The TOC and TN contents showed an increasing trend along the glacier chronosequence, while NH 4 + -N and NO 3 – -N contents showed a decreasing trend, at line middle and line top, respectively ( Supplementary Figure 1 ).
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Prokaryotic Community Succession in Bulk and Rhizosphere Soils Along a High-Elevation Glacier Retreat Chronosequence on the Tibetan Plateau.
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