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[贝加尔湖底部沉积物中的需氧甲烷营养菌群落]

[Aerobic methanotrophic communities in the bottom sediments of Lake Baikal].

作者信息

Gaĭnutdinova E A, Eshinimaev B Ts, Tsyrenzhapova I S, Dagurova O P, Suzina N E, Khmelenina V N, Namsaraev B B, Trotsenko Iu A

出版信息

Mikrobiologiia. 2005 Jul-Aug;74(4):562-71.

Abstract

The results of the first methodical investigation into the aerobic methanotrophic communities inhabiting the bottom sediments of Lake Baikal are reported. Use of the radioisotopic method revealed methane consumption in 12 10- to 50-cm-long sediment cores. The maximum methane consumption rates (495-737 microl/(dm3 day) were recorded in sediments in the regions of hydrothermal vents and oil and gas occurrence. Methane consumption was most active in the surface layers of the sediments (0-4 cm); it decreased with the sediment depth and became negligible or absent at depths below 20 cm. The number of methanotrophic bacteria usually ranged from 100 to 1000 cells/cm3 of sediment and reached 1 million cells/cm3 in the regions of oil and gas occurrence. The 17 enrichment cultures obtained were represented mainly by morphotype II methanotrophs. Phylogenetic analysis of the enrichment cultures in terms of the amino acid sequence of the alpha subunit of the membrane-bound methane monooxygenase revealed the predominance of methanotrophs of the genus Methylocystis. The results obtained suggest the presence of an active aerobic methanotrophic community in Lake Baikal.

摘要

报道了对贝加尔湖底部沉积物中需氧甲烷营养菌群落进行的首次系统调查结果。采用放射性同位素方法揭示了在12个长度为10至50厘米的沉积物岩芯中有甲烷消耗现象。在热液喷口以及油气赋存区域的沉积物中记录到了最高甲烷消耗率(495 - 737微升/(立方分米·天))。甲烷消耗在沉积物表层(0 - 4厘米)最为活跃;随着沉积物深度增加而降低,在20厘米以下深度可忽略不计或不存在。甲烷营养菌数量通常在每立方厘米沉积物100至1000个细胞范围内,在油气赋存区域达到每立方厘米100万个细胞。所获得的17个富集培养物主要由II型形态的甲烷营养菌组成。根据膜结合甲烷单加氧酶α亚基的氨基酸序列对富集培养物进行系统发育分析,结果显示甲基孢囊菌属的甲烷营养菌占主导地位。所获结果表明贝加尔湖存在活跃的需氧甲烷营养菌群落。

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