欢迎访问《生态学杂志》官方网站,今天是 分享到:

生态学杂志 ›› 2021, Vol. 40 ›› Issue (2): 381-391.doi: 10.13292/j.1000-4890.202102.002

• 研究报告 • 上一篇    下一篇

水位埋深和微地貌对金川泥炭土壤微生物活性及甲烷功能基因的影响

张雪冰1,2,孟迪1,2,陈蕾1,2,王梓橦1,2,杨倩楠1,2,常青1,2*,樊宪磊1,2   

  1. 1长白山地理过程与生态安全教育部重点实验室, 长春 130024;2东北师范大学地理科学学院, 长春 130024)
  • 出版日期:2021-02-10 发布日期:2021-07-09

Effects of depth to water table and micro-topography on microbial activity and methane functional genes of peat bog in Jinchuan.

ZHANG Xue-bing1,2, MENG Di1,2, CHEN Lei1,2, WANG Zi-tong1,2, YANG Qian-nan1,2, CHANG Qing1,2*, FAN Xian-lei1,2, LIU Zi-ping1,2, BAI E1,2*   

  1. (1Key Laboratory of Geographical Processes and Ecological Security in Changbai Mountains, Ministry of Education, Changchun 130024, China; 2School of Geographical Sciences, Northeast Normal University, Changchun 130024, China).
  • Online:2021-02-10 Published:2021-07-09

摘要: 泥炭沼泽是长期储存碳最有效的陆地生态系统。水文特征和微地貌可能会通过调控微生物群落和功能影响泥炭地碳储存。本研究以长白山金川泥炭沼泽为研究对象,选取-10、-1、0、4、10、13、14和18 cm八个水位埋深,并在各水位埋深点采集臌囊薹草(Carexs chmidtii)草丘和丘间微地貌的土壤样品,以探究水位埋深和微地貌对土壤微生物量碳氮、酶活性及甲烷功能基因的影响。结果表明:微生物量碳氮受水位埋深影响因土壤层不同而不同,两者在草丘30~45 cm和丘间0~15 cm土壤层呈显著正相关。土壤碳氮循环相关的酶(β-1,4-葡萄糖苷酶和β-1,4-N-乙酰葡糖胺糖苷酶)活性与水位埋深呈显著正相关且受土壤层调控,磷酸酶活性与水位埋深无关。此外,水位埋深与甲烷还原菌丰度(每克干土的mcrA功能基因拷贝数)呈显著负相关,而与甲烷氧化菌丰度(每克干土的pmoA功能基因拷贝数)呈显著正相关,且水位埋深对甲烷还原菌丰度的影响更大。草丘微地貌显著影响微生物量碳,同为15~30 cm土壤层,其含量表现为草丘>丘间;处于相同海拔的草丘15~30 cm和丘间0~15 cm,其含量表现为丘间>草丘。草丘微地貌也显著影响甲烷氧化菌丰度,同为15~30 cm土壤层,甲烷氧化菌丰度表现为草丘>丘间。本研究表明,泥炭地空间异质性对微生物活性具有重要影响,从定点研究到大尺度估算的尺度放大过程中,应对这一现象充分考虑。

关键词: 微生物量碳氮, 酶活性, mcrA基因, pmoA基因

Abstract: Peat bogs are the most effective terrestrial ecosystems for long-term carbon storage. Hydrologic characteristics and micro-topography may affect carbon storage in peatlands by regulating the composition and function of microbial communities. In the site located in the peat bog of Jinchuan in Changbai Mountain, we collected soil samples in hummock and hollow of Carex schmidtii from eight different levels of the depth to water table (-10, -1, 0, 4, 10, 13, 14 and 18 cm), to explore the effects of depth to water table and microtopography on soil microbial biomass carbon and nitrogen, enzyme activity, and methane functional genes. Results showed that the effects of the depth to water table on the content of microbial biomass carbon and nitrogen differed across different soil layers, with a significant positive correlation with microbial biomass carbon and nitrogen in the 30-45 cm soil layer of hummock and the 0-15 cm soil layer of hollow. The activities of enzymes (β-1,4-glucosidase and β-1,4-Nacetylglucosamine glycosidase) related with soil carbon and nitrogen cycling were significantly positively correlated with the depth to water table and regulated by soil layer, while the phosphatase activities were not correlated with the depth to water table. In addition, the depth to water table had a significant negative correlation with the abundance of methanogenesis bacteria (the copy number of mcrA functional gene per gram dry soil), and a significant positive correlation with the abundance of methaneoxidizing bacteria (the copy number of pmoA functional gene per gram dry soil), with a stronger effect of the depth to water table on the abundance of methanogenesis bacteria. The microtopography significantly affected microbial biomass carbon and nitrogen, with higher microbial biomass carbon and nitrogen in hummock than in hollow at the same 15-30 cm soil layer and higher microbial biomass carbon in 15-30 cm soil layer of hollow than in 0-15 cm soil layer of hummock. Themicro topography significantly affected the abundance of methaneoxidizing bacteria, which was higher in hummock than in hollow in the same 15-30 cm soil layer. Our results indicated that the spatial heterogeneity of peatlands would affect microbial activity, which should be fully considered in scaling up the results from local to large scale.

 

Key words: microbial biomass carbon and nitrogen, enzyme activity, mcrA gene, pmoA gene.