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Hydrologic Variation in the Northern Great Plains During the Last Two Millennia

Published online by Cambridge University Press:  20 January 2017

Sherilyn C. Fritz ,
Emi Ito ,
Zicheng Yu ,
Kathleen R. Laird  and
Daniel R. Engstrom
Sherilyn C. Fritz
Affiliation:
Department of Geosciences, University of Nebraska, Lincoln, Nebraska 68588
Emi Ito
Affiliation:
Department of Geology & Geophysics and Limnological Research Center, University of Minnesota, Minneapolis, Minnesota 55455
Zicheng Yu
Affiliation:
Department of Geology & Geophysics and Limnological Research Center, University of Minnesota, Minneapolis, Minnesota 55455
Kathleen R. Laird
Affiliation:
Department of Biology, Queens University, Kingston, Ontario, K7L 3N6, Canada
Daniel R. Engstrom
Affiliation:
St. Croix Watershed Research Station, Science Museum of Minnesota, Marine-on-St. Croix, Minnesota 55047
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Abstract

Reconstructions of lake-water salinity at decadal resolution for the last 2000 yr are compared among three lakes in North Dakota to infer regional patterns of drought. The intersite comparisons are used to distinguish local variation in climate or hydrology from regional patterns of change. At one lake, diatom-inferred salinity and lake-water Mg/Ca inferred from ostracode shell chemistry are coherent, both in terms of direction and magnitude of change, indicating that each is a robust technique for reconstructing lake-water chemistry. The data show that the last 2000 yr have been characterized by frequent shifts between high and low salinity, suggesting shifts between dry and moist periods. Long intervals of high salinity suggest periods of multiple decades when droughts were intense and frequent, thus indicating times when drought was more persistent than in the 20th century. Both the Medieval Period and Little Ice Age were hydrologically complex, and there is no clear evidence to suggest that either interval was coherent or unusual in effective moisture relative to long-term patterns. Differences among the three sites may be attributed to variation in local hydrology, and these differences emphasize the need for multiple sites in deriving regional climate interpretations from paleoecological data.

Keywords

paleoclimatepaleolimnologypaleohydrologydroughtnorthern Great Plainssaline lakesdiatomsostracodes
Type
Research Article
Information
Quaternary Research , Volume 53 , Issue 2 , March 2000 , pp. 175 - 184
Copyright
University of Washington

