Pollen‐based biomes for Beringia 18,000, 6000 and 0 14C yr bp†
- 1 May 2000
- journal article
- research article
- Published by Wiley in Journal of Biogeography
- Vol. 27 (3) , 521-554
- https://doi.org/10.1046/j.1365-2699.2000.00426.x
Abstract
No abstract availableKeywords
This publication has 72 references indexed in Scilit:
- Palaeovegetation of China: a pollen data‐based synthesis for the mid‐Holocene and last glacial maximumJournal of Biogeography, 2000
- Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP)Geophysical Research Letters, 1999
- Intercomparison of Simulated Global Vegetation Distributions in Response to 6 kyr BP Orbital ForcingJournal of Climate, 1998
- BIOME3: An equilibrium terrestrial biosphere model based on ecophysiological constraints, resource availability, and competition among plant functional typesGlobal Biogeochemical Cycles, 1996
- Potential role of vegetation feedback in the climate sensitivity of high‐latitude regions: A case study at 6000 years B.P.Global Biogeochemical Cycles, 1996
- Vegetation/Ecosystem Modeling and Analysis Project:Comparing biogeography and biogeochemistry models in a continental‐scale study of terrestrial ecosystem responses to climate change and CO2 doublingGlobal Biogeochemical Cycles, 1995
- Late Quaternary vegetational history of the Black River region in northeastern AlaskaCanadian Journal of Earth Sciences, 1988
- The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximumClimate Dynamics, 1987
- Late Wisconsin and Holocene vegetational history of the Upper Koyukuk region, Brooks Range, AKCanadian Journal of Botany, 1985
- Late Quaternary Vegetational and Climatic History of the Snag-Klutlan Area, Southwestern Yukon Territory, CanadaGSA Bulletin, 1971