Leads, lags, or synchronies in climatic events among different regions are key to
understanding mechanisms of climate change, as they provide insights into the causal …

The Quaternary is synonymous with extensive glaciation of Earth's mid-and high-latitudes.
Although there were local precursors, significant glaciation began in the latest Eocene (ca …

To better understand our present-day climate and its future, paleoclimatologists are
searching the past for analogues or even warmer periods than our present interglacial. For …

Glacial maxima and their terminations provide key insights into inter-hemispheric climate
dynamics and the coupling of atmosphere, surface and deep ocean, hydrology, and …

Comparison of large-scale temperature reconstructions over the past millennium reveals
agreement on major climatic episodes, but substantial divergence in reconstructed …

Global and hemispheric temperature reconstructions provide an important means of placing
recent anthropogenic temperature trends in the context of preindustrial climate variations …

Earth's climate has oscillated between short-lived interglacial and extended glacial periods
for the past million years. Before the last interglacial, absolutely dated markers of sea level …

The late Paleozoic icehouse was the longest-lived ice age of the Phanerozoic, and its
demise constitutes the only recorded turnover to a greenhouse state. This review …

The conventional view of the late Paleozoic ice age is that it was a single long, protracted
event some tens of millions of years in duration, with some internal waxing and waning of …

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 …