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Spatial and temporal variability of Holocene temperature in the North Atlantic region

Published online by Cambridge University Press:  30 January 2006

Michael R. Kaplan  and
Alexander P. Wolfe
Michael R. Kaplan*
Affiliation:
School of GeoSciences, University of Edinburgh, Edinburgh, EH8 9XP, Scotland
Alexander P. Wolfe
Affiliation:
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada T6G 2E3
*
*Corresponding author.E-mail address:[email protected](M.R. Kaplan).
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Abstract

The early Holocene climate of the North Atlantic region was influenced by two boundary conditions that were fundamentally different from the present: the presence of the decaying Laurentide Ice Sheet (LIS) and higher than present summer solar insolation. In order to assess spatial and temporal patterns of Holocene climate evolution across this region, we collated quantitative paleotemperature records at sub-millennial resolution and synthesized their temporal variability using principal components analysis (PCA). The analysis reveals considerable spatial variability, most notably in the time-transgressive expression of the Holocene thermal maximum (HTM). Most of the region, but especially areas peripheral to the Labrador Sea and hence closest to the locus of LIS disintegration, experienced maximum Holocene temperatures that lagged peak summer insolation by 1000–3000 years. Many sites from the northeastern North Atlantic sector, including the Nordic Seas and Scandinavia, either warmed in phase with maximum summer insolation (11,000–9000 years ago) or were less strongly lagged than the Baffin Bay–Labrador Sea region. These spatially complex patterns of Holocene climate development, which are defined by the PCA, resulted from the interplay between final decay of the LIS and solar insolation forcing.

Keywords

HoloceneNorth Atlantic OceanLaurentide Ice SheetInsolationPrincipal components analysis
Type
Original Articles
Information
Quaternary Research , Volume 65 , Issue 02 , March 2006 , pp. 223 - 231
Copyright
University of Washington

