Bacterial Activity at −2 to −20°C in Arctic Wintertime Sea Ice

作者：Karen Junge, Hajo S. Eicken, Jody W. Deming · 发表于：Applied and Environmental Microbiology · 年份：2004 · DOI：10.1128/aem.70.1.550-557.2004 · 被引用次数：419 · 研究领域：Polar Research and Ecology、Microbial Community Ecology and Physiology、Indigenous Studies and Ecology

Arctic wintertime sea-ice cores, characterized by a temperature gradient of -2 to -20 degrees C, were investigated to better understand constraints on bacterial abundance, activity, and diversity at subzero temperatures. With the fluorescent stains 4',6'-diamidino-2-phenylindole 2HCl (DAPI) (for DNA) and 5-cyano-2,3-ditoyl tetrazolium chloride (CTC) (for O(2)-based respiration), the abundances of total, particle-associated (>3- micro m), free-living, and actively respiring bacteria were determined for ice-core samples melted at their in situ temperatures (-2 to -20 degrees C) and at the corresponding salinities of their brine inclusions (38 to 209 ppt). Fluorescence in situ hybridization was applied to determine the proportions of Bacteria, Cytophaga-Flavobacteria-Bacteroides (CFB), and Archaea. Microtome-prepared ice sections also were examined microscopically under in situ conditions to evaluate bacterial abundance (by DAPI staining) and particle associations within the brine-inclusion network of the ice. For both melted and intact ice sections, more than 50% of cells were found to be associated with particles or surfaces (sediment grains, detritus, and ice-crystal boundaries). CTC-active bacteria (0.5 to 4% of the total) and cells detectable by rRNA probes (18 to 86% of the total) were found in all ice samples, including the coldest (-20 degrees C), where virtually all active cells were particle associated. The percentage of active bacteria associated with particles increa...