Metagenomes from Late Pleistocene Ice Complex Sediments of the Siberian Arctic
The late Pleistocene Ice Complex (also known as Yedoma) encompasses ice-rich permafrost formed when alluvial and/or aeolian sediments accumulated under cold climatic conditions. Three metagenomes obtained from Yedoma deposits continually frozen for periods up to 60,000 years are reported here.
Published in: | Microbiology Resource Announcements |
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Main Authors: | , , , , , , |
Format: | Text |
Language: | English |
Published: |
American Society for Microbiology
2019
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Subjects: | |
Online Access: | http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6813392/ http://www.ncbi.nlm.nih.gov/pubmed/31649080 https://doi.org/10.1128/MRA.01010-19 |
Summary: | The late Pleistocene Ice Complex (also known as Yedoma) encompasses ice-rich permafrost formed when alluvial and/or aeolian sediments accumulated under cold climatic conditions. Three metagenomes obtained from Yedoma deposits continually frozen for periods up to 60,000 years are reported here. |
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