Marine Sciences Research Center, State University of New York, Stony Brook, New York 11794.
Appl Environ Microbiol. 1983 May;45(5):1586-91. doi: 10.1128/aem.45.5.1586-1591.1983.
The effects of several metals on microbial methane, carbon dioxide, and sulfide production and microbial ATP were examined in sediments from Spartina alterniflora communities. Anaerobically homogenized sediments were amended with 1,000 ppm (ratio of weight of metal to dry weight of sediment) of various metals. Time courses in controls were similar for CH(4), H(2)S, and CO(2), with short initial lags (0 to 4 h) followed by periods of constant gas production (1 to 2 days) and declining rates thereafter. Comparisons were made between control and experimental assays with respect to initial rates of production (after lag) and overall production. Methane evolution was inhibited both initially and overall by CH(3)HgCl, HgS, and NaAsO(2). A period of initial inhibition was followed by a period of overall stimulation with Hg, Pb, Ni, Cd, and Cu, all as chlorides, and with ZnSO(4), K(2)CrO(4), and K(2)Cr(2)O(7). Production of CO(2) was generally less affected by the addition of metals. Inhibition was noted with NaAsO(2), CH(3)HgCl, and Na(2)MoO(4). Minor stimulation of CO(2) production occurred over the long term with chlorides of Hg, Pb, and Fe. Sulfate reduction was inhibited in the short term by all metals tested and over the long term by all but FeCl(2) and NiCl(2). Microbial biomass was decreased by FeCl(2), K(2)Cr(2)O(7), ZnSO(4), CdCl(2), and CuCl(2) but remained generally unaffected by PbCl(2), HgCl(2), and NiCl(2). Although the majority of metals produced an immediate inhibition of methanogenesis, for several metals this was only a transient phenomenon followed by an overall stimulation. The initial suppression of methanogenesis may be relieved by precipitation, complexation, or transformation of the metal (possibly by methylation), with the subsequent stimulation resulting from a sustained inhibition of competing organisms (e.g., sulfate-reducing bacteria). For several environmentally significant metals, severe metal pollution may substantially alter the flow of carbon in sediments.
本研究考察了几种金属对互花米草群落沉积物中微生物甲烷、二氧化碳和硫化物产生以及微生物三磷酸腺苷(ATP)的影响。将厌氧均化的沉积物用 1000ppm(金属重量与沉积物干重的比值)的各种金属进行处理。在对照中,CH(4)、H(2)S 和 CO(2) 的时间过程相似,初始短滞后(0 至 4 小时),随后是恒定的气体产生期(1 至 2 天),此后产率下降。对控制组和实验组的初始产率(滞后后)和整体产率进行了比较。CH(3)HgCl、HgS 和 NaAsO(2) 均初始和总体上抑制了甲烷的产生。汞、铅、镍、镉和铜的氯化物以及 ZnSO(4)、K(2)CrO(4) 和 K(2)Cr(2)O(7),最初有一段抑制期,随后是整体刺激期。CO(2)的产生总体上受金属添加的影响较小。NaAsO(2)、CH(3)HgCl 和 Na(2)MoO(4) 均有抑制作用。Hg、Pb 和 Fe 的氯化物长期轻微刺激 CO(2)产生。所有测试的金属在短期内均抑制硫酸盐还原,除了 FeCl(2)和 NiCl(2)外,长期内也抑制硫酸盐还原。微生物生物量受 FeCl(2)、K(2)Cr(2)O(7)、ZnSO(4)、CdCl(2)和 CuCl(2)的抑制,但基本不受 PbCl(2)、HgCl(2)和 NiCl(2)的影响。尽管大多数金属会立即抑制产甲烷作用,但对于几种金属,这种抑制只是一个短暂的现象,随后是整体刺激。产甲烷作用的初始抑制可能通过金属的沉淀、络合或转化(可能通过甲基化)得到缓解,随后的刺激是由于对竞争生物(如硫酸盐还原菌)的持续抑制所致。对于几种具有重要环境意义的金属,严重的金属污染可能会大大改变沉积物中碳的流动。