热带亚热带植物学报
熱帶亞熱帶植物學報
열대아열대식물학보
Journal of Tropical and Subtropical Botany
2015年
6期
653-661
,共9页
韩世忠%高人%李爱萍%马红亮%尹云锋%司友涛%陈仕东%蔡献贺%程清平%郑群瑞
韓世忠%高人%李愛萍%馬紅亮%尹雲鋒%司友濤%陳仕東%蔡獻賀%程清平%鄭群瑞
한세충%고인%리애평%마홍량%윤운봉%사우도%진사동%채헌하%정청평%정군서
中亚热带%米槠天然林%微生物群落%磷脂脂肪酸
中亞熱帶%米櫧天然林%微生物群落%燐脂脂肪痠
중아열대%미저천연림%미생물군락%린지지방산
Mid-subtropics%Castanopsis carlesii Nature forest%Microbial community%PLFAs
为了解土壤微生物群落的结构,采用磷脂脂肪酸方法对武夷山和建瓯的米槠(Castanopsis carlesii)天然林土壤微生物群落的结构多样性进行了研究。结果表明,两地米槠天然林的土壤微生物群落组成十分丰富,多样性指数、丰富度指数和均匀度指数分别为2.92~3.01、25.84~28.23和0.88~0.90。0~10 cm土层的磷脂脂肪酸总量、细菌特征脂肪酸、真菌特征脂肪酸、放线菌特征脂肪酸、革兰氏阳性菌和阴性菌特征脂肪酸含量均高于10~20 cm土层的,且建瓯万木林自然保护区的高于武夷山国家级自然保护区。10~20 cm土层的革兰氏阳性菌/革兰氏阴性菌高于0~10 cm土层的;细菌特征脂肪酸含量显著高于真菌,表明细菌在土壤微生物群落结构中处于优势地位。主成分分析表明,土壤微生物群落结构的差异主要是由采样地点的不同引起。
為瞭解土壤微生物群落的結構,採用燐脂脂肪痠方法對武夷山和建甌的米櫧(Castanopsis carlesii)天然林土壤微生物群落的結構多樣性進行瞭研究。結果錶明,兩地米櫧天然林的土壤微生物群落組成十分豐富,多樣性指數、豐富度指數和均勻度指數分彆為2.92~3.01、25.84~28.23和0.88~0.90。0~10 cm土層的燐脂脂肪痠總量、細菌特徵脂肪痠、真菌特徵脂肪痠、放線菌特徵脂肪痠、革蘭氏暘性菌和陰性菌特徵脂肪痠含量均高于10~20 cm土層的,且建甌萬木林自然保護區的高于武夷山國傢級自然保護區。10~20 cm土層的革蘭氏暘性菌/革蘭氏陰性菌高于0~10 cm土層的;細菌特徵脂肪痠含量顯著高于真菌,錶明細菌在土壤微生物群落結構中處于優勢地位。主成分分析錶明,土壤微生物群落結構的差異主要是由採樣地點的不同引起。
위료해토양미생물군락적결구,채용린지지방산방법대무이산화건구적미저(Castanopsis carlesii)천연림토양미생물군락적결구다양성진행료연구。결과표명,량지미저천연림적토양미생물군락조성십분봉부,다양성지수、봉부도지수화균균도지수분별위2.92~3.01、25.84~28.23화0.88~0.90。0~10 cm토층적린지지방산총량、세균특정지방산、진균특정지방산、방선균특정지방산、혁란씨양성균화음성균특정지방산함량균고우10~20 cm토층적,차건구만목림자연보호구적고우무이산국가급자연보호구。10~20 cm토층적혁란씨양성균/혁란씨음성균고우0~10 cm토층적;세균특정지방산함량현저고우진균,표명세균재토양미생물군락결구중처우우세지위。주성분분석표명,토양미생물군락결구적차이주요시유채양지점적불동인기。
In order to understand the soil microbial community structure, its diversities of Castanopsis carlesii forests in Wuyi Mountain and Jian’ou Wanmulin Nature Reserves at northern Fujian, eastern China were investigated by phospholipid fatty acid (PLFAs) method. The results showed that soil microbial community composition in C. carlesii forest was rich, the diversity index, richness index and evenness index of soil microbial communities for the two forests were 2.92–3.01, 25.84–28.23 and 0.88–0.90, respectively. The total PLFAs, bacterial PLFAs, fungal PLFAs, actinomycete PLFAs, gram-positive bacterial PLFAs, and gram-negative bacterial PLFAs at soil depth of 0–10 cm were higher than those of 10–20 cm, and those in Jian’ou were higher than those in Wuyi Mountain. The ratio of gram-positive bacterial PLFAs to gram-negative bacterial PLFAs at soil depth of 10–20 cm was higher than that of 0–10 cm. In each soil layer, the content of bacterial PLFAs was signiifcantly higher than those of fungal PLFAs, accounting for 46.0%–50.2%and 10.0%–11.5%, respectively, indicating that bacteria were dominated in soil microbial community. Principal component analysis showed that the difference in soil microbial community structure came from the sampling site.