Hostname: page-component-cd9895bd7-hc48f Total loading time: 0 Render date: 2024-12-26T16:07:29.952Z Has data issue: false hasContentIssue false
  • English
  • Français

Rapid response of forested vegetation to multiple climatic oscillations during the last deglaciation in the northeastern United States

Published online by Cambridge University Press:  20 January 2017

Zicheng Yu
Zicheng Yu*
Affiliation:
Department of Earth and Environmental Sciences, Lehigh University, 31 Williams Drive, Bethlehem, PA 18015, USA
*
⁎Fax: +1 610 7583677. E-mail address:[email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

Isotopic and pollen results from a marl lake (White Lake) in the Mid-Atlantic region of USA indicate the coupling of climate and vegetation changes. Oxygen isotopes of calcite from this site show multiple oscillations at millennial and centennial scales, including the Younger Dryas with 3‰ negative shifts in δ18O at 12.4–11.4 ka (1 ka = 1000 cal yr BP) and three cold events of magnitude 1–2‰ shifts during the Bølling–Allerød warm period (BOA) at 14.3–12.4 ka. Pollen data from the same core show nearly synchronous, close correspondence with isotope-inferred climate shifts, indicating rapid forest response to deglacial climate oscillations in southern New England. A plateau-like BOA is similar to other records around the North Atlantic Ocean.

