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Phosphorus limitation in a Ferralsol: Impact on microbial activity and cell internal P pools

机译:Ferralsol中的磷限制:对微生物活性和细胞内部P池的影响

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Soil microorganisms are key regulators of the biogeochemical phosphorus (P) cycle. Microbial P limitation in highly weathered tropical soils has been reported, but whether it affects the cellular P content of indigenous soil microorganisms and its biochemical composition is unknown. We investigated the effect of microbial P limitation by measuring respiration, microbial growth, community composition and P content of microbial cells in a Ferralsol with low amounts of available P as affected by amendments with C substrates with ample nitrogen (CN) with and without extra phosphate (P). Microbial biomass and community composition were quantified by phospholipid fatty acid (PLFA) analyses. Cellular P content and P pools (PLFA, DNA and RNA per cell) were determined after extraction of microbial cells from soil by density gradient centrifugation. The apparent microbial growth rate during exponential increase in respiration rates in response to CNP addition was 0.072 h1, compared to 0.017 h1 for the CN amendment (no extra P added). This suggests that the microbial growth after a combined C and N addition was retarded by P limitation in the native soil (without added P). The net increase in microbial biomass, however, reached similar levels for both the CN and CNP treatment (measured at the point in time when respiration rates peaked). This outcome was unexpected since maximum respiration rates were about three times higher in the CNP compared to the CN treatment. Total P in extracted cells ranged from 2.1 to 8.9 fg P cell1 (microscopic counts), with a tendency for lower values for treatments without C amendments. Only 1025% of the measured total P in extracted cells was accounted for by the measured RNA, DNA and PLFA. This low percentage could partly be due to underestimation of the RNA pool (degradation during extraction). PLFA analyses showed that substrate induced growth, regardless of P addition, led to a change in microbial community composition and was dominated by fungi. The extraction of microbial cells from soil by density gradient centrifugation, however, discriminates against fungi. Accordingly, the extracted cells were not fully representative for the entire soil microbiota regarding the community composition and metabolic state. Nevertheless, for the first time microbial cell P content and P pools are reported for microorganisms that actually grew in soil and not in chemostat or batch cultures.
机译:土壤微生物是生物地球化学磷(P)循环的关键调节剂。已经报道了在高度风化的热带土壤中对微生物磷的限制,但是它是否影响土著土壤微生物的细胞磷含量及其生化组成尚不清楚。我们通过测量在有效磷含量低的Ferralsol中受受含氮和不含磷的C底物修正的影响,通过测量呼吸,微生物生长,群落组成和微生物细胞中P的含量来研究微生物P限制的影响。 (P)。通过磷脂脂肪酸(PLFA)分析定量微生物的生物量和群落组成。通过密度梯度离心从土壤中提取微生物细胞后,测定细胞中的P含量和P池(每个细胞的PLFA,DNA和RNA)。响应于CNP添加,呼吸速率呈指数增加期间的表观微生物生长速率为0.072 h1,相比之下,CN改良剂的微生物生长速率为0.017 h1(不添加额外的P)。这表明在天然土壤(不添加磷)中,磷和磷限制了碳和氮的混合添加,从而阻碍了微生物的生长。但是,对于CN和CNP处理,微生物生物量的净增加量达到了相似的水平(在呼吸频率达到峰值时测得)。这一结果是出乎意料的,因为与CN治疗相比,CNP的最大呼吸速率大约高三倍。提取细胞中的总P在2.1至8.9 fg P cell1(微观计数)的范围内,未经C修正的处理趋向于降低值。提取的细胞中只有1025%的总P被测定为RNA,DNA和PLFA。较低的百分比可能部分是由于RNA库的估计不足(提取过程中的降解)。 PLFA分析表明,无论添加P如何,底物诱导的生长均会导致微生物群落组成发生变化,并以真菌为主导。然而,通过密度梯度离心从土壤中提取微生物细胞对真菌是有区别的。因此,就群落组成和代谢状态而言,提取的细胞不能完全代表整个土壤微生物群。然而,首次报道了实际上在土壤中而不是在恒化器或分批培养中生长的微生物的微生物细胞P含量和P池。

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