Shen Ju-Pei, Zhang Li-Mei, He Ju-Pei
State Key Laboratory of Urban and Regional Ecology, Research Centre for Eco-environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.
Ying Yong Sheng Tai Xue Bao. 2011 Nov;22(11):2996-3002.
Eukaryota, bacteria and archaea are the three domains of life. As the third domain of life, archaea has been found not only in extreme environments such as high-temperature, high-saline, and extremely acid habitats, but also in moderate environments including ocean, lake and soil, which implies that archaea may contribute greatly to various ecosystems. By targeting the 16S rRNA gene with real-time PCR approaches, this paper studied the abundance of archaea, crenarchaea and bacteria from two agricultural soil profiles and two long-term fertilization stations Qiyang (QY) and Fengqiu (FQ). The 16S rRNA gene copy number of crenarchaea was 1-2 orders of magnitude lower than that of archaea, and the order of these three groups was crenarchaea < archaea < bacteria. The ratios of both archaea and crenarchaea to bacteria increased with soil depth. The abundance of archaea and crenarchaea had significantly different responses to different fertilization treatments. In QY station, the copy numbers of archaeal and bacterial 16S rRNA gene had significant positive correlations with soil pH (r = 0.850, P < 0.01 and r = 0.676, P < 0.05, respectively); in FQ station, all the 16S rRNA gene copy numbers of archaea, crenarchaea and bacteria had no significant correlations with soil pH, but significantly correlated with soil organic matter (r = 0.783, P < 0.05; r = 0. 827, P < 0.05; r = 0.767, P < 0.05, respectively). To understand the distribution of archaea and crenarchaea in agricultural soil could provide important information to evaluate their ecological functions in soil ecosystem and element cycling.
真核生物、细菌和古菌是生命的三个域。作为生命的第三个域,古菌不仅存在于高温、高盐和极端酸性等极端环境中,也存在于海洋、湖泊和土壤等温和环境中,这表明古菌可能对各种生态系统有很大贡献。本文通过实时荧光定量PCR技术靶向16S rRNA基因,研究了两个农业土壤剖面以及祁阳(QY)和封丘(FQ)两个长期施肥站点中古菌、泉古菌和细菌的丰度。泉古菌的16S rRNA基因拷贝数比古菌低1-2个数量级,这三类菌群的顺序为泉古菌<古菌<细菌。古菌和泉古菌与细菌的比例均随土壤深度增加。古菌和泉古菌的丰度对不同施肥处理有显著不同的响应。在祁阳站点,古菌和细菌16S rRNA基因的拷贝数与土壤pH呈显著正相关(分别为r = 0.850,P < 0.01和r = 0.676,P < 0.05);在封丘站点,古菌、泉古菌和细菌的所有16S rRNA基因拷贝数与土壤pH均无显著相关性,但与土壤有机质显著相关(分别为r = 0.783,P < 0.05;r = 0.827,P < 0.05;r = 0.767,P < 0.05)。了解古菌和泉古菌在农业土壤中的分布,可为评估它们在土壤生态系统和元素循环中的生态功能提供重要信息。