Specific activity of cell-surface acid phosphatase in different bacterioplankton morphotypes in an acidified mountain lake
Jazyk angličtina Země Anglie, Velká Británie Médium print
Typ dokumentu časopisecké články, práce podpořená grantem
PubMed
16817935
DOI
10.1111/j.1462-2920.2006.01023.x
PII: EMI1023
Knihovny.cz E-zdroje
- MeSH
- biomasa MeSH
- fosfáty metabolismus MeSH
- fytoplankton enzymologie MeSH
- indoly MeSH
- kyselá fosfatasa metabolismus MeSH
- organofosforové sloučeniny metabolismus MeSH
- plankton enzymologie mikrobiologie MeSH
- počet mikrobiálních kolonií metody MeSH
- sladká voda mikrobiologie MeSH
- substrátová specifita MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Názvy látek
- DAPI MeSH Prohlížeč
- fosfáty MeSH
- indoly MeSH
- kyselá fosfatasa MeSH
- organofosforové sloučeniny MeSH
Activity of extracellular acid phosphatases was measured at single-cell level in bacterioplankton groups defined by their morphology and size, in acidified mountain Lake Certovo, during the 2003 season, with a method based on use of the substrate ELF97 phosphate which provides fluorescent precipitates upon hydrolysis by phosphatases. The bacterial cell-associated precipitates were quantified by image analysis. A specific, conspicuous, apparently homogeneous morphotype of curved cells of approximately 5 microm average length, despite its low total biomass (average of 4%), contributed significantly (in average by 31%) to the total bacterioplankton phosphatase activity in Lake Certovo (ranging from 1.0 to 12.7 micromol l(-1) h(-1), using ELF97 phosphate as a substrate). Bacterial filaments (> 10 microm), although comprising in average 85% of bacterioplankton biomass, contributed to the total bacterioplankton activity only by 45%. Biomass-specific activity of extracellular (cell-surface) phosphatases of the main bacterioplankton morphotypes increased in the order filaments < cocci and rods < curved cells. The biomass-specific activity of bacterioplankton extracellular phosphatases (0-300 nmol microgC(-1) h(-1)) was generally highest in the spring and decreased gradually during summer. These changes could result from seasonal changes in the phosphorus status of the lake and from subsequent regulation of enzyme expression by bacteria.
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