A framework for interpreting paleoclimatic variations in Eastern Beringia
- 1 January 1991
- journal article
- Published by Elsevier in Quaternary International
- Vol. 10-12, 73-83
- https://doi.org/10.1016/1040-6182(91)90041-l
Abstract
No abstract availableThis publication has 29 references indexed in Scilit:
- A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulationNature, 1989
- Orbital variations, climate and paleoecologyTrends in Ecology & Evolution, 1989
- Ice Core Evidence for Extensive Melting of the Greenland Ice Sheet in the Last InterglacialScience, 1989
- Climate model simulations of the equilibrium climatic response to increased carbon dioxideReviews of Geophysics, 1987
- Late Pleistocene time series of atmospheric and oceanic variables recorded in sediments from the Subarctic PacificPaleoceanography and Paleoclimatology, 1987
- The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximumClimate Dynamics, 1987
- Correlation of quaternary glacial deposits in AlaskaQuaternary Science Reviews, 1986
- A theoretical framework for the Pleistocene ice agesJournal of the Geological Society, 1985
- Simulation of the climate of 18,000 years BP: Results for the North American/North Atlantic/European sector and comparison with the geologic record of North AmericaQuaternary Science Reviews, 1985
- Long-Term Variations of Caloric Insolation Resulting from the Earth's Orbital ElementsQuaternary Research, 1978