Resistance of Permafrost and Modern Acinetobacter lwoffii Strains to Heavy Metals and Arsenic Revealed by Genome Analysis

Table 1

Characteristics of permafrost Acinetobacter lwoffii strains.

Strain	Age of sediment	Sampling locality
ED23-35	20–40 K	Kolyma Lowland, Bank of river Homus-Yuryiah, Late-Pleistocene-Ice-Complex
ED45-23	20–40 K	Kolyma Lowland, Bank of river Homus-Yuryiah, Late-Pleistocene-Ice-Complex
ЕD9-5а	15–30 K	Kolyma Lowland, Bank of river Homus-Yuryiah, Late-Pleistocene-Ice-Complex
ЕК30А	1,6–1,8 M	Kolyma Lowland, Bank of river Konkovaya, Early Pleistocene
VS15	2-3 M	Kolyma Lowland, Bank of river Grand Chukochia, Late-Pleistocene-Ice-Complex

Age of subsoil permafrost sediments (corresponding to the period of freezing before the present) in years: K = 10³ years; M = 10⁶ years.