Ancient hunters who stalked the world’s last woolly mammoths likely helped warm the Earth’s far northern latitudes thousands of years before humans began burning fossil fuels, according to a study of prehistoric climate change.
The demise of the leaf-chomping woolly mammoths contributed to a proliferation of dwarf birch trees in and around the Arctic, darkening a largely barren, reflective landscape and accelerating a rise in temperatures across the polar north, researchers at the Carnegie Institution for Science concluded.
The northward march of vegetation affected the climate because of the “albedo effect,” in which replacement of white snow and ice with darker land surfaces absorbs more sunlight and creates a self-repeating warming cycle, the study found.
The end of the last Ice Age, marked by a worldwide rise in temperatures and the dramatic retreat of glaciers that once covered much of the Northern Hemisphere, was already under way when the extinction of woolly mammoths began.
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