Evolution of pastoralism in Southern Greenland during the last two millennia reconstructed from bile acids and coprophilous fungal spores in lacustrine sediments

Therefore, these quantitative correlations between DOC flux and coprophilous fungal spores flux potentially suggest a quantitative relationship with the livestock grazing in the catchment. The comparison between sedimentary DOC and coprophilous fungal spores provides significant highlights on past pastoral dynamics over the last 2000 yr in SW Greenland.