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Change, edited by W. H. Berger and L. D. Labeyrie, pp. 137
-
in North America during the past 14,000 yr, Geology, 30,
455
143, D. Reidel, Norwell, Mass.
Overpeck, J. T., T. Webb III, and I. C. Prentice (1985), Quantitative
interpretation of fossil pollen spectra: Dissimilarity coef
458.
Viau, A. E., K. Gajewski, M. C. Sawada, and P. Fines (2006),
Millennial-scale temperature variations in North America during
the Holocene, J. Geophys. Res., 111, D09102, doi:10.1029/
2005JD006031.
Viau, A. E., K. Gajewski, M. C. Sawada, and J. Bunbury (2008),
Low- and High-frequency climate variability in Beringia during
the past 25,000 years, Can. J. Earth Sci., 45, 1435
-
cients
108.
Peros, M., and K. Gajewski (2008), Holocene climate and vegeta-
tion change on Victoria Island, western Canadian Arctic, Quat.
Sci. Rev., 27, 235
and the method of modern analogs, Quat. Res., 23,87
-
249.
Peros, M., K. Gajewski, and A. E. Viau (2008), Continental-scale
tree population response to rapid climate change, competition
and disturbance, Global. Ecol. Biogeogr., 17, 658
-
1453.
Walker, I. R., and L. C. Cwynar (2006), Midges and palaeotem-
perature reconstruction
-
669.
Peros, M., K. Gajewski, T. Paull, R. Ravindra, and B. Podritske
(2010), Multi-proxy record of postglacial environmental change
of south-central Melville Island, Northwest Territories, Canada,
Quat. Res., 73, 247
-
—
The North American experience, Quat.
1925.
Webb, T., III (1986), Is vegetation in equilibrium with climate?
How to interpret Late-Quaternary pollen data, Vegetatio, 67,
75
Sci. Rev., 25, 1911
-
258.
Podritske, B., and K. Gajewski (2007), Diatom community response
to multiple scales of Holocene climate variability in a small lake on
Victoria Island, NWT, Canada, Quat. Sci. Rev., 26,3179
-
91.
Webb, T., III, and R. A. Bryson (1972), Late- and postglacial
climatic change in the northern midwest USA: Quantitative esti-
mates derived from fossil pollen spectra by multivariate statistical
analysis, Quat. Res., 2,70
-
3196.
Rahmstorf, S. (2003), Timing of abrupt climate change: A precise
clock, Geophys. Res. Lett., 30(10), 1510, doi:10.1029/
2003GL017115.
Raymo, M. E., K. Ganley, S. Carter, D. W. Oppo, and J. MacManus
(1998), Millennial-scale climate instability during the early Pleis-
tocene epoch, Nature, 392, 699
-
115.
Wendland, W., and R. A. Bryson (1974), Dating climatic episodes
of the Holocene, Quat. Res., 4,9
-
24.
Whitmore, J., et al. (2005), Modern Pollen Data from North Amer-
ica and Greenland for Multi-scale Paleoenvironmental Applica-
tions, Quat. Sci. Rev., 24, 1828
-
702.
Ruddiman, W. (2003), The anthropogenic greenhouse era began
thousands of years ago, Clim. Change, 61, 261
-
1848.
Willemse, N. W., and T. E. Törnqvist (1999), Holocene century-
scale temperature variability from West Greenland lake records,
Geology, 27, 580
-
293.
Sawada, M., K. Gajewski, A. deVernal, and P. Richard (1999),
Comparison of marine and terrestrial Holocene climates in east-
ern North America, Holocene, 9, 267
-
584.
Williams, J. W., and S. T. Jackson (2007), Novel climates, no-
analog plant communities, and ecological surprises: Past and
future, Front. Ecol. Evol., 5, 475
-
278.
Sawada, M., A. E. Viau, G. Vettoretti, W. R. Peltier, and K. Ga-
jewski (2004), Comparison of North-American pollen-based
temperature and global lake-status with CCCma AGCM2 output
at 6 ka, Quat. Sci. Rev., 23, 225
-
482.
Williams, J. W., T. Webb III, B. N. Shuman, and P. J. Bartlein
(2000), Do low CO
2
concentrations affect pollen-based recon-
structions of LGM climates? A response to
-
244.
Schulz, M., and A. Paul (2002), Holocene climate variability on
centennial to millennial time scales: 1. Climate records from the
North-Atlantic realm, in Climate Development and History of the
North Atlantic Realm, edited by G. Wefer et al., pp. 41
-
'
Physiological sig-
ni
cance of low atmospheric CO
2
for plant-climate interactions
'
404.
Williams, J. W., D. M. Post, L. C. Cwynar, A. F. Lotter, and A. J.
Levesque (2002), Rapid vegetation responses to past climate
change, Geology, 30, 971
by Cowling and Sykes, Quat. Res., 53, 402
-
-
54,
Springer, New York.
Shuman, B., P. Bartlein, N. Logar, P. Newby, and T. Webb III
(2002a), Parallel climate and vegetation responses to the early-
Holocene collapse of the Laurentide Ice Sheet, Quat. Sci. Rev.,
21, 1793
974.
Williams, J. W., B. N. Shuman, T. Webb III, P. J. Bartlein, and P.
Leduc (2004), Quaternary vegetation dynamics in North Amer-
ica: Scaling from taxa to biomes, Ecol. Monogr., 74, 309
-
334.
Williams, J. W., et al. (2006), An Atlas of Pollen-Vegetation-Climate
Relationships for the United States and Canada, Am. Assoc. of
Stratigr. Palynol., Dallas, Tex.
Wright, H. E. (1976), The dynamic nature of Holocene vegetation,
Quat. Res., 6, 581
-
1805.
Shuman, B., T. Webb III, P. J. Bartlein, and J. W. Williams (2002b),
The anatomy of a climatic oscillation: Vegetation change in
eastern North America during the Younger Dryas chronozone,
Quat. Sci. Rev., 21, 1777
-
1791.
Tape, K., M. Sturm, and C. Racine (2006), The evidence for shrub
expansion in Northern Alaska and the Pan-Arctic, Global
Change Biol., 12, 686
-
596.
Wright, H. E., J. E. Kutzbach, T. Webb III, W. F. Ruddiman, F. A.
Street-Perrott, and P. J. Bartlein (1993), Global Climates Since
the Last Glacial Maximum, Univ. of Minn. Press, Minneapolis.
-
702.
Viau, A. E., and K. Gajewski (2009), Reconstructing millennial-
scale, regional paleoclimates of boreal Canada during the Holo-
cene, J. Clim., 22, 316
-
K. Gajewski and A. E. Viau, Laboratory for Paleoclimatology
and Climatology, Department of Geography, University of Ottawa,
Ottawa, ON K1N 6N5, Canada. (gajewski@uottawa.ca; aviau@
uottawa.ca)
330.
Viau, A. E., K. Gajewski, P. Fines, D. Atkinson, and M. C. Sawada
(2002), Widespread evidence of 1500 yr climate variability
-
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