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Characteristics of magnetotactic bacteria in Duanjiapo loess section, Shaanxi Province and their environment significance

机译:陕西段家坡黄土段趋磁细菌的特征及其环境意义

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Magnetotactic bacteria (MB) have been isolated from 61 samples which have been collected from S0, L1, S1 and L2 layers in the Duanjiapo loess section. A few MB ( < 25 cell counts per sieve mesh) have been found in loess layers (L1, L2), bow-shaped, each cell containing only two magnetosomes, while much more MB ( > 125 cells counts per sieve mesh) have been found from paleosol layers (S0, S1), rod-shaped, each cell containing 8-26 magnetosomes arranged in irregular chains. Magnetosomes with Fe and Co as the main metallic elements are spheroid-shaped, and mainly round in cross-section. Normal saturated fatty acids in MB ranged from C_(14) to C_(28); almost no monounsaturated fatty acids have been identified. Most suitable oxygen content for MB growing is 10%, and low concentration of organic salt (0.02 mmol/L qunisic iron) is beneficial to the forming of magnetosomes. Results suggest that the paleosol development stage is suitable for the growing of MB and the climate fluctuation periods for magnetosomes formation.
机译:从61个样品中分离出趋磁细菌(MB),这些样品是从段家坡黄土段的S0,L1,S1和L2层收集的。在弓形的黄土层(L1,L2)中发现了几个MB(每个筛孔网格少于25个细胞计数),每个细胞仅包含两个磁小体,而已经发现了更多的MB(每个筛孔网格大于125个细胞计数)。从杆状的古土壤层(S0,S1)中发现,每个细胞包含以不规则链排列的8-26个磁小体。以Fe和Co为主要金属元素的磁小体呈球状,横截面主要为圆形。 MB中的正常饱和脂肪酸范围为C_(14)至C_(28);几乎没有发现单不饱和脂肪酸。 MB生长最合适的氧含量为10%,低浓度的有机盐(0.02 mmol / L奎尼铁)有利于磁小体的形成。结果表明,古土壤的发育阶段适合MB的生长和磁小体形成的气候波动时期。

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