Department of Plant Sciences, University of Cambridge, Cambridge, UK.
FEMS Microbiol Ecol. 2013 Jul;85(1):37-50. doi: 10.1111/1574-6941.12096. Epub 2013 Mar 20.
Tropical forests have high rates of soil carbon cycling, but little information is available on how roots, arbuscular mycorrhizal fungi (AMF), and free-living microorganisms interact and influence organic matter mineralization in these ecosystems. We used mesh ingrowth cores and isotopic tracers in phospholipid fatty acid biomarkers to investigate the effects of roots and AMF mycelia on (1) microbial community composition, microbial carbon utilization, and hydrolytic enzyme activities for large, potted tropical trees and (2) enzyme activities and litter mass loss in a lowland tropical forest. Under the tropical tree, plant-derived carbon was incorporated predominantly into bacterial groups in both rhizosphere and AMF-only soils. Gram-positive bacteria incorporated additional soil-derived carbon in rhizosphere soils, which also contained the highest microbial biomass. For hydrolytic enzymes, β-glucosidase and N-acetyl β-glucosaminidase activities were highest in rhizosphere soils, while phosphomonoesterase activity was highest in AMF-only soil. In the forest, leaf litter mass loss was increased by the presence of roots, but not by the presence of AMF mycelia only. Root-microbial interactions influenced organic matter cycling, with evidence for rhizosphere priming and accelerated leaf litter decomposition in the presence of roots. Although AMF mycelia alone did not stimulate organic matter mineralization, they were a conduit of carbon to other soil microorganisms.
热带森林具有较高的土壤碳循环速率,但关于根系、丛枝菌根真菌 (AMF) 和自由生活微生物如何相互作用并影响这些生态系统中的有机质矿化,信息有限。我们使用网内生长芯和磷脂脂肪酸生物标志物中的同位素示踪剂,研究了根系和 AMF 菌丝对(1)大型盆栽热带树木的微生物群落组成、微生物碳利用和水解酶活性,以及(2)低地热带森林中的酶活性和凋落物质量损失的影响。在热带树下,植物来源的碳主要被根际和仅 AMF 土壤中的细菌群吸收。根际土壤中的革兰氏阳性菌吸收了更多的土壤来源的碳,而根际土壤中的微生物生物量最高。对于水解酶,β-葡萄糖苷酶和 N-乙酰-β-葡萄糖胺酶活性在根际土壤中最高,而磷酸单酯酶活性在仅 AMF 土壤中最高。在森林中,根的存在增加了叶凋落物的质量损失,但 AMF 菌丝的存在则没有。根-微生物相互作用影响有机质循环,根的存在导致了根际激发和加速了叶凋落物分解。虽然 AMF 菌丝本身不能刺激有机质矿化,但它们是碳向其他土壤微生物传递的途径。