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References

Almendinger, J.E., (1993). A groundwater model to explain past lake levels at Parkers Prairie, Minnesota, USA.. The Holocene 3, 105–115.Google Scholar
Appleby, P.G., Oldfield, F., (1978). The calculation of lead-210 dates assuming a constant rate of supply of the unsupported lead-210 to the sediment.. Catena 5, 1–8.CrossRefGoogle Scholar
Barlow, L.K., Sadler, J.P., Ogilvie, A.E.J., Buckland, P.C., Amorosi, T., Ingimundarson, J.H., Skidmore, P., Dugmore, A.J., McGovern, T.H., (1997). Interdisciplinary investigations of the end of the Norse western settlement in Greenland.. The Holocene 7, 489–500.Google Scholar
Bryson, R.A., (1966). Air masses, streamlines, and the boreal forest.. Geographical Bulletin 8, 228–269.Google Scholar
Carpenter, J.R., (1940). The grassland biome.. Ecological Monographs 10, 618–684.CrossRefGoogle Scholar
Chivas, A.R., DeDeckker, P., Cali, J.A., Chapman, A., Kiss, E., Shelly, J.M.G., (1993). Coupled stable-isotope and trace-element measurements of lacustrine carbonates as paleoclimatic indicators.. Swart, P.K., Lohmann, K.C., McKenzie, J., Savin, S., Climate Change in Continental Isotopic Records American Geophysical Union, Washington.113–121.Google Scholar
Clayton, L., (1962). Glacial geology of Logan and McIntosh Counties, North Dakota.. North Dakota Geological Survey Bulletin 37, 1–84.Google Scholar
Cook, E.R., Meko, D.M., Stockton, C.W., (1997). A new assessment of possible solar and lunar forcing of the bidecadal drought rhythm in the western United States.. Journal of Climate 10, 1343–1356.Google Scholar
Crowe, A.S., (1993). The application of a coupled water-balance–salinity model to evaluate the sensitivity of a lake dominated by groundwater to climate variability.. Journal of Hydrology 141, 33–73.Google Scholar
Dean, W.E., (1997). Rates, timing, and cyclicity of Holocene eolian activity in north-central United States: Evidence from varved lake sediments.. Geology 25, 331–334.Google Scholar
Dean, W.E., Ahlbrandt, T.S., Anderson, R.Y., Bradbury, J.P., (1996). Regional aridity in North America during the middle Holocene.. The Holocene 6, 145–155.CrossRefGoogle Scholar
Donovan, J.J., (1994). Measurement of reactive mass fluxes in evaporative groundwater-source lakes.. Renaut, R., Last, W.M., Sedimentology and Geochemistry of Modern and Ancient Saline Lakes SEPM Society for Sedimentology Geology, 33–50.Google Scholar
Fee, E.J., Hecky, R.E., Kasian, S.E.M., Cruikshank, D.R., (1995). Effects of lake size, water clarity, and climatic variability on mixing depths in Canadian Shield lakes.. Limnology and Oceanography 41, 912–920.Google Scholar
Forester, R.M., (1987). Late Quaternary paleoclimate records from lacustrine ostracodes.. Ruddiman, W.F., Wright, H.E. Jr., North America and Adjacent Oceans during the Last Deglaciation, The Geology of North America Geological Society of America, Boulder.261–276.Google Scholar
Fritz, S.C., Juggins, S., Battarbee, R.W., (1993). Diatom assemblages and ionic characterization of lakes of the Northern Great Plains, North America: A tool for reconstructing past salinity and climate fluctuations.. Canadian Journal of Fisheries and Aquatic Sciences 50, 1844–1856.Google Scholar
Grimm, E.C., (1983). Chronology and dynamics of vegetation change in the prairie-woodland region of southern Minnesota, U.S.A.. New Phytologist 93, 311–350.Google Scholar
Higgins, W.R., Yao, Y., Yarosh, E.S., Janowiak, J.E., Mo, K.C., (1997). Influence of the Great Plains low-level jet on summertime precipitation and moisture over the central United States.. American Meteorological Society, Bulletin 10, 481–507.Google Scholar
Hirschboeck, K. K., (1991). Climate and floods.. USGS Water Supply Paper 2376, pp. 67–88..Google Scholar
Hughes, M., Diaz, H.F., (1994). Was there a Medieval Warm Period, and if so, where and when.. Climatic Change 26, 109–142.Google Scholar
Ito, E., Yu, Z., Engstrom, D.R., Fritz, S.C., (1998). Is paleoclimatic interpretation of oxygen isotope records from glaciated Great Plains possible.. Abstracts, AMQUA 15, 119.Google Scholar
Jacobson, H.A., Engstrom, D.R., (1989). Resolving the chronology of recent lake sediments: An example from Devils Lake, North Dakota.. Journal of Paleolimnology 2, 81–98.CrossRefGoogle Scholar
Kelly, T.E., Block, D.A., (1967). Geology and ground water resources, Barnes County, North Dakota. Part I: Geology.. North Dakota Geological Survey Bulletin 43, .Google Scholar
Kelly, T.E., (1966). Geology and ground water resources, Barnes County, North Dakota. Part III: Ground water resources.. North Dakota Geological Survey Bulletin 43, .Google Scholar
Laird, K.R., Fritz, S.C., Cumming, B.F., (1998). A diatom-based reconstruction of drought intensity, duration, and frequency from Moon Lake, North Dakota: A sub-decadal record of the last 2300 years.. Journal of Paleolimnology 19, 161–179.CrossRefGoogle Scholar
