Sedimentary ancient DNA, fecal biomarker, and tephrochronology from Eidisvatn, Faroe Islands

This dataset includes sedimentary ancient DNA, lipid biomarker, and tephra geochemical data from a lake sediment core from the Faroe Islands. The purpose of the study was to characterize the signature of human influence on the landscape via lake sediment analysis, and to determine the timing of huma...

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Bibliographic Details
Main Authors: Curtin, Lorelei, D'Andrea, William J, Balascio, Nicholas L, Shirazi, Sabrina, Shapiro, Beth, Gregory, de Wet, Bradley, Raymond S, Bakke, Jostein
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
Biomarker
DNA
EI-D-01-15
EI-P-01-15
Faroe Islands
GC
Gravity corer
Lake sediment core
PC
Piston corer
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.939311
https://doi.org/10.1594/PANGAEA.939311
Description
Summary:This dataset includes sedimentary ancient DNA, lipid biomarker, and tephra geochemical data from a lake sediment core from the Faroe Islands. The purpose of the study was to characterize the signature of human influence on the landscape via lake sediment analysis, and to determine the timing of human arrival to the Faroe Islands. To achieve this, we analyzed fecal sterols, which are lipid biomarkers that are produced by the mammalian gut microbiome and deposited on the land surface in feces. We also used metabarcoding techniques to determine the first appearance of ancient sheep DNA in the lake sedimentary sequence. The lake sediment core was recovered from Eidisvatn on the island of Esturoy (62.286194, -7.057611) in August of 2015. Radiocarbon and tephrochronology were used to constrain sediment core chronology. Radiocarbon samples were analyzed via accelerator mass spectrometry at either the Woods Hole NOSAMS facility or the University of California Irvine Keck AMS facility. We analyzed the geochemistry of five tephra layers using microprobe. We extracted lipid biomarkers from 68 core subsamples, and following column chromatography, fecal biomarkers were identified and quantified via GC-MSD at the Lamont-Doherty Earth Observatory. 14 sediment samples were analyzed in the University of California Santa Cruz Paleogenomics Center. Plant and mammal DNA were amplified from each sample, and libraries were sequenced via an Illumina NextSeq.

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