Microbial response to surface microtopography: the role of metabolism in localized mineral dissolution

被引:102
作者
Edwards, KJ
Rutenberg, AD
机构
[1] Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, McLean Lab, Woods Hole, MA 02543 USA
[2] Dalhousie Univ, Dept Phys, Halifax, NS B3H 3J5, Canada
基金
美国国家科学基金会;
关键词
bacteria; mineral surfaces; attachment; pyrite; dissolution; sulfur;
D O I
10.1016/S0009-2541(01)00303-5
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We examine the role of microtopographical surface features on sulfide minerals in localizing and aligning bacterial adhesion. Experimental data shows strong correlation between bacterial cell alignment and principal crystallographic axes of pyrite (< 100 > and < 110 >). While bacteria often adhere to visible surface imperfections such as scratches, in many cases no associated surface features are visible. Additionally, the size of the surface imperfection does not unambiguously determine its effect in localizing and aligning bacterial cells. We theoretically model bacterial adhesion. We find that the depth of a surface feature such as a scratch is less important than its cross-sectional shape. Surface features that conform to the bacterial shape can strongly alter local bacterial adhesion energies, even with heights of only 10 nm. Hence, small local surface alterations due to bacterial metabolism could strongly affect local adhesion parameters, and may account for the observed bacterial distributions on mineral surfaces. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:19 / 32
页数:14
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