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Holocene Environmental Variability in Southern Greenland Inferred from Lake Sediments

Published online by Cambridge University Press:  20 January 2017

Michael R. Kaplan ,
Alexander P. Wolfe  and
Gifford H. Miller
Michael R. Kaplan*
Affiliation:
Department of Geology and Geophysics, University of Wisconsin, 1215 W. Dayton St. Madison, Wisconsin, 53706, E-mail: [email protected]
Alexander P. Wolfe
Affiliation:
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, T6G 2E3, Canada
Gifford H. Miller
Affiliation:
Institute of Arctic and Alpine Research and Department of Geological Sciences, University of Colorado, Colorado, 80309-0450
*
1To whom correspondence should be addressed.
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Abstract

Sediments from Qipisarqo Lake provide a continuous Holocene paleoenvironmental record from southern Greenland. Following deglaciation and glacio-isostatic emergence of the basin from the sea ∼9100 cal yr B.P., proxies of lake paleoproductivity, including biogenic silica and organic matter, increased markedly until 6000 cal yr B.P. and thereafter remained stable over the ensuing warm three millennia. Subsequent decreases in these proxies, most dramatically between 3000 and 2000 cal yr B.P., show the lake's responses to initial Neoglacial cooling. Intervals of ameliorated limnological conditions occurred between 1300 and 900 and between 500 and 280 cal yr B.P., briefly interrupting the decreasing trend in productivity that culminated in the Little Ice Age. Increased lake productivity during the latter half of the 20th century, which reflects the limnological response to circum-arctic warming, still has not reached peak Holocene values. The Neoglacial climate of the last 2000 yr includes the most rapid high-amplitude environmental changes of the past nine millennia. The Norse thus migrated around the North Atlantic Ocean region in the most environmentally unstable period since deglaciation. Lacustrine sediment records provide a context with which to consider future environmental changes in the Labrador Sea region. In particular, any future warming will be superposed on a regional climate system that is currently exhibiting highly unstable behavior at submillennial timescales.

Type
Research Article
Information
Quaternary Research , Volume 58 , Issue 2 , September 2002 , pp. 149 - 159
Copyright
University of Washington

