Colloidal andDissolved Organic Matter Excreted byaMixotrophic Flagellate during Bacterivory andAutotrophy
Colloidal andDissolved Organic Matter Excreted byaMixotrophic Flagellate during Bacterivory andAutotrophy
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混合营养鞭毛虫在食菌和自养过程中排出的胶体和溶解有机物
DOI:
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发表时间:
1994
期刊:
影响因子:
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通讯作者:
L. Tranvik
中科院分区:
文献类型:
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作者:
L. Tranvik
Excretion ofdissolved andcolloidal organic carbon byamixotrophic flagellate, thechrysophyte Poterioochromonas malhamensis, wasstudied. Flagellates wereincubated either with14C-labeled bacteria orwith inorganic 14C, inordertocompare organic exudates originating fromprimary production withexudates originating fromingested bacteria. Colloids of>0.02pumconstituted a larger fraction oftheexudates originating fromingested bacteria, compared withexudates derived fromprimary production. Flagellate feeding onbacteria specifically labeled indifferent cell components wascompared. Cellwallcomponents gave risetolesscolloidal organic carbon thandidothercell constituents. Toinvestigate thedegradability of flagellate '4C-exudates, they wereaddedtolakewaterandmineralization to'4Co2wasmonitored. Bacterially derived exudates weremorerecalcitrant thanexudates originating fromphotosynthesis. Theresults support thehypothesis thatbacterial utilization oflabile organic compounds, followed byflagellate bacterivory and exudation, results inatransformation oflabile organic matter intomorerecalcitrant forms. Mostoftheorganic matter inpelagic environments generally exists inthedissolved form. Thus, processes involved inthe dynamics ofdissolved organic matter(DOM;operationally defined asorganic matterthatpasses theporesoffilters, usually of0.2-to0.7-,um poresize[1]) arecrucial toour