Biology Department, Woods Hole Oceanographic Institution, Woods Hoie, Massachusetts 02543, and Institute of Ecology and Genetics, Aarhus University, Ny Munkegade, DK-8000 Aarhus C, Denmark.
Appl Environ Microbiol. 1986 Jul;52(1):161-8. doi: 10.1128/aem.52.1.161-168.1986.
Beggiatoa spp. grow optimally in media containing opposed gradients of oxygen and soluble sulfide, although some strains also require an organic substrate. By using microelectrodes, we characterized oxygen and sulfide gradients during their initial development in uninoculated media and in cultures of marine and freshwater strains. In gradient media, Beggiatoa strains always grew some distance below the air/agar interface as a dense "plate" of constantly gliding filaments with sharply demarcated upper and lower boundaries. Within established plates, the maximum oxygen partial pressure was 0.6 to 6.0% of air saturation and not significantly lower if filaments were fixing nitrogen. Oxygen penetrated only 100 to 300 mum into the plate, and the anoxic fraction increased from less than 10% to approximately 90% during later stages of growth. For lithoautotrophically grown marine strains, the linearity of the oxygen profile above the plate plus its drop to zero therein indicated that oxygen uptake for the entire tube occurred only within the Beggiatoa plate. Consequently, oxygen consumption could be predicted solely from the distance between the air/agar interface and the top of a plate, given the diffusion coefficient for oxygen. By contrast, for freshwater strains grown heterotrophically (with sulfide also in the medium), oxygen profiles were frequently nonlinear because of nonbiological reaction with sulfide which had diffused past the aggregated filaments. For all strains tested, microoxic aggregation also occurred in the absence of sulfide, apparently reflecting a step-up phobic response to oxygen.
硫发菌属(Beggiatoa)在含有氧气和可溶硫化物相反梯度的培养基中生长最佳,尽管有些菌株也需要有机底物。通过使用微电极,我们在未接种的培养基中和海洋和淡水菌株的培养物中描述了它们在初始发育期间的氧气和硫化物梯度。在梯度培养基中,硫发菌属菌株总是在距离空气/琼脂界面一定距离处生长,形成密集的“平板”,其中不断滑行的丝状菌具有明显的上下边界。在已建立的平板内,最大氧分压为空气饱和的 0.6%至 6.0%,如果丝状菌固定氮,则不会显著降低。氧气仅渗透到平板 100 至 300 微米深处,并且在生长后期,缺氧部分从小于 10%增加到大约 90%。对于以岩石自养方式生长的海洋菌株,平板上方的氧气分布的线性及其在其中降至零表明整个管中的氧气摄取仅发生在硫发菌属平板内。因此,只要知道氧气的扩散系数,就可以仅根据空气/琼脂界面与平板顶部之间的距离来预测氧气消耗。相比之下,对于异养生长的淡水菌株(培养基中也含有硫化物),由于与已经扩散过聚集丝状菌的硫化物发生非生物学反应,氧气分布通常是非线性的。对于所有测试的菌株,即使没有硫化物,微氧聚集也会发生,显然反映了对氧气的趋氧反应。