Both δ 13 C and δ 15 N exhibited a decreasing trend, indicating an increasing abundance of lighter isotopes closer to the summit (mean δ 13 C: −24.68‰, δ 15 N: + 5.51‰).
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Polychlorinated Alkane Profiles and Concentrations in Bolivian Andes Soils Point to a Long-Range Transport Influence.
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