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微生物对土壤冷却的反应可能解释了冬季微生物生物质的增加
Jörg Schnecker1, Felix Spiegel1, Yue Li2
1Centre for Microbiology and Environmental Systems Science, University of Vienna, Vienna, Austria.
概括
土壤微生物减少细胞分裂,但在冷却时保持葡萄糖的吸收,增加不和脂肪酸,为冬季做准备. 这种微生物反应可能解释了寒冷月份土壤碳增加.
科学领域:
- 土壤科学 土壤科学
- 微生物学 微生物学
- 生物地质化学生物地质化学
背景情况:
- 温带,北极和北极土壤中的微生物生物量通常在冬季增加,在春季减少.
- 这种季节性微生物碳波动可能会在冬季稳定土壤碳.
- 潜在的机制 (生理学,社区转移,基质分配) 仍然不清楚.
研究的目的:
- 研究微生物生理和碳分配对冷却的反应.
- 确定土壤冷却是否影响微生物呼吸,生长和葡萄糖吸收.
- 了解土壤微生物如何为冬季条件做好准备.
主要方法:
- 温带森林和耕地土壤的实验室化.
- 降温土壤从11°C降低到1°C.
- 通过O-纳入DNA测量微生物生长.
- 将C标记的葡萄糖追溯到生物质,CO2和脂脂肪酸 (PLFA).
主要成果:
- 土壤冷却显著减少了微生物生长和细胞分裂.
- 总呼吸量下降,但葡萄糖吸收和葡萄糖衍生呼吸量保持不变.
- 微生物在较低温度下增加了对不和PLFA的投资,增强了膜流动性.
- 尽管细胞分裂减少,但仍观察到持续的葡萄糖吸收.
结论:
- 土壤微生物对冷却表现出即时的生理反应,可能为结做准备.
- 改变碳分配 (增加不和脂肪酸) 是对寒冷的关键适应.
- 碳吸收和细胞分裂之间的差异可能解释微生物生物质碳的冬季积累.
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