Laird, K.R., Fritz, S.C., Grimm, E.C., Mueller, P.G., (1996). Century-scale paleoclimatic reconstruction from Moon Lake, a closed-basin lake in the northern Great Plains.. Limnology and Oceanography 41, 890–902.Google Scholar
Laird, K.R., Fritz, S.C., Maasch, K.A., Cumming, B.F., (1996). Greater drought intensity and frequency before AD 1200 in the Northern Great Plains, USA.. Nature 384, 552–555.Google Scholar
Last, W.M., (1992). Chemical composition of saline and subsaline lakes of the northern Great Plains, western Canada.. International Journal of Salt Lake Research 1, 47–76.Google Scholar
Mann, M.E., Bradley, R.S., Hughes, M.K., (1998). Global-scale temperature patterns and climate forcing over the past six centuries.. Nature 392, 779–787.CrossRefGoogle Scholar
Mason, I.M., Guzkowska, M.A.J., Rapley, C.G., (1994). The response of lake levels and areas to climatic change.. Climatic Change 27, 161–197.Google Scholar
Meko, D.M., (1992). Dendroclimatic evidence from the Great Plains of the United States.. Bradley, R.S., Jones, P.D., Climate Since A.D. 1500 Routledge, New York.312–330.Google Scholar
Muhs, D.R., Stafford, T.W.J., Been, J., Mahan, S., Burdett, J., Skipp, G., Muhs Rowland, Z., (1997). Holocene eolian activity in the Minot Dune Field, North Dakota.. Canadian Journal of Earth Sciences 34, 1442–1459.Google Scholar
Namias, J., (1983). Some causes of United States droughts.. Journal of Climate and Applied Meteorology 22, 30–39.2.0.CO;2>CrossRefGoogle Scholar
Oladipo, E.O., (1986). Spatial patterns of drought in the interior plains of North America.. Journal of Climate 6, 495–513.Google Scholar
Overpeck, J.P., Hugen, K., Hardy, D., Bradley, R., Case, R., Douglas, M., Finney, B., Gajewski, K., Jacoby, G., Jennings, A., Lamoureux, S., Lasca, A., MacDonald, G., Moore, J., Retelle, M., Smith, S., Wolfe, A., Zielinski, G., (1997). Arctic environmental change of the last four centuries.. Science 278, 1251–1256.CrossRefGoogle Scholar
Porter, S.C., (1986). Pattern and forcing of Northern Hemisphere glacier variations during the last millennium.. Quaternary Research 26, 27–48.Google Scholar
Rind, D., Overpeck, J., (1993). Hypothesized causes of decade to century scale climate variability: Climate model results.. Quaternary Science Reviews 12, 357–374.CrossRefGoogle Scholar
Sloan, C. E., (1972). Ground-water hydrology of prairie potholes in North Dakota.. U.S. Geological Survey Professional Paper, 585-C, pp. 1–28.Google Scholar
Smith, A.J., Donovan, J.J., Ito, E., Engstrom, D.R., (1997). Ground-water processes controlling a prairie lake's response to middle Holocene drought.. Geology 25, 391–394.2.3.CO;2>CrossRefGoogle Scholar
Stevens, L.R., (1997). The Stable Isotopic Composition of Varved Lake Sediment: Implications for Climatic Change in Minnesota.. University of Minnesota, .Google Scholar
Stine, S., (1994). Extreme and persistent drought in California and Patagonia during mediaeval time.. Nature 369, 546–549.Google Scholar
Stokes, S., Swinehart, J.B., (1997). Middle- and late-Holocene dune reactivation in the Nebraska Sand Hills, USA.. The Holocene 7, 263–272.Google Scholar
Stuiver, M., Pearson, G.W., (1993). High-precision bidecadal calibration of the radiocarbon timescale, AD 1950–500 BC and 2500–6000 BC.. Radiocarbon 35, 1–23.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14C data base and revised CALIB 3.0 14C age calibration program.. Radiocarbon 35, 215–230.CrossRefGoogle Scholar
Trenberth, K.E., Branstator, G.W., Arkin, P.A., (1988). Origins of the 1988 North American drought.. Science 242, 1640–1645.Google Scholar
Webster, K.E., Kratz, T.K., Bowser, C.J., Magnuson, J.J., (1996). The influence of landscape position on lake chemical responses to drought in northern Wisconsin.. Limnology and Oceanography 41, 977–984.Google Scholar
Winter, T.C., Woo, M., (1990). Hydrology of lakes and wetlands.. Wolman, M.G., Riggs, H.C., Surface Water Hydrology Geological Society of America, Boulder.159–188.Google Scholar
Woodhouse, C.A., Overpeck, J.T., (1998). 2000 years of drought variability in the central United States.. American Meteorological Society, Bulletin 79, 2693–2714.2.0.CO;2>CrossRefGoogle Scholar
Wright, H.E., (1967). A square-rod piston sampler for lake sediments.. Journal of Sedimentary Petrology 37, 975–976.CrossRefGoogle Scholar
Xia, J., Engstrom, D.R., Ito, E., (1997). Geochemistry of ostracode calcite: Part 2. The effects of water chemistry and seasonal temperature variation on Candona rawsoni.. Geochimica et Cosmochimica Acta 61, 383–391.Google Scholar
Xia, J.J., Haskell, B.J., Engstrom, D.R., Ito, E., (1997). Holocene climate reconstructions from tandem trace-element and stable-isotope composition of ostracodes from Coldwater Lake, North Dakota, USA.. Journal of Paleolimnology 17, 85–100.Google Scholar
Yu, Z.C., Ito, E., (1999). Possible solar forcing of century-scale drought frequency in the northern Great Plains.. Geology 27, 263–266.Google Scholar