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References

Andrews, J.T., Giraudeau, J., (2003). Multi-proxy records showing significant Holocene environmental variability: the inner N. Iceland shelf (Hunaflói). Quaternary Science Reviews 22, 175–193.Google Scholar
Andrews, J.T., Keigwin, L.D., Hall, F.R., Jennings, A.E., (1999). Abrupt deglaciation events and Holocene palaeoceanography from high-resolution cores, Cartwright Saddle, Labrador Shelf, Canada. Journal of Quaternary Science 14, 383–397.3.0.CO;2-J>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., Gagnon, J.-M., (1999). Forcing of the cold event of 8,200 years ago by catastrophic drainage of Laurentide lakes. Nature 400, 344–348.CrossRefGoogle Scholar
Belkin, I.M., Levitus, S., Antonov, J.I., Malmberg, S.-A., (1998). ‘Great Salinity Anomalies’ in the North Atlantic. Progress in Oceanography 41, 1–68.CrossRefGoogle Scholar
Berger, A., Loutre, M.F., (1991). Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, 297–318.Google Scholar
Birks, H.H., (1991). Holocene vegetational history and climatic change in west Spitsbergen-plant macrofossils from Skardtjørna, an arctic lake. The Holocene 1, 209–218.CrossRefGoogle Scholar
Birks, C.J.A., Koç, N., (2002). A high-resolution diatom record of late-Quaternary sea-surface temperatures and oceanographic conditions from the eastern Norwegian Sea. Boreas 31, 323–344.Google Scholar
Bond, G., Heinrich, H., Broecker, W., Labeyrie, L., McManus, J., Andrews, J., Huon, S., Jantschik, R., Clasen, S., Simet, C., Tedesco, K., Klas, M., Bonani, G., Ivy, S., (1992). Evidence for massive discharges of icebergs into the North Atlantic Ocean during the last glacial. Nature 360, 245–249.CrossRefGoogle Scholar
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hadjas, I., Bonani, G., (1997). A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278, 1257–1266.Google Scholar
Calvo, E., Grimalt, J., Jansen, E., (2002). High resolution UK37 sea surface temperature reconstruction in the Norwegian Sea during the Holocene. Quaternary Science Reviews 21, 1385–1394.CrossRefGoogle Scholar
CAPE, , (2001). Holocene paleoclimate data from the Arctic: testing models of global climate change. Quaternary Science Reviews 20, 1275–1287.Google Scholar
Clark, P.U., Marshall, S.J., Clarke, G.K.C., Hostetler, S.W., Licciardi, J.M., Teller, J.T., (2001). Freshwater forcing of abrupt climate change during the last glaciation. Science 293, 283–287.CrossRefGoogle ScholarPubMed
Clark, P.U., Pisias, N.G., Stocker, T.S., Weaver, A.J., (2002). The role of the Atlantic thermohaline circulation in abrupt climate change. Nature 415, 863–869.CrossRefGoogle ScholarPubMed
COHMAP, , (1998). Climatic changes of the last 18,000 years: observations and model simulations. Science 241, 1043–1052.CrossRefGoogle Scholar
Cuffey, K.M., Clow, G.D., (1997). Temperature, accumulation and ice sheet elevation in central Greenland through the last deglacial transition. Journal of Geophysical Research 102, 26383–26396.CrossRefGoogle Scholar
Dahl, S.O., Nesje, A., (1996). A new approach to calculating Holocene winter precipitation by combining glacier equilibrium-line altitudes and pine-tree limits: a case study from Hardangerjøkulen, central southern Norway. The Holocene 6, 381–398.Google Scholar
Dickson, R.R., Lazier, J., Meincke, J., Rhines, P., Swift, J., (1996). Long-term coordinated changes in the convective activity of the North Atlantic. Progress in Physical Oceanography 38, 241–295.CrossRefGoogle Scholar
Duplessy, J.C., Labeyrie, L., Arnold, M., Paterne, M., Duprat, J., van Weering, T.C.E., (1992). Changes in surface salinity of the North Atlantic Ocean during the last deglaciation. Nature 358, 485–487.CrossRefGoogle Scholar
Dyke, A.S., Hooper, J., Savelle, J.M., (1996). A history of sea ice in the Canadian Arctic Archipelago based on postglacial remains of the Bowhead Whale (Balaena mystecetus). Arctic 49, 235–255.Google Scholar
Dyke, A.S., Moore, A., Roberson, L., (2003). Deglaciation of North America.. Geological Survey of Canada Open File Report 1574 (CD ROM).CrossRefGoogle Scholar
Jennings, A.E., Knudsen, K.L., Hald, M., Hansen, C.V., Andrews, J.T., (2002). A mid-Holocene shift in Arctic sea-ice variability on the East Greenland Shelf. The Holocene 12, 49–58.Google Scholar
Kaufman, D.S., Ager, T.A., Anderson, N.J., Anderson, P.M., Andrews, J.T., Bartlein, P.J., Brubaker, L.B., Coats, L.L., Cwynar, L.C., Duvall, M.L., Dyke, A.S., Edwards, M.E., Eisner, W.R., Gajewski, K., Geirsdottir, A., Hu, F.S., Jennings, A.E., Kaplan, M.R., Kerwin, M.N., Lozhkin, A.V., MacDonald, G.M., Miller, G.H., Mock, C.J., Oswald, W.W., Otto-Bliesner, B.L., Porinchu, D.F., Rühland, K., Smol, J.P., Steig, E.J., Wolfe, B.B., (2004). Holocene thermal maximum in the western Arctic (0 to 180°W). Quaternary Science Reviews 23, 529–560.Google Scholar
Koç, N., Jansen, E., Haflidason, H., (1993). Paleoceanographic reconstructions of surface ocean conditions in the Greenland, Iceland, and Norwegian Seas through the last 14 ka based on diatoms. Quaternary Science Reviews 12, 115–140.CrossRefGoogle Scholar
Koerner, R.M., Fisher, D.A., (1990). A record of Holocene summer climate from a Canadian high-Arctic ice core. Nature 343, 630–631.Google Scholar
