Photochemical effects on the interaction of enzymes and dissolved organic matter in natural waters

被引:26
作者
Scully, NM
Tranvik, LJ
Cooper, WJ
机构
[1] Uppsala Univ, Evolutionary Biol Ctr, Dept Limnol, SE-75236 Uppsala, Sweden
[2] Ctr Marine Sci, Dept Chem, Wilmington, NC 28409 USA
关键词
D O I
10.4319/lo.2003.48.5.1818
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Extracellular enzymes such as phosphatase (Pase) and glucosidase (Gase) can be inactivated in natural waters through photochemical processes. In this study, we examined the mechanisms involved in enzyme inactivation. We first explored the possibility of direct photoinactivation. The quantum yield spectrum (Phi(lambda)) for the direct photoinactivation of Pase increased exponentially with decreasing wavelength, with a much steeper slope relative to other Phi(lambda). This, combined with modeled half-life values for direct photoinactivation in excess of 5 d, indicates that direct photoinactivation of Pase by natural sunlight in lakes is negligible. Nonetheless, photoinactivation of enzymes occurred rapidly in light-exposed natural waters and suggested an indirect mechanism. The pH of natural waters greatly affected photoinactivation. In acid humic lake water exposed to ultraviolet radiation, the half-lives of both Pase and Gase were 4 h. The half-life of these enzymes under the same conditions were twofold higher for lake waters obtained from a limed humic lake (8 h). The higher rate of inactivation in acid water was likely caused by a pH-mediated increase in Fe photoreduction and enzyme binding. Solutions of Pase with Fe(II) and H2O2 resulted in rapid inactivation (half-life 7 min at 8.9 mumol L-1 Fe). There was no significant inactivation of controls without H2O2, indicating that enzymes are inactivated through Fe(III)/enzyme binding, which is enabled through the oxidation of Fe(II) by H2O2 to Fe(III). Direct inactivation by reactive oxygen species (ROS) was ruled out by tests with ROS scavengers.
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页码:1818 / 1824
页数:7
相关论文
共 33 条
[1]   Photochemical transformations of surface and deep marine dissolved organic matter: Effects on bacterial growth [J].
Benner, R ;
Biddanda, B .
LIMNOLOGY AND OCEANOGRAPHY, 1998, 43 (06) :1373-1378
[2]   Photochemically produced carboxylic acids as substrates for freshwater bacterioplankton [J].
Bertilsson, S ;
Tranvik, LJ .
LIMNOLOGY AND OCEANOGRAPHY, 1998, 43 (05) :885-895
[3]   Photochemical transformation of dissolved organic matter in lakes [J].
Bertilsson, S ;
Tranvik, LJ .
LIMNOLOGY AND OCEANOGRAPHY, 2000, 45 (04) :753-762
[4]   Inhibition of phosphatase activity by dissolved humic substances and hydrolytic reactivation by natural ultraviolet light [J].
Boavida, MJ ;
Wetzel, RG .
FRESHWATER BIOLOGY, 1998, 40 (02) :285-293
[5]   Spatial characterization of water quality in Florida Bay and Whitewater Bay by multivariate analyses: Zones of similar influence [J].
Boyer, JN ;
Fourqurean, JW ;
Jones, RD .
ESTUARIES, 1997, 20 (04) :743-758
[6]   Photochemical release of biologically available nitrogen from aquatic dissolved organic matter [J].
Bushaw, KL ;
Zepp, RG ;
Tarr, MA ;
SchulzJander, D ;
Bourbonniere, RA ;
Hodson, RE ;
Miller, WL ;
Bronk, DA ;
Moran, MA .
NATURE, 1996, 381 (6581) :404-407
[7]  
COOPER WJ, 1994, ADV CHEM SER, V237, P391
[8]   Complexation, stabilization, and UV photolysis of extracellular and surface-bound glucosidase and alkaline phosphatase: Implications for biofilm microbiota [J].
Espeland, EM ;
Wetzel, RG .
MICROBIAL ECOLOGY, 2001, 42 (04) :572-585
[9]  
Findlay S.E., 2003, Aquatic Ecosystems: Interactivity of Dissolved Organic Matter, DOI 10.1016/B978-012256371-3/50016-0
[10]   UV-SENSITIVE COMPLEX PHOSPHORUS - ASSOCIATION WITH DISSOLVED HUMIC MATERIAL AND IRON IN A BOG LAKE [J].
FRANCKO, DA ;
HEATH, RT .
LIMNOLOGY AND OCEANOGRAPHY, 1982, 27 (03) :564-569