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Tropical peat swamp soils: The impact of agricultural and restoration practices on activity and diversity of the soil microbial community

机译:热带泥炭沼泽土壤:农业和恢复实践对土壤微生物群落活动和多样性的影响

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摘要

Although occupying just 3-4% of the world’s landmass covering temperate, boreal and tropical areas, peatlands play an important role in conserving biodiversity and as a carbon sink. Current intensification of agricultural activities, especially in tropical areas, has led to increased use of tropical peatlands such as those in Indonesia. There is currently only limited information on the impact of this conversion. This project aimed to examine the effect of agricultural and restoration practices on the physico-chemical characteristics together with the activity and diversity of the microbial community present in tropical peat swamp soils. In addition, the impact of peat swamp restoration on microbial communities was also evaluated in an effort to monitor the success of the restoration process. To achieve this, analyses of physical, chemical and biological characteristics coupled with molecular biological analyses of peat swamp soils exposed to different human practices was carried out within the Giam Siak Kecil – Bukit Batu (GSKBB) Biosphere Reserve, Riau – Indonesia. The first component of this study examined the impact of oil palm (burning and without burning) and rubber plantations (5-10 and &40 years old) on both the biotic and abiotic properties of the peatland soil through comparisons with soil from a natural forest. Based on analysis of the physico-chemical properties, soils from plantations demonstrated increased decomposition rates, as shown by a reduction in soil organic matter (4-18%), an increase in bulk density (ρb) (0.08 – 0.17 g cm-3) and an increase in bacterial biomass (0.6 – 5.9 fold) compared with natural forest peat soils. Moreover, drier conditions due to plantation management in peat swamp soil were found, with deeper water tables (45 – 67 cm) and reduced soil water holding capacities (22-53% reduction). However, community level physiological profiling (CLPP) showed impaired microbial community function only in soils from oil palm plantations. Oil palm plantation soil (without burning) showed the lowest microbial activities (50% decrease) and the lowest Shannon diversity values (2.90) compared to natural forest soils. In contrast, soil from young rubber plantations exhibited increased microbial activities (54%) and similar Shannon diversity values (3.13) compared to natural forest soils. The second part of this study involved further assessment of the impact of oil palm and rubber plantations on tropical peatland soils using a polyphasic approach involving biochemical and molecular microbial assays. The concentration of ammonium, nitrate and phosphate observed in agricultural soils indicated a substantial increase compared with natural forest. These changes were accompanied by changes in the soil enzyme activity; reduced activities of β-glucosidase, cellobiohydrolase and acid phosphatase activities (50–55% reduction) were detected in agricultural soils while increased chitinase activity was detected in the rubber plantation soil (37% increase). In terms of soil microbial community diversity, PCR-Denaturing Gradient Gel Electrophoresis (DGGE) based analysis showed that the soil bacterial community from agricultural soils exhibited the lowest similarity amongst the different microbial groups (bacteria, fungi and archaea) evaluated, showing only 34% similarity to the natural forest soil. The Shannon diversity index values further confirmed that the conversion of tropical peatland natural forest to agriculture resulted in the greatest impact on microbial diversity being significantly different compared with the