A. V. Lozhkin

Publication List Details

Period

2003 - 2009

Number

9

Co-Authors

Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia (2008)

H.D. Kokorowski, P.M. Anderson, R.S. Sletten, A.V. Lozhkin, T.A. Brown

Palynological (species assemblage, pollen accumulation rate), geochemical (carbon to nitrogen ratios, organic carbon and biogenic silica content), and sedimentological (particle size, magnetic...

Climate change and Arctic ecosystems: 1. Vegetation changes north of 55 degrees N between the last glacial maximum, mid-Holocene, and present (2003)

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...

Climate change and Arctic ecosystems: 2. Modeling, paleodata-model comparisons, and future projections (2003)

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...

Climate change and Arctic ecosystems: 2. Modeling, paleodata-model comparisons, and future projections (2003)

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...

Climate change and Arctic ecosystems: 2. Modeling, paleodata-model comparisons, and future projections (2003)

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...