Boyle-Yarwood Stephanie A, Bottomley Peter J, Myrold David D
Departments of Crop and Soil Science, Oregon State University, Corvallis, Oregon, USA.
Environ Microbiol. 2008 Nov;10(11):2956-65. doi: 10.1111/j.1462-2920.2008.01600.x. Epub 2008 Apr 3.
This study determined nitrification activity and nitrifier community composition in soils under stands of red alder (Alnus rubra) and Douglas fir (Pseudotsuga menziesii) at two sites in Oregon. The H.J. Andrews Experimental Forest, located in the Cascade Mountains of Oregon, has low net N mineralization and gross nitrification rates. Cascade Head Experimental Forest, in the Coast Range, has higher net N mineralization and nitrification rates and soil pH is lower. Communities of putative bacterial [ammonia-oxidizing bacteria (AOB)] and archaeal [ammonia-oxidizing archaea (AOA)] ammonia oxidizers were examined by targeting the gene amoA, which codes for subunit A of ammonia monooxygenase. Nitrification potential was significantly higher in red alder compared with Douglas-fir soil and greater at Cascade Head than H.J. Andrews. Ammonia-oxidizing bacteria amoA genes were amplified from all soils, but AOA amoA genes could only be amplified at Cascade Head. Gene copy numbers of AOB and AOA amoA were similar at Cascade Head regardless of tree type (2.3-6.0 x 10(6)amoA gene copies g(-1) of soil). DNA sequences of amoA revealed that AOB were members of Nitrosospira clusters 1, 2 and 4. Ammonia-oxidizing bacteria community composition, determined by terminal restriction fragment length polymorphism (T-RFLP) profiles, varied among sites and between tree types. Many of the AOA amoA sequences clustered with environmental clones previously obtained from soil; however, several sequences were more similar to clones previously recovered from marine and estuarine sediments. As with AOB, the AOA community composition differed between red alder and Douglas-fir soils.
本研究测定了俄勒冈州两个地点的红桤木(Alnus rubra)林和花旗松林(Pseudotsuga menziesii)土壤中的硝化活性及硝化细菌群落组成。位于俄勒冈州喀斯喀特山脉的H.J.安德鲁斯实验林,其净氮矿化率和总硝化率较低。位于海岸山脉的喀斯喀特角实验林,其净氮矿化率和硝化率较高,且土壤pH值较低。通过靶向编码氨单加氧酶亚基A的amoA基因,检测了假定的细菌[氨氧化细菌(AOB)]和古菌[氨氧化古菌(AOA)]氨氧化菌群落。与花旗松土壤相比,红桤木土壤中的硝化潜力显著更高,且在喀斯喀特角比在H.J.安德鲁斯更高。所有土壤中均扩增出了氨氧化细菌的amoA基因,但仅在喀斯喀特角扩增出了AOA的amoA基因。无论树木类型如何,喀斯喀特角AOB和AOA amoA的基因拷贝数相似(土壤中2.3 - 6.0×10⁶个amoA基因拷贝 g⁻¹)。amoA的DNA序列显示AOB是亚硝化螺菌属簇1、2和4的成员。通过末端限制性片段长度多态性(T-RFLP)图谱确定的氨氧化细菌群落组成,在不同地点和不同树木类型之间存在差异。许多AOA amoA序列与先前从土壤中获得的环境克隆聚类;然而,有几个序列与先前从海洋和河口沉积物中回收的克隆更相似。与AOB一样,红桤木和花旗松土壤中的AOA群落组成也不同。