Orwin Kate H, Wardle David A, Greenfield Laurence G
School of Biological Sciences, University of Canterbury, P.O. Box 4800, New Zealand.
Ecology. 2006 Mar;87(3):580-93. doi: 10.1890/05-0383.
Plants return a wide range of carbon (C) substrates to the soil system. The decomposition rate of these substrates is determined by their chemical nature, yet few studies have examined the relative ecological role of specific substrates (i.e., substrate identity) or mixtures of substrates. Carbon substrate identity and diversity may alter soil chemistry and soil community composition, resulting in changes in belowground ecosystem functions such as decomposition and nutrient transfer, creating feedbacks that may affect plant growth and the aboveground community. A laboratory experiment was set up in which eight C substrates of varying chemical complexity were added to a base soil singly, in pairs, fours, or with all eight together every four days over a 92-day period. After 92 days these soils were analyzed for changes in chemistry, microbial community structure, and components of ecosystem functioning. The identity of the added C substrates significantly affected soil chemistry, microbial basal and substrate-induced respiration, and soil microbial community structure measured by either the catabolic response profile (CRP) technique or phospholipid fatty acid composition. These belowground changes strongly affected the ability of the soil microflora to decompose cellulose paper, probably because of differential effects of the C substrates on soil energy supplies and enzyme activities. The addition of C substrates to soils also reduced plant growth compared to the unamended control soil, but less so in soils amended with a tannin than those amended with other substrates. Carbon substrate diversity effects saturated at low diversity levels, tended to have neutral or negative effects on ecosystem functions, and depended strongly on which C substrates were added. It increased CRP compound use but had little effect on other measures of the soil microbial community. Overall, results showed that the chemical nature of C substrates added to soil, and sometimes their diversity, can affect the soil microbial community and soil chemistry, which subsequently affect other ecosystem processes such as decomposition and plant growth. The identity and diversity of substrates that plants add to soil may therefore have important consequences for both above- and belowground ecosystem functions.
植物向土壤系统归还多种碳(C)底物。这些底物的分解速率由其化学性质决定,但很少有研究考察特定底物(即底物身份)或底物混合物的相对生态作用。碳底物身份和多样性可能改变土壤化学性质和土壤群落组成,导致地下生态系统功能(如分解和养分转移)发生变化,产生可能影响植物生长和地上群落的反馈。开展了一项实验室实验,在92天的时间里,每隔四天将八种化学复杂性不同的C底物单独、成对、四种一组或八种一起添加到一种基础土壤中。92天后,分析这些土壤在化学性质、微生物群落结构和生态系统功能组成方面的变化。添加的C底物身份显著影响土壤化学性质、微生物基础呼吸和底物诱导呼吸,以及通过分解代谢反应谱(CRP)技术或磷脂脂肪酸组成测定的土壤微生物群落结构。这些地下变化强烈影响土壤微生物分解纤维素纸的能力,这可能是因为C底物对土壤能量供应和酶活性有不同影响。与未改良的对照土壤相比,向土壤中添加C底物也会降低植物生长,但用单宁酸改良的土壤比用其他底物改良的土壤影响更小。碳底物多样性效应在低多样性水平时达到饱和,往往对生态系统功能产生中性或负面影响,并且强烈依赖于添加了哪些C底物。它增加了CRP化合物的利用,但对土壤微生物群落的其他指标影响很小。总体而言,结果表明,添加到土壤中的C底物的化学性质,有时还有其多样性,可以影响土壤微生物群落和土壤化学性质,进而影响其他生态系统过程,如分解和植物生长。因此,植物添加到土壤中的底物的身份和多样性可能对地上和地下生态系统功能都产生重要影响。