. (1993). Geochemical evidence for anoxic deep water in the Arabian Sea during the last glaciation. Geochimica Cosmochimica Acta 57, 1009–1016.CrossRefGoogle Scholar
Singh, G., Joshi, R.D., Chopra, S.K., and Singh, A.B. (1974). Late Quaternary history of vegetation and climate of Rajasthan desert. Philosophical Transactions, Royal Society of London 269, 467–501.Google Scholar
Somayajulu, B.L.K., Sharma, P., and Berger, W.H. (1984). 10 14 18 . Marine Geology 54, 169–180.CrossRefGoogle Scholar
Sonntag, C., Klitzsch, E., Lohnert, E.P., El-Shazly, E.M., Munnich, K.O., Junghans, Ch., Thorweihe, U., Weistroffer, K., and Swailem, F.M. (1979). Paleoclimatic information from deuterium and oxygen-18 in carbon-14 dated north Saharian groundwaters: Groundwater formation in the past. Isotope Hydrology 1978 International Atomic Energy Agency, Vienna.p. 569–581Google Scholar
Sukhija, B.S. (1982). Environmental radioisotope studies in groundwater hydrology. Geophysical Research Bulletin 20, 225–242.Google Scholar
Sukhija, B.S., Reddy, D.V., Nagabhushanam, P., and Chand, R. (1988). Validity of the environmental chloride method for recharge evaluation of coastal aquifers, India. Journal of Hydrology 99, 349–366.CrossRefGoogle Scholar
Sukhija, B.S., Reddy, D.V., Nagabhushanam, P., Hussain, S., Giri, V.Y., and Patil, D.J. (1996). Environmental and injected tracers methodology to estimate direct precipitation recharge to a confined aquifer. Journal of Hydrology 177, 77–97.CrossRefGoogle Scholar
Sukhija, B.S., Reddy, D.V., and Nandakumar, M.V. (1997). A method for evaluation of artificial recharge through percolation tanks using environmental chloride. Groundwater 35, 161–165.CrossRefGoogle Scholar
Sukumar, R., Ramesh, R., Pant, R.K., and Rajagopalan, G. (1993). 13 . Nature 364, 703–706.Google Scholar
Swain, A.M., Kutzbach, J.E., and Hastenrath, S. (1983). Estimates of Holocene precipitation for Rajasthan, India, based on pollen and lake-level data. Quaternary Research 19, 1–17.Google Scholar
Thorp, M., and Thomas, M. (1992). The timing of alluvial sedimentation and floodplain formation in the lowland humid tropics of Ghana, Sierra Leone, and western Kalimantan (Indonesian Borneo). Geomorphology 4, 409–422.Google Scholar
Van Campo, E. (1986). Monsoon fluctuation in two 20,000 yr B.P. oxygen isotope pollen records of southwest India. Quaternary Research 26, 376–388.CrossRefGoogle Scholar
Vogel, J.C. (1989). Evidence of past climatic change in the Namib Desert. Palaeogeography, Palaeoclimatology, Palaeoecology 70, 355–366.CrossRefGoogle Scholar
Wasson, R.J., Rajaguru, S.N., Misra, V.N., Agrawal, D.P., Dhir, R.P., Singhvi, A.K., and Rao, K.K. (1983). Late Quaternary stratigraphy and paleoclimatology of the Thar dune field. Zeitschrift Geomorphologie 45, 117–151.Google Scholar
Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., Markgraf, V., Kutzbach, J.E., Bartlein, P.J., Wright, H.E. Jr., and Prell, W.L. (1993). Climatic changes during the past 18,000 years: Regional synthesis, mechanisms, and causes.Wright, H.E., Kutzbach, J.E., Webb III, T., Ruddiman, W.F., Street-Perrott, F.A., Bartlein, P.J. Global Climates Since the Last Glacial Maximum University of Minnesota Press, Minneapolis.514–535.Google Scholar
Williams, M.A.J., and Clarke, M.F. (1984). Late Quaternary environments in north-central India. Nature 308, 633–635.CrossRefGoogle Scholar