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deglaciation |
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| 14] BP (Barrie and Conway, 2002); deglaciation was very rapid with regional downwasting and widespread stagnation (Gullbault et al. Schneider detailed such speculative effects as a possible collapse of the North Atlantic thermohaline circulation (the Day After Tomorrow scenario, though on a much less dramatic timetable), and the deglaciation of polar ice sheets in Greenland and the West Antarctic, causing many feet of additional sea-level rise. If a species had populations in Eurasia and North America, it had a much better chance of making it through, even though Eurasia and North America were the two areas where the deglaciation was the most intense," says Alroy. |
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