natural forest. Overall, this study indicated substantial shifts in soil microbial activity and diversity occured upon conversion of natural peatland forest to agricultural areas. The final stage of the study investigated the restoration process of burnt oil palm plantation through revegetation with native peat swamp forest plants and land rewetting through assessment of the activity and diversity of the soil microbial community together with soil chemical and physical characterisation. Overall, the physical-chemical characteristics of the restoration soils remained similar to the soil from the burnt oil palm plantation with increased depth of water table (5-6 times deeper), reduced water holding capacity (23-35%), increased bulk density (ρb) (0.31–.32 g cm-3), an increase the C:N ratio (41:1) and higher ammonium and nitrate concentrations (4-17 times higher) when compared to the forest soil (p&0.05). Restoration, involving revegetation and land rewetting resulted in a significant decrease in the phosphate concentration of the restoration soils (4.722 mg kg-1) (p&0.05) compared with other soil samples. In terms of microbial diversity, PCR-DGGE revealed that the bacterial community of the restoration soil changed significantly (only 10% similarity), amongst the different microbial groups (fungal and archaeal communities). Principal Component Analyses (PCA) showed all three soil samples clustered individually with different dependent parameters. Overall, after 3.5 years of restoration, the degraded burnt oil palm plantation soils did not appear to be similar to the peat swamp natural forest soil. Overall, this thesis contributes to our understanding of the impact of agricultural practices, especially oil palm and rubber plantations, on the microbial activity and diversity in tropical peat swamp soil. In addition, soil microbial ecology was found to be a useful indicator for use in the monitoring of the restoration process. Periodic analyses of soils under restoration using molecular microbial techniques are suggested as a useful tool for monitoring the success of the restoration process.
机译:尽管泥炭地仅占全球温带,寒带和热带地区的3-4%,但泥炭地在保护生物多样性和作为碳汇方面发挥着重要作用。当前农业活动的加剧,特别是在热带地区,导致诸如印度尼西亚的热带泥炭地的使用增加。当前,关于此转换的影响的信息很少。该项目旨在研究农业和恢复实践对理化特性的影响,以及热带泥炭沼泽土壤中存在的微生物群落的活性和多样性。此外,还评估了泥炭沼泽恢复对微生物群落的影响,以监测恢复过程的成功。为了实现这一目标,在Giam Siak Kecil&ndash中对泥炭沼泽土壤的物理,化学和生物学特性进行了分析,并对暴露于不同人类实践的泥炭沼泽土壤进行了分子生物学分析。廖内的武吉巴都(GSKBB)生物圈保护区&ndash;印度尼西亚。这项研究的第一部分通过与天然土壤进行比较,研究了油棕(燃烧和不燃烧)和橡胶园(5-10岁和40岁以上)对泥炭地土壤生物和非生物特性的影响。森林。根据理化性质的分析,人工林的土壤分解速度加快,如土壤有机质减少(4-18%),堆积密度增加(ρ)(0.08-0.17 g)所示。与天然森林泥炭土相比,细菌生物量增加了(cm-3)和0.6(5.9倍)。此外,在泥炭沼泽土壤中发现了因人工林管理而导致的干燥条件,地下水位较深(45至67厘米),土壤持水量降低(降低了22-53%)。但是,社区水平的生理学分析(CLPP)仅在油棕人工林的土壤中显示了微生物群落功能受损。与天然森林土壤相比,油棕人工林土壤(未燃烧)显示出最低的微生物活性(下降了50%)和最低的香农多样性值(2.90)。相反,与天然森林土壤相比,来自年轻橡胶种植园的土壤表现出增加的微生物活性(54%)和相似的香农多样性值(3.13)。本研究的第二部分涉及使用生物化学和分子微生物分析的多相方法,进一步评估油棕和橡胶园对热带泥炭地土壤的影响。与天然林相比,在农业土壤中观察到的铵,硝酸盐和磷酸盐浓度显着增加。这些变化伴随着土壤酶活性的变化。在农业土壤中检测到β-葡糖苷酶,纤维二糖水解酶和酸性磷酸酶活性降低(降低50-55%),而在橡胶种植土壤中检测到几丁质酶活性增加(增加37%)。在土壤微生物群落多样性方面,基于PCR-变性梯度凝胶电泳(DGGE)的分析表明,在所评价的不同微生物组(细菌,真菌和古细菌)中,农业土壤的土壤细菌群落表现出最低的相似性,仅显示34%与天然森林土壤相似。 Shannon多样性指数值进一步证实,热带泥炭地天然林向农业的转化对微生物多样性的最大影响与天然林相比有显着差异。总体而言,这项研究表明,在自然泥炭地森林向农业地区转化后,土壤微生物活性和多样性发生了重大变化。研究的最后阶段通过对原生泥炭沼泽森林植物进行植被恢复来研究烧过的油棕人工林的恢复过程,并通过评估土壤微生物群落的活性和多样性以及土壤化学和物理特性来对土地进行湿润。总体而言,恢复的土壤的物理化学特征与烧过的油棕种植园的土壤相似,但地下水位增加(深5-6倍),持水量降低(23-35%),堆积密度增加(ρb)(0.31-0.32 g cm-3),与森林土壤相比,C:N比增加(41:1),铵盐和硝酸盐浓度更高(高4-17倍)(p < ; 0.05)。与其他土壤样品相比,涉及植被恢复和土地湿润的恢复导致恢复土壤的磷酸盐浓度(4.722 mg kg-1)显着降低(p <0.05)。在微生物多样性方面,PCR-DGGE表明,恢复土壤的细菌群落发生了显着变化(相似度仅为10%),在不同的微生物组(真菌和古细菌群落)中。主成分分析(PCA)显示,所有三个土壤样品分别以不同的相关参数进行聚类。总体而言,经过3.5年的恢复,退化的烧焦油棕种植园土壤似乎与泥炭沼泽天然森林土壤相似。总体而言,本论文有助于我们了解农业实践(尤其是油棕和橡胶种植园)对热带泥炭沼泽土壤微生物活性和多样性的影响。此外,发现土壤微生物生态学是监测恢复过程的有用指标。建议使用分子微生物技术对土壤进行定期分析,以监测恢复过程的成功。

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    Nurulita Y;

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