Kutzbach, J.E., (1981). Monsoon climate of the early Holocene: climate experiment with the Earth's orbital parameters for 9000 years ago. Science 214, 59–61.CrossRefGoogle ScholarPubMed
Laird, K.R., Fritz, S.C., Grimm, E.C., Mueller, P.G., (1996). Century-scale paleoclimatic reconstructions from Moon Lake, a closed-basin lake in the northern Great Plains. Limnology and Oceanography 41, 890–902.Google Scholar
Levac, E., (2001). High resolution Holocene palynological record from the Scotian shelf. Marine Micropaleontology 43, 179–197.Google Scholar
Levac, E., de Vernal, A., Blake, W. Jr., (2001). Sea-surface conditions in northernmost Baffin Bay during the Holocene: palynological evidence. Journal of Quaternary Science 16, 353–363.Google Scholar
Licciardi, J.M., Teller, J.T., Clark, P.U., (1999). Freshwater routing by the Laurentide Ice Sheet during the last deglaciation. Clark, P.U., Webb, R.S., Keigwin, L., Mechanisms of Global Climate Change at Millennial Time Scales, Geophysical Monograph Series 112 American Geophysical Union, Washington, DC.177–201.Google Scholar
Lubinski, D.J., Forman, S.L., Miller, G.H., (1999). Holocene glacier and climate fluctuations on Franz Josef Land, Arctic Russia, 80°N. Quaternary Science Reviews 18, 85–108.Google Scholar
Mayewski, P.A., Rohling, E.J., Stager, J.C., Karlén, W., Maasch, K., Meeker, L.D., Meyerson, E., Gasse, F., Van Kreveld, S., Holmgren, K., Lee-Thorp, J., Rosqvist, G., Rack, F., Staubwasser, M., Schneider, R.R., Steig, E.J., (2004). Holocene climate variability. Quaternary Research 62, 243–255.Google 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., (1999). Stratified interglacial lacustrine sediments from Baffin Island, Arctic Canada: chronology and paleoenvironmental implications. Quaternary Science Reviews 18, 789–810.Google Scholar
Nesje, A., Dahl, S.O., Bakke, J., (2004). Were abrupt Late glacial and early-Holocene climatic changes in northwest Europe related to freshwater outbursts to the North Atlantic and Arctic oceans?. The Holocene 14, 299–310.Google Scholar
Overpeck, J.T., Hughen, K.A., Hardy, D., Bradley, R.S., Case, R., Douglas, M.S.V., Finney, B., Gajewski, K., Jacoby, G., Jennings, A.E., Lamoureux, S., Lasca, A., MacDonald, G.M., Moore, J.J., Retelle, M., Wolfe, A.P., (1997). Arctic environmental change of the last four centuries. Science 278, 1251–1256.Google Scholar
Patterson, W.S.B., Koerner, R.M., Fisher, D.A., Johnsen, S.J., Clausen, H.B., Dansgaard, W., Butcher, P., Oeschger, M., (1977). An oxygen-isotope climatic record from the Devon Island Ice Cap, Arctic Canada. Nature 266, 508–511.CrossRefGoogle Scholar
Penalba, M.C., Arnold, M., Guiot, J., Duplessey, J.-C., de Beaulieu, J.-L., (1997). Termination of the last glaciation in the Iberian Peninsula inferred from the pollen sequence of Quintanar de la Sierra. Quaternary Research 48, 205–214.Google Scholar
Rahmstorf, S., (1995). Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycle. Nature 378, 145–149.CrossRefGoogle Scholar
Rahmstorf, S., (1997). Risk of sea-change in the Atlantic. Nature 388, 825–826.Google Scholar
Sachs, J.P., Keigwin, L.D., (2004). Extreme Cooling of Slopewaters East of the USA and Canada During the Holocene.. EOS Transactions AGU, 85, (47), Fall Meeting Supplement, Abstract PP13A–0591.Google Scholar
Sarnthein, M., van Kreveld, S., Erlenkeuser, H., Grootes, P.M., Kucera, M., Pflaumann, U., Schulz, M., (2003). Centennial to millennial-scale periodicities of Holocene climate and sediment injections off the western Barents shelf, 75°N. Boreas 32, 447–461.Google Scholar
Sawada, M., Gajewski, K., de Vernal, A., Richard, P.J.H., (1999). Comparison of marine and terrestrial Holocene climatic reconstructions from northeastern North America. The Holocene 9, 267–277.Google Scholar
Sejrup, H.P., Haflidason, H., Flatebø, T., Kristensen, D., Grøsfjeld, K., Larsen, E., (2001). Late-glacial to Holocene environmental changes and climate variability: evidence from Voldafjorden, western Norway. Journal of Quaternary Science 16, 181–198.CrossRefGoogle Scholar
Seppä, H., Birks, H.J.B., (2001). July mean temperature and annual precipitation trends during the Holocene in the Fennoscandian tree-line area: pollen-based climate reconstructions. The Holocene 11, 527–539.Google Scholar
Steig, E.J., (1999). Mid-Holocene climate change. Science 286, 1485–1487.Google Scholar
ter Braak, C.J.F., Prentice, I.C., (1988). A theory of gradient analysis. Advances in Ecological Research 18, 271–317.CrossRefGoogle Scholar
ter Braak, C.J.F., Šmilauer, P., (1998). CANOCO Reference Manual and User's Guide to Canoco for Windows: Software for Canonical Community Ordination (version 4) Ithaca. Microcomputer Power, New York.Google Scholar
Whitlock, C., Bartlein, P.J., Watts, W.A., (1993). Vegetation history of Elk Lake. Bradbury, J.P., Dean, W.E., Elk Lake, Minnesota: Evidence for Rapid Change in The North-Central United States Special Paper - Geological Society of America vol. 276, Geological Society of America, Boulder, Colorado.251–274.Google Scholar
Wooller, M.J., Francis, D., Fogel, M.L., Miller, G.H., Walker, I.R., Wolfe, A.P., (2004). Quantitative paleotemperature estimates from δ 18O of chironomid head capsules preserved in arctic lake sediments. Journal of Paleolimnology 31, 267–274.CrossRefGoogle Scholar