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U.S. National Science Foundation


Boreal forests in Alaska becoming more flammable

Researchers found that the composition of tree species in the Yukon Flats gradually shifted from coniferous trees to deciduous trees, which are more fire-resistant, during a warm period in the Holocene epoch. Current wildfire activity has already surpassed this limit, with the average fire frequency doubling in the last 50 years.

SourceU.S. National Science Foundation·JournalProceedings of the National Academy of Sciences·DateJul 24, 2013

Extreme algae blooms: The new normal?

A record-breaking algae bloom in Lake Erie was triggered by a combination of long-term agricultural practices and extreme weather events. The researchers predict that future blooms will be even more severe unless agricultural policies are revised to reduce nutrient runoff.

SourceU.S. National Science Foundation·JournalProceedings of the National Academy of Sciences·DateApr 10, 2013

Endangered lemurs' genomes sequenced

The complete genomes of three aye-aye lemur populations in Madagascar have been sequenced, revealing genetic diversity and historical separation. The research aims to prioritize conservation efforts for these critically endangered species, which are threatened by habitat loss and fragmentation.

SourceU.S. National Science Foundation·JournalProceedings of the National Academy of Sciences·DateMar 26, 2013

Antarctic and Arctic insects use different genetic mechanisms to cope with lack of water

Researchers discovered distinct gene expression patterns in Antarctic midge and Arctic springtail species, revealing unique strategies for coping with dehydration. The findings highlight the power of genomics in advancing polar science and uncovering previously undetected differences between these extreme ecosystems.

SourceU.S. National Science Foundation·JournalProceedings of the National Academy of Sciences·DateMar 12, 2013

Analysis of Greenland ice cores adds to historical record and provide glimpse into climate's future

A new study analyzing Greenland ice cores suggests that melting of the Antarctic ice sheet may have contributed more to sea-level rise than the Greenland ice sheet around 100,000 years ago. The research findings indicate a warmer-than-expected climate during the Eemian interglacial period, with surface temperatures about 8 degrees Cels...