A study published in Science reveals that the Laurentide Ice Sheet, a major Pleistocene ice sheet, reached its smallest size about 3,600 years ago. Subsequently, it began to re-expand roughly 2,000 years ago, a process interpreted as the onset of a new glaciation period. This re-expansion continued until approximately 1960.
The research indicates that human-caused climate warming reversed the natural re-expansion of the ice sheet around 1960. This suggests that a potential new ice age was underway before being interrupted by anthropogenic climate change.
The Barnes Ice Cap, located on Baffin Island in the Canadian Arctic, provided the direct physical evidence for these findings. It is the last remnant of the Laurentide Ice Sheet. Nicolás Young, a geologist at Columbia University’s Lamont-Doherty Earth Observatory and lead author, explained that the cap's unique characteristics allowed for the preservation of this historical record.
Unlike most warm-based glaciers that slide and erode underlying material, the Barnes Ice Cap is cold-based. This means it is frozen directly onto the bedrock, preventing movement and preserving the ground beneath it. Tundra plants that colonized the ground after the initial retreat were smothered and preserved when the ice re-advanced, allowing researchers to date the re-expansion using two independent methods.
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Research on the Barnes Ice Cap indicates that the Laurentide Ice Sheet began re-expanding approximately 2,000 years ago, suggesting the start of a new glaciation. This natural re-expansion was reversed around 1960 due to human-caused climate warming. The findings provide direct physical evidence of past ice sheet dynamics.