Visual matches and statistical tests suggest correlations between marine isotope curves,
retrodictive solar insolation at lat 65° N, and magnetic susceptibility profiles through late …

Glaciers cover only about 5 percent of Alaska today, but they spread over as much as half of
the state during the most widespread advances of the late Cenozoic (Fig. 1). Both modern …

The ancient, boreal Eva forest forms the centerpiece in this evaluation of the time and nature
of the enfironment during an interglaciation. This title brings together results of exmaination …

The effects of predicted anthropogenic warming can be assessed in part by documenting
responses to past warming events. One of the most pronounced warmings was the last …

At least 20 localities in Alaska contain deposits that may provide information on the last
interglaciation (Oxygen-Isotope Substage 5e). These widely dispersed localities include …

Gravels deposited by the ancestral Yukon River are preserved in terrace remnants on the
margins of the Yukon River valley near the village of Circle in east-central Alaska. Plant …

A 12-m sequence of lake sediment and peat in a 45-m high exposure on Birch Creek,
northeast Alaska, contains pollen of Picea, Betula, Alnus and Populus, and wood of Picea …

A 20-cm-thick volcanic ash layer at the Palisades along the Yukon River is geochemically
correlated with the Old Crow tephra. A buried organic and wood-rich layer above the Old …

The paleoclimatic informations preserved at some selected sites from high northern latitudes
correlative with the last interglacial maximum of Isotopic Substage 5e have been compiled …

Two sites within the boreal forest of interior Alaska shed light on the climate and vegetation
of terminal marine isotope stage (MIS) 6 (ca. 140–130 kyr ago) and MIS 5e (125–116 kyr …