Institute of Oceanography, Hellenic Centre for Marine Research, Anavissos 19013, Attiki, Greece.
Microbes Environ. 2012;27(4):504-8. doi: 10.1264/jsme2.me12045. Epub 2012 Apr 14.
Studies in the center and margin of the Medee Basin, a Mediterranean deep-sea hypersaline anoxic basin, and at a reference site during Penelope cruise (2007), revealed the existence of a 7 m-thick halocline, with high salinity (328 psu), and high sedimentary organic carbon and biopolymer concentrations. The 194 16S rRNA sequences retrieved were grouped into 118 unique phylotypes. Pseudomonas gessardii, dominated in the center, while 33 phylotypes were detected at the margin and 73 at the reference site. The study suggested conditions hostile to bacteria in the sediments of the Medee Basin and preservation of sedimentary labile organic matter.
对地中海深海高盐缺氧盆地梅迪盆地的中心和边缘以及佩内洛普号考察(2007 年)期间的一个参考点进行的研究表明,存在一个 7 米厚的盐水层,其盐度很高(328 实用盐度单位),并且含有高浓度的沉积有机碳和生物聚合物。所获得的 194 个 16S rRNA 序列被分为 118 个独特的基因型。假单胞菌在中心占主导地位,而在边缘检测到 33 个基因型,在参考点检测到 73 个基因型。研究表明,梅迪盆地沉积物中的细菌生存条件恶劣,并且沉积的不稳定有机物质得以保存。