Lower S K, Hochella M F, Beveridge T J
NanoGeoscience and Technology Laboratory, Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061, USA.
Science. 2001 May 18;292(5520):1360-3. doi: 10.1126/science.1059567.
Force microscopy has been used to quantitatively measure the infinitesimal forces that characterize interactions between Shewanella oneidensis (a dissimilatory metal-reducing bacterium) and goethite (alpha-FeOOH), both commonly found in Earth near-surface environments. Force measurements with subnanonewton resolution were made in real time with living cells under aerobic and anaerobic solutions as a function of the distance, in nanometers, between a cell and the mineral surface. Energy values [in attojoules (10(-18) joules)] derived from these measurements show that the affinity between S. oneidensis and goethite rapidly increases by two to five times under anaerobic conditions in which electron transfer from bacterium to mineral is expected. Specific signatures in the force curves suggest that a 150-kilodalton putative iron reductase is mobilized within the outer membrane of S. oneidensis and specifically interacts with the goethite surface to facilitate the electron transfer process.
力显微镜已被用于定量测量微小力,这些力表征了常见于地球近地表环境中的奥奈达希瓦氏菌(一种异化金属还原菌)与针铁矿(α-FeOOH)之间的相互作用。在有氧和厌氧溶液中,以纳米为单位实时测量活细胞与矿物表面之间距离的亚纳牛顿分辨率的力。从这些测量中得出的能量值[以阿托焦耳(10^(-18)焦耳)为单位]表明,在预期细菌向矿物进行电子转移的厌氧条件下,奥奈达希瓦氏菌与针铁矿之间的亲和力迅速增加两到五倍。力曲线中的特定特征表明,一种150千道尔顿的推定铁还原酶在奥奈达希瓦氏菌的外膜内被调动起来,并与针铁矿表面特异性相互作用以促进电子转移过程。