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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.

Detalles Bibliográficos
Autores principales: Vishnivetskaya, Tatiana, Spirina, Elena, Shmakova, Lyubov, Tutukina, Maria, Li, Zhou, Wu, Xiaofen, Rivkina, Elizaveta
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Society for Microbiology 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6813392/
https://www.ncbi.nlm.nih.gov/pubmed/31649080
http://dx.doi.org/10.1128/MRA.01010-19
Descripción
Sumario: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.