Climate change and Arctic ecosystems I: Vegetation changes north of 55 (2003)
Bigelow, N.H., Brubaker, L.B., Edwards, M.E., Harrison, S.M., Prentice, I.C., Andreson, P.M., ...
Bigelow, N. H., Brubaker, L. B., Edwards, M. E., Harrison, Sandy P., Prentice, I. Colin, Anderson, P. M., ...
Kaplan, Jed O., Bigelow, N. H., Prentice, I. Colin, Harrison, Sandy P., Bartlein, Patrick J., Christensen, T. R., ...
Bigelow, N. H., Brubaker, L. B., Edwards, M. E., Harrison, S. P., Prentice, I. C., Anderson, P. M., ...
A unified scheme to assign pollen samples to vegetation types was used to reconstruct vegetation patterns north of 55°N at the last glacial maximum (LGM) and mid-Holocene (6000 years B.P.). The...
Kaplan, J. O., Bigelow, N. H., Prentice, I. C., Harrison, S. P., Bartlein, P. J., Christensen, T. R., ...
Large variations in the composition, structure, and function of Arctic ecosystems are determined by climatic gradients, especially of growing-season warmth, soil moisture, and snow cover. A unified...
Kaplan, J. O., Bigelow, N. H., Prentice, I. C., Harrison, S.P., Bartlein, P.J., Christensen, T.R., ...
Large variations in the composition, structure, and function of Arctic ecosystems are determined by climatic gradients, especially of growing-season warmth, soil moisture, and snow cover. A unified...
Kaplan, J. O, Bigelow, N. H, Prentice, I. C, Harrison, S. P, Bartlein, P. J, Christensen, T. R, ...
Large variations in the composition, structure, and function of Arctic ecosystems are determined by climatic gradients, especially of growing-season warmth, soil moisture, and snow cover. A unified...
Pollen-based biomes for Beringia 18,000, 6,000 and 0 14C yr B.P. (2000)
Edwards, M.E., Anderson, P.M., Brubaker, L.B., Ager, T.A., Andreev, A.A., Et Al.
Davis, Margaret Bryan, Brubaker, L. B., Beiswenger, J. M.
Pollen in surface sediments from five lakes in southern Michigan shows evidence of differential deposition. In most lakes, pollen from ragweed occurs in a higher ratio to tree pollen in shallow-water...