It has long been known that mountain glaciers and continental ice sheets around the globe
reached their respective maximum extent at different times during the last glacial cycle, often …

This paper reconstructs the deglaciation of the Laurentide Ice Sheet (LIS; including the
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …

Since the recognition in the mid-19th century that glaciers had been considerably more
extensive than at present, the Quaternary (Pleistocene and Holocene series) has been …

The most recent deglaciation of the North American Ice Sheet Complex (NAISC: comprising
the Innuitian, Cordilleran, and Laurentide ice sheets) offers a broad perspective from which …

Recent archaeological and paleoecological work along both interior and coastal routes for
early colonization of the New World has suggested that the interior route was impossible …

Studies of past glacial cycles yield critical information about climate and sea-level (ice-
volume) variability, including the sensitivity of climate to radiative change, and impacts of …

Ice volume during the last ten 100 ka glacial cycles was driven by solar radiation flux in the
Northern Hemisphere. Early minima in solar radiation combined with critical levels of …

Global glaciations have varied in size and magnitude since the Early–Middle Pleistocene
transition (~ 773 ka), despite the apparent regular and high-amplitude 100 ka pacing of …

Past glacials can be thought of as natural experiments in which variations in boundary
conditions influenced the character of climate change. However, beyond the last glacial, an …

Stocking of fish is an important tool for maintaining fisheries but can also significantly alter
population genetic structure and erode the portfolio of within‐species diversity that is …