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产甲烷古菌与水稻根上依赖二氧化碳的甲烷生成

Methanogenic archaea and CO2-dependent methanogenesis on washed rice roots.

作者信息

Lehmann-Richter S, Grosskopf R, Liesack W, Frenzel P, Conrad R

机构信息

Max-Planck-Institut für terrestrische Mikrobiologie, Marburg, Germany.

出版信息

Environ Microbiol. 1999 Apr;1(2):159-66. doi: 10.1046/j.1462-2920.1999.00019.x.

Abstract

Washed excised roots of rice (Oryza sativa) immediately started to produce CH4 when they were incubated in phosphate buffer under anoxic conditions (N2 atmosphere), with initial rates varying between 2 and 70nmolh(-1)g(-1) dry weight of root material (mean +/- SE: 20.3 +/- 5.9 nmol h(-1) g(-1) dry weight; n = 18). Production of CH4 continued for at least 500 h, with rates usually decreasing slowly. CH4 production was not significantly affected by methyl fluoride, an inhibitor of acetoclastic methanogenesis. Less than 0.5% of added [2-14C]-acetate was converted to 14CH4, and conversion of 14CO2 to 14CH4 indicated that CH4 was almost exclusively produced from CO2. Occasionally, however, especially when the roots were incubated without additional buffer, CH4 production started to accelerate after about 200h reaching rates of > 100 nmol h(-1) g(-1) dry weight. Methyl fluoride inhibited methanogenesis by more than 20% only in these cases, and the conversion of 14CO2 to 14CH4 decreased. These results indicate that CO2-dependent rather than acetoclastic methanogenesis was primarily responsible for CH4 production in anoxically incubated rice roots. Determination of most probable numbers of methanogens on washed roots showed highest numbers (10(6)g(-1) dry roots) on H2 and ethanol, i.e. substrates that support CH4 production from CO2. Numbers on acetate (10(5) g(-1) dry roots) and methanol (10(4)g(-1) dry roots) were lower. Methanogenic consortia enriched on H2 and ethanol were characterized phylogenetically by comparative sequence analysis of archaeal small-subunit (SSU) ribosomal RNA-encoding genes (rDNA). These sequences showed a high similarity to SSU rDNA clones that had been obtained previously by direct extraction of total DNA from washed rice roots. The SSU rDNA sequences recovered from the H2/CO2-using consortium either belonged to a novel lineage of methanogens that grouped within the phylogenetic radiation of the Methanosarcinales and Methanomicrobiales or were affiliated with Methanobacterium bryantii. SSU rDNA sequences retrieved from the ethanol-using consortium either grouped within the genus Methanosarcina or belonged to another novel lineage within the phylogenetic radiation of the Methanosarcinales and Methanomicrobiales. Cultured organisms belonging to either of the two novel lineages have not been reported yet.

摘要

将水稻(Oryza sativa)切除的根系洗净后,在缺氧条件下(氮气环境)于磷酸盐缓冲液中孵育时,立即开始产生甲烷,初始速率在2至70 nmol h⁻¹ g⁻¹根干重之间变化(平均值±标准误:20.3±5.9 nmol h⁻¹ g⁻¹干重;n = 18)。甲烷产生持续至少500小时,速率通常缓慢下降。氟甲烷是乙酸裂解产甲烷作用的抑制剂,但其对甲烷产生没有显著影响。添加的[2-¹⁴C] - 乙酸中转化为¹⁴CH₄的比例不到0.5%,¹⁴CO₂转化为¹⁴CH₄表明甲烷几乎完全由CO₂产生。然而,偶尔,特别是当根系在没有额外缓冲液的情况下孵育时,甲烷产生在约200小时后开始加速,速率超过100 nmol h⁻¹ g⁻¹干重。仅在这些情况下,氟甲烷抑制产甲烷作用超过20%,并且¹⁴CO₂转化为¹⁴CH₄的比例降低。这些结果表明,在缺氧孵育的水稻根系中,依赖CO₂而非乙酸裂解的产甲烷作用是甲烷产生的主要原因。对洗净根系上产甲烷菌的最可能数量的测定表明,在氢气和乙醇上数量最高(10⁶ g⁻¹根干重),即支持从CO₂产生甲烷的底物。在乙酸(10⁵ g⁻¹根干重)和甲醇(10⁴ g⁻¹根干重)上的数量较低。通过对古菌小亚基(SSU)核糖体RNA编码基因(rDNA)的比较序列分析,对在氢气和乙醇上富集的产甲烷菌群落进行了系统发育特征分析。这些序列与先前通过从洗净的水稻根系中直接提取总DNA获得的SSU rDNA克隆具有高度相似性。从利用H₂/CO₂的菌群落中回收的SSU rDNA序列要么属于产甲烷菌的一个新谱系,该谱系聚集在甲烷八叠球菌目和甲烷微菌目的系统发育辐射范围内,要么与布氏甲烷杆菌相关。从利用乙醇的菌群落中检索到的SSU rDNA序列要么聚集在甲烷八叠球菌属内,要么属于甲烷八叠球菌目和甲烷微菌目的系统发育辐射范围内的另一个新谱系。尚未报道属于这两个新谱系中的任何一个的培养生物。

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