Keywords

Bølling–Allerød periodClimate changeFossil pollenLacustrine carbonateLate glacialNortheastern United StatesStable isotopesYounger Dryas
Type
Short Paper
Information
Quaternary Research , Volume 67 , Issue 2 , March 2007 , pp. 297 - 303
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Alley, R.B., Meese, D.A., Shuman, C.A., Gow, A.J., Taylor, K.C., Grootes, P.M., White, J.W.C., Ram, M., Waddington, E.D., Mayewski, P.A., and Zielinski, G.A. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event. Nature 362, (1993). 527–529.Google Scholar
Brook, E.J., Harder, S., Severinghaus, J., Steig, E.J., and Sucher, C.M. On the origin and timing of rapid changes in atmospheric methane during the last glacial period. Global Biogeochemical Cycles 14, (2000). 559–572.Google Scholar
Chappellaz, J., Blunier, T., Raynaud, D., Barnola, J.M., Schwander, J., and Stauffer, B. Synchronous changes in atmospheric CH4 and Greenland climate between 40 and 8 kyr BP. Nature 366, (1993). 443–446.Google Scholar
Cotter, J.F.P., Ridge, J.C., Evenson, E.B., Sevon, W.D., Sirkin, L., and Stuchenrath, R. The Wisconsinan history of the Great Valley, Pennsylvania and New Jersey, and the age of the “Terminal Moraine”. New York State Museum Bulletin 455, (1986). 22–49.Google Scholar
Cwynar, L.C., and Spear, R.W. Lateglacial climate change in the White Mountains of New Hampshire. Quaternary Science Reviews 20, (2001). 1265–1274.CrossRefGoogle Scholar
Dansgaard, W. Stable isotopes in precipitation. Tellus 16, (1964). 436–468.CrossRefGoogle Scholar
Dansgaard, W., Johnsen, S., Clausen, H., Dahl-Jensen, D., Gundestrup, N., Hammer, C., Hvidberg, C., Steffensen, J., Sveinbjornsdottir, A., Jouzel, J., and Bong, G. Evidence for general instability in past climate from a 250 kyr ice-core record. Nature 364, (1993). 218–220.CrossRefGoogle Scholar
Davis, M.B. Climatic changes in southern Connecticut recorded by pollen deposition at Rogers Lake. Ecology 50, (1969). 409–422.Google Scholar
Deevey, E.S. Studies on Connecticut lake sediments: I. A postglacial climate chronology for southern New England. American Journal of Science 237, (1939). 691–724.CrossRefGoogle Scholar
Drummond, C.N., Patterson, W.P., and Walker, J.C.G. Climatic forcing of carbon-oxygen isotopic covariance in temperate-region marl lakes. Geology 23, (1995). 1031–1034.2.3.CO;2>CrossRefGoogle ScholarPubMed
Ebbeson, H., and Hald, M. Unstable Younger Dryas climate in the northeast North Atlantic. Geology 32, (2004). 673–676.CrossRefGoogle Scholar
Fægri, K., Kaland, P.E., and Krzywinski, K. Textbook of Pollen Analysis by Knut Fægri and Johs. Iversen. 4th ed. (1989). Wiley and Sons, London.Google Scholar
Friedman, I., and O'Neil, J.R. Complication of stable isotope fractionation factors of geochemical interest. Chapter, K.K. 6th ed. Data of Geochemistry (1977). United States Geological Survey, Professional Paper, KK–440.Google Scholar
Grimm, E.C., Jacobson, G. Jr. Late-Quaternary vegetation history of the eastern United States.. Gillespie, A.R., Porter, S.C., and Atwater, B.F. The Quaternary Period in the United States. (2004). Elsevier, Amsterdam. 381–402.Google Scholar
Huang, Y.S., Shuman, B., Wang, Y., Webb, T. III Hydrogen isotope ratios of palmitic acid in lacustrine sediments record late-Quaternary climate variations. Geology 30, (2002). 1103–1106.2.0.CO;2>CrossRefGoogle Scholar
Hughen, K.A., Overpeck, J.T., Peterson, L.C., and Trumbore, S. Rapid climate changes in the tropical Atlantic region during the last deglaciation. Nature 380, (1996). 51–54.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
Levesque, A.J., Cwynar, L.C., and Walker, I.R. Exceptionally steep north–south gradients in lake temperatures during the last deglaciation. Nature 385, (1997). 423–426.Google Scholar
Li, Y.X., Yu, Z.C., Kodama, K.P., and Moeller, R.E. A 14,000-year environmental change history revealed by mineral magnetic data from White Lake, New Jersey, USA. Earth and Planetary Research Letters 246, (2006). 27–40.Google Scholar
Mayewski, P.A., Meeker, L.D., Twickler, M.S., Whitlow, S., Yang, Q.Z., Lyons, W.B., and Prentice, M. Major features and forcing of high-latitude northern hemisphere atmospheric circulation using a 110,000-year-long glaciochemical series. Journal of Geophysical Research 102, (1997). 26345–26366.Google Scholar
Mayle, F.E., Levesque, A.J., and Cwynar, L.C. Alnus as an indicator taxon of the Younger Dryas cooling in eastern North America. Quaternary Science Reviews 12, (1993). 295–305.Google Scholar
Peteet, D.M., Vogel, J.S., Nelson, D.E., Southon, J.R., Nickmann, R.J., and Heusser, L.E. Younger Dryas climatic reversal in northeastern USA? AMS ages for an old problem. Quaternary Research 33, (1990). 219–230.Google Scholar
Reimer, P.J. et al. IntCa104 Terrestrial radiocarbon age calibration, 0-26 cal kyr BP. Radiocarbon 46, (2004). 1029–1058.Google Scholar
Rozanski, K., Araguas-Araguas, L., and Gonfiantini, R. Relation between long-term trends of oxygen-18 isotope composition of precipitation and climate. Science 258, (1992). 981–985.Google Scholar
Ruddiman, W.F., and McIntyre, A. The mode and mechanism of the last deglaciation: Oceanic evidence. Quaternary Research 16, (1981). 125–134.Google Scholar
Shuman, B., Newby, P., Huang, Y., Webb, T. III Evidence for the close climatic control of New England vegetation history. Ecology 85, (2004). 1297–1310.Google Scholar
Ter Braak, C.J.F., (1988). CANOCO–a FORTRAN program for canonical community ordination by [partial] [detrended] [canonical] correspondence analysis, principal components analysis and redundancy analysis (Version 2.1). Wageningen, The Netherlands: Agricultural Mathematics Group, .Google Scholar
Von Grafenstein, U., Erlenkeuser, H., Brauer, A., Jouzel, J., and Johnsen, S.J. A mid-European decadal isotope-climate record from 15,500 to 5000 years B. P.. Science 284, (1999). 1654–1657.Google Scholar
Watts, W.A. Late Quaternary vegetation of central Appalachia and the New Jersey coastal plain. Ecological Monographs 49, (1979). 427–469.Google Scholar
Webb, T. III Is vegetation in equilibrium with climate? How to interpret Late-Quaternary pollen data. Vegetatio 67, (1986). 75–91.Google Scholar
Williams, J.W., Post, D.M., Cwynar, L.C., and Lotter, A.F. Rapid and widespread vegetation responses to past climate change in the North Atlantic region. Geology 30, (2002). 971–974.Google Scholar
Yu, Z.C., and Eicher, U. Abrupt climate oscillations during the last deglaciation in central North America. Science 282, (1998). 2235–2238.CrossRefGoogle ScholarPubMed
Yu, Z.C., and Eicher, U. Three amphi-Atlantic century-scale cold events during the Bølling–Allerød warm period. Géographie Physique et Quaternaire 55, (2001). 175–183.Google Scholar