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Here we present orbitally-resolved records of terrestrial higher plant leaf wax input to the North Atlantic over the last 3.5Ma, based on the accumulation of long-chain n-alkanes and n-alkanl-1-ols at IODP Site U1313. These lipids are a major component of dust, even in remote ocean areas, and have a predominantly aeolian origin in distal marine sediments. Our results demonstrate that around 2.7million...
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