If these Spectral Type L418_d points are removed (and they may be one single feature since many of the signals are consecutive returns from the same point cloud transect), then there is a slight trend of a decrease in signal intensity for signals in glacial ice. 3.5.
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Subsurface <i>In Situ</i> Detection of Microbes and Diverse Organic Matter Hotspots in the Greenland Ice Sheet.
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