Throughout the Holocene, the δ 7 Li LK signal (LK: lake sediments) displays a decreasing trend from ca. 9.4 (−2.1 ‰) to ca. 5.6 kyrcal BP (−3.2 ‰).
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Human and climate impacts on the alpine Critical Zone over the past 10,000 y.
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Throughout the Holocene, the δ 7 Li LK signal (LK: lake sediments) displays a decreasing trend from ca. 9.4 (−2.1 ‰) to ca. 5.6 kyrcal BP (−3.2 ‰).