甲类共生体为泥炭沼泽地区的光合作用提供碳
Ashna A Raghoebarsing1, Alfons J P Smolders, Markus C Schmid
1Department of Microbiology, Radboud University Nijmegen, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands.
Nature
|August 27, 2005
概括
湿地通过Sphagnum和甲性细菌之间的共生来回收甲. 这一过程有效地将甲转化为二氧化碳,然后Sphagnum将其用作碳源.
科学领域:
- 环境科学 环境科学
- 微生物学 微生物学
- 植物科学 植物科学
背景情况:
- 湿地是大气中甲的主要天然来源,甲是一种强大的温室气体.
- 在湿地产生的大部分甲都在内部回收,但人们对这种机制的了解很少.
- 有效的甲氧化对于调节温室气体排放至关重要.
研究的目的:
- 调查湿地中甲回收的生物地质化学控制.
- 为了确定藻在甲消耗中的作用.
- 为了阐明植物和甲氧化细菌之间的共生关系.
主要方法:
- 利用分子探针检测Sphagnum的组织中的细菌.
- 使用 (13) C标记的甲进行了化实验.
- 追踪了甲衍生的碳融入植物化合物的过程.
主要成果:
- 证实了Sphagnum (氨酸细胞和干叶) 中甲菌的存在.
- 通过这些细菌,证明了甲在现场快速氧化为二氧化碳.
- 表明,斯法gnum利用产生的二氧化碳作为一个重要的碳来源 (10-15%).
结论:
- 斯法gnum 和甲性细菌之间的共生关系推动了有效的 in situ 甲回收.
- 这种共生解释了这些生态系统中有效的甲消耗和高的有机碳埋葬.
- 甲是斯法gnum的重要碳来源,影响湿地生物地质化学.
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