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Microbial Assimilation of Atmospheric C0_2 to Synthesize Organic Matter in Soils

机译:大气CO_2的微生物同化在土壤中合成有机物

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There are no reports on the activity and quantitative capacity of microbial atmospheric carbon dioxide (CO2) assimilation in terrestrial ecosystems, although such CO2 assimilative microorganisms are numerous and widespread. Both non-phototrophic and phototrophic microbial CO2 assimilations were investigated in two sets of microcosms of eight selected soils in a closed, continuously carbon-14 (14C)-labelled CO2 atmosphere chamber. A significant amount of 14C-labelled CO2 was incorporated into the microbial biomass, accounting for between 0.12 percent and 0.59 percent of the soil organic carbon (average 37.8 ± 19.4 mg/kg after 80 d, CV = 51.3 percent, n = 8) in the set exposed to artificial light (about 500 mmol-photons-m"2-s_1 parabolic aluminized reflector light [PAR]), whereas none was detected in the set in the dark condition. Hence, soil phototrophic CO2 assimilation represents a significant part of microbial activity which cannot be ignored since it is estimated to have an annual organic C assimilative capacity of 4.9-37.5 g-C/m.
机译:上有活性的和陆地生态系统微生物大气中的二氧化碳(CO2)同化的定量能力的报道,尽管这样的CO 2同化微生物是许多和广泛。两个非光养和光养微生物CO2同化是在两组8个选择的土壤的缩影的在一个封闭的,连续的碳-14(14 C)标记的CO 2的大气室研究。 14C标记的CO 2的显著量被并入所述微生物生物质,占0.12%,而土壤有机碳的0.59%之间(平均37.8±19.4毫克/公斤后80 d,CV = 51.3%,N = 8)在所述一组暴露于人造光(约500毫摩尔光子-M“2-S_1抛物面镀铝反射灯[PAR]),而在黑暗条件下的组中没有检测到,因此,土壤光养CO2同化表示的显著部分微生物活性,因为它估计有4.9-37.5 GC / m的年度有机碳同化能力,其不能被忽略。

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