Late quaternary dynamics of arctic biota from ancient environmental genomics

HIGHLIGHTS

• who: from the Sampling, chronology and eDNA taphonomy Sampling and subsampling methods are described in Supplementary Information Sample ages were determined through conventional or accelerator mass spectrometer radiocarbon ( C) as well as optically stimulated luminescence. In total, radiocarbon ages and , optically stimulated luminescence dates were used. For sedimentary sections with multiple contiguous dates without stratigraphic inversions, age-depth models were built to calculate sedimentation rates and estimate the ages of undated samples within these sections. All radiocarbon ages are in calibrated years before present, calibrated using IntCal, (ref., ). Chronological information is provided in Supplementary Information , and Supplementary . . .
  

   

  

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