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References

Abbott, M.B., Stafford, T.W. Jr. Radiocarbon geochemistry of modern and ancient arctic lake systems, Baffin Island, Canada. Quaternary Research 45, (1996). 300 311.CrossRefGoogle Scholar
Alley, R.B., Mayewski, P.A., Sowers, T., Stuiver, M., Taylor, K.C., and Clark, P.U. Holocene climatic instability: A prominent, widespread event 8200 years ago. Geology 25, (1997). 483 486.2.3.CO;2>CrossRefGoogle Scholar
Barber, D.C., Dyke, A.S., Hillaire-Marcel, C., Jennings, A.E., Andrews, J.T., Kerwin, M.W., Bilodeau, G., McNeely, R., Southon, J., Morehead, M.D., and Gagnon, J.-M. Forcing of the cold event of 8,200 years ago by catastrophic drainage of Laurentide lakes. Nature 400, (1999). 344 348.Google Scholar
Barlow, L.K., Sadler, J.P., Ogilvie, A.E.J., Buckland, P.C., Amorosi, T., Ingimundarson, J.H., Skidmore, P., Dugmore, A.J., and McGovern, T.H. Interdisciplinary investigations of the end of the Norse western settlement in Greenland. The Holocene 7, (1997). 489 499.Google Scholar
Bennike, O. Palaeoecological studies of Holocene lake sediments from west Greenland. Palaeogeography, Palaeoclimatology, Palaeoecology 155, (2000). 285 304.CrossRefGoogle Scholar
Berger, A. Long term variations of caloric insolation resulting from the Earth's orbital elements. Quaternary Research 9, (1978). 139 167.Google Scholar
Blake, W. Jr., Boucherle, M., Fredskild, B., Janssens, J.A., and Smol, J.P. The geomorphological setting, glacial history and Holocene development of ‘Kap Inglefield Sø’, Inglefield Land, North-West Greenland. Meddelelser om Grønland Geoscience 27, (1992). 1 42.CrossRefGoogle Scholar
Bradley, R.S. Past global changes and their significance for the future. Quaternary Science Reviews 19, (2000). 391 402.CrossRefGoogle Scholar
Buckland, P.C., Amorosi, T., Barlow, L.K., Mayewski, P., McGovern, T.H., Ogilvie, A.E.J., and Skidmore, P. Climate change, bioarchaeology, and the end of Norse settlement. Antiquity 70, (1996). 88 96.CrossRefGoogle Scholar
Carter, S.J., and Colman, S.M. Biogenic silica in Lake Baikal sediments: Results from 1990–1992 American cores. Journal of Great Lakes Research 20, (1994). 751 760.Google Scholar
Colman, S.M., Peck, J.A., Karabanov, E.B., Carter, S.J., Bradbury, J.P., King, J.W., and Willimans, D.F. Continental climate response to orbital forcing from biogenic silica records in Lake Baikal. Nature 378, (1995). 769 771.Google Scholar
Conley, D.J. Biogenic silica as an estimate of siliceous microfossil abundance in Great Lakes sediments. Biogeochemistry 6, (1988). 161 179.Google Scholar
Cremer, H., Wagner, B., Melles, M., and Hubberten, H.W. The postglacial environmental development of Raffles Sø, east Greenland: Inferences from a 10,000 year diatom record. Journal of Paleolimnology 26, (2001). 67 87.CrossRefGoogle Scholar
Crowley, T.J. Causes of climate change over the past 1000 years. Science 289, (2000). 270 277.Google Scholar
Dahl-Jensen, D., Mosegaard, K., Gundestrup, G., Clow, G.D., Johnson, S.J., Hansen, A.W., and Balling, B. Past temperature directly from the Greenland ice sheet. Science 282, (1998). 268 271.Google Scholar
Dean, W.E. Jr. Determination of carbonate and organic matter in calcareous sediments and sedimentary rocks by loss on ignition: Comparison with other methods. Journal of Sedimentary Petrology 44, (1974). 242 248.Google Scholar
Douglas, M.S.V., Smol, J.P., Blake, W. Jr. Marked post-18th century environmental change in high-arctic ecosystems. Science 266, (1994). 416 419.CrossRefGoogle ScholarPubMed
Dyke, A.S., Dale, J.E., and McNeely, R.N. Marine molluscs as indicators of environmental change in glaciated North America and Greenland during the last 18,000 years. Géographie Physique et Quaternaire 50, (1996). 125 184.CrossRefGoogle Scholar
Edlund, M.B., and Stoermer, E.F. A 200,000-year high-resolution record of diatom productivity and community makeup from Lake Baikal shows high correspondence to the marine oxygen-isotope record of climate change. Limnology and Oceanography 45, (2000). 948 962.Google Scholar
Eggimann, D.W., Manheim, F.T., and Betzer, P.R. Dissolution and analyses of amorphous silica in marine sediments. Journal of Sedimentary Petrology 50, (1980). 215 225.Google Scholar
Engstrom, D.R., Wright, H.E. Jr. Chemical stratigraphy of lake sediments as a record of environmental change. Hawworth, E.W., and Lund, J.W.G. Lake Sediments and Environmental History. (1984). Leicester Univ. Press, Leicester. 11 67.Google Scholar
Funder, S. Quaternary Geology of the ice free areas and adjacent shelves of Greenland. Fulton, R.J. Quaternary Geology of Canada and Greenland. (1989). Geological Survey of Canada Geology of Canada Vol. 1, Ottawa. 741 792.Google Scholar
Glew, J.R. A new trigger mechanism for sediment samplers. Journal of Paleolimnology 2, (1989). 241 248.Google Scholar
