Technische Universität München, Ingolstädter Landstrasse 1, 85764 Neuherberg, Germany.
Appl Environ Microbiol. 2011 Sep;77(17):6109-16. doi: 10.1128/AEM.01751-10. Epub 2011 Jul 15.
In many areas of China, tidal wetlands have been converted into agricultural land for rice cultivation. However, the consequences of land use changes for soil microbial communities are poorly understood. Therefore, we investigated bacterial and archaeal communities involved in inorganic nitrogen turnover (nitrogen fixation, nitrification, and denitrification) based on abundances and relative species richness of the corresponding functional genes along a soil chronosequence ranging between 50 and 2,000 years of paddy soil management compared to findings for a tidal wetland. Changes in abundance and diversity of the functional groups could be observed, reflecting the different chemical and physical properties of the soils, which changed in terms of soil development. The tidal wetland was characterized by a low microbial biomass and relatively high abundances of ammonia-oxidizing microbes. Conversion of the tidal wetlands into paddy soils was followed by a significant increase in microbial biomass. Fifty years of paddy management resulted in a higher abundance of nitrogen-fixing microbes than was found in the tidal wetland, whereas dominant genes of nitrification and denitrification in the paddy soils showed no differences. With ongoing rice cultivation, copy numbers of archaeal ammonia oxidizers did not change, while that of their bacterial counterparts declined. The nirK gene, coding for nitrite reductase, increased with rice cultivation time and dominated its functionally redundant counterpart, nirS, at all sites under investigation. Relative species richness showed significant differences between all soils with the exception of the archaeal ammonia oxidizers in the paddy soils cultivated for 100 and 300 years. In general, changes in diversity patterns were more pronounced than those in functional gene abundances.
在中国许多地区,潮滩湿地已经被转化为水稻种植的农业用地。然而,土地利用变化对土壤微生物群落的影响还知之甚少。因此,我们调查了参与无机氮转化(固氮、硝化和反硝化)的细菌和古菌群落,其依据是沿 50 至 2000 年稻田管理时间序列的相应功能基因的丰度和相对物种丰富度,与潮滩湿地的发现相比。可以观察到功能组的丰度和多样性的变化,反映了土壤的不同化学和物理性质,这些性质在土壤发育方面发生了变化。潮滩湿地的特点是微生物生物量低,氨氧化微生物的丰度相对较高。将潮滩湿地转化为稻田后,微生物生物量显著增加。50 年的稻田管理导致固氮微生物的丰度高于潮滩湿地,而稻田土壤中硝化和反硝化的主要基因没有差异。随着水稻的持续种植,古菌氨氧化菌的拷贝数没有变化,而其细菌对应物的拷贝数则下降。编码亚硝酸盐还原酶的nirK 基因随着水稻种植时间的增加而增加,并且在所有研究地点都超过了其功能冗余的 nirS 基因。除了种植 100 年和 300 年的稻田土壤中的古菌氨氧化菌外,所有土壤之间的相对物种丰富度都存在显著差异。总的来说,多样性模式的变化比功能基因丰度的变化更为显著。