Grove, J. M. 1988, The Little Ice Age, Methuen, New York.Google Scholar
Heiri, O., Lotter, A.F., and Lemcke, G. Loss on ignition as a method for estimating organic and carbonate content in sediments: Reproducibility and compatibility of results. Journal of Paleolimnology 25, (2001). 101 110.Google Scholar
Joynt, E.H. III, and Wolfe, A.P. Paleoenvironmental inference models from diatoms in Baffin Island lakes (Nunavut, Canada), and reconstruction of summer water temperature. Canadian Journal of Fisheries and Aquatic Sciences 58, (2001). 1222 1243.Google Scholar
Keigwin, L.D., and Boyle, E.A. Detecting Holocene changes in thermohaline circulation. Proceedings of the National Academy of Sciences 97, (2000). 1343 1346.Google Scholar
Kelly, M. A review of the Quaternary Geology of western Greenland. Andrews, J.T. Quaternary Environments: Eastern Canadian Arctic, Baffin Bay and Western Greenland. (1985). Allen and Unwin, Boston. 461 501.Google Scholar
Kerwin, M.W., Overpeck, J.T., Webb, R.S., DeVernal, A., Rind, D.H., and Healy, R.J. The role of oceanic forcing in mid-Holocene Northern Hemisphere climatic change. Paleoceanography 14, (1999). 200 210.Google Scholar
Levesque, A.J., Mayle, F.E., Walker, I.R., and Cwynar, L.C. A previously unrecognized late-glacial cold event in eastern North America. Nature 361, (1993). 623 626.Google Scholar
MacDonald, G.M., Felzer, B., Finney, B.P., and Foreman, S.L. Holocene lake sediment records of Arctic hydrology. Journal of Paleolimnology 24, (2000). 1 14.Google Scholar
Manabe, S., and Broccoli, A.J. The influence of the continental ice sheets on the climate of the ice age. Journal of Geophysical Research 90, (1985). 2167 2190.CrossRefGoogle Scholar
Miller, G.H., Mode, W.N., Wolfe, A.P., Sauer, P.E., Bennike, O., Forman, S.L., Short, S.K., Stafford, T.W. Jr. Stratified interglacial lacustrine sediments from Baffin Island, Arctic Canada: Chronology and paleoenvironmental implications. Quaternary Science Reviews 18, (1999). 789 810.Google Scholar
Moore, J.J. Glacial and Climatic History of the Cape Dyer Region, Eastern Cumberland Peninsula, Baffin Island, Canada: A Rock Magnetic and Varved Sediment Investigation of Donard Lake. (1996). University of Colorado, Google Scholar
Mortlock, R.A., and Froelich, P.N. A simple method for the rapid determination of biogenic opal in pelagic marine sediments. Deep Sea Research 36, (1989). 1415 1426.CrossRefGoogle Scholar
Nesje, A. A piston corer for lacustrine and marine sediments. Arctic and Alpine Research 24, (1992). 257 259.Google Scholar
Noon, P.E., Birks, H.J.B., Jones, V.J., and Ellis-Evans, J.C. Quantitative models for reconstructing catchment ice extent using physical-chemical characteristics of lake sediments. Journal of Paleolimnology 25, (2001). 375 392.Google Scholar
Ogilvie, A.E.J., Barlow, L.K., and Jennings, A.E. North Atlantic climate c. A.D. 1000: Millennial reflections on the Viking discoveries of Iceland, Greenland and North America. Weather 55, (2000). 34 45.Google Scholar
Overpeck, J., Hughen, K., Hardy, D., Bradley, R.S., 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., and Zelinski, G. Arctic environmental change of the last four centuries. Science 278, (1997). 1251 1256.Google Scholar
Putnins, P. The climate of Greenland. Orvig, S. Climates of the Polar Regions. (1970). World Survey of Climatology, Amsterdam. 3 128.Google Scholar
Rouse, W.R., Douglas, M.S.V., Hecky, R.E., Hershey, A.E., Kling, G.W., Lesack, L., Marsh, P., McDonald, M., Nicholson, B.J., Roulet, N.T., and Smol, J.P. Effects of climate change on fresh waters of Region 2: Arctic and Sub-Arctic North America. Hydrologic Processes 11, (1997). 873 902.Google Scholar
Schindler, D.W., Beatty, K.G., Fee, E.J., Cruikshank, D.R., Debruyn, E.R., Findlay, D.L., Linsey, G.A., Shearer, J.A., Stainton, M.P., and Turner, M.A. Effects of climatic warming on lakes of the central Boreal Forest. Science 250, (1990). 967 970.Google Scholar
Smith, G.D. Numerical Solution of Partial Differential Equations: Finite Difference Methods. (1985). Clarendon, Oxford.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., van der Plicht, J., and Spurk, M. INTCAL98 radiocarbon age calibration 24,000–0 cal yr B.P. Radiocarbon 40, (1998). 1041 1083.CrossRefGoogle Scholar
Wigley, T.M.L., and Raper, S.C.B. Interpretation of high projections for global-mean warming. Science 293, (2001). 451 454.Google Scholar
Willemse, N.W., and Törnqvist, T.E. Holocene century-scale temperature variability from West Greenland lake records. Geology 27, (1999). 580 584.Google Scholar
Wolfe, A.P. Climate modulates the acidity of Arctic lakes on millennial time scales. Geology 30, (2002). 215 218.Google Scholar
Wolfe, A.P., and Perren, B.B. Chrysophycean microfossils record marked responses to recent environmental changes in high- and mid-Arctic lakes. Canadian Journal of Botany 79, (2001). 747 752.Google Scholar