首页> 外文期刊>International Journal of Agriculture and Biology >Nitrification Resilience and Response of Ammonia-Oxidizing Bacteria upon Heat-Drought Extremes across Three Soil Ecosystems in Lower Himalaya
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Nitrification Resilience and Response of Ammonia-Oxidizing Bacteria upon Heat-Drought Extremes across Three Soil Ecosystems in Lower Himalaya

机译:硝化弹性和氨氧化细菌在较低的三种土壤生态系统中热水干旱极端的响应

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Soil ecosystems despite of providing a vast range of value services are expected to face climatic extremes. Assessing the resilience degree of such ecosystems is integral in evaluating their functional stability. This study investigated the resilience and resistance of potential nitrification activity (PNA) and involved guilds (ammonia-oxidizing bacteria - AOB) upon two heat-drought extremes (low (40°C for 24 h) and high (40°C for 48 h)) at 1, 7, 14, 28 days’ intervals across three different soil ecosystems (arable, grassland, forest) in lower Himalaya. Results demonstrated that three soils responded differentially to heat-droughts (~20–55% decrease PNA) with arable soil showing high resistance (withheld ~55.3% PNA) and low resilience (~82–85%). The gene abundances of AOB revealed that the community size was significantly reduced upon the heat-droughts (up to 50.1%) and could not ultimately recover showing an incomplete resilience. In contrast to arable, the grassland and forest soils were better in resilience with PNA at day 28 observed near to control (93.4 and 91.4%). The correlation analyses showed a strong positive relationship of AOB to PNA particularly in arable soil. The high resilience exhibited by grassland and forest soils implied that despite of reduction in AOB numbers, functional redundancy might have inferred an increased resilience showing that these soils can recover once the stress period is over. This work underlines the functional stability of different soils for nitrification potential highlighting the relevance of resilience and resistance perspectives in wake of predicted climatic extremes on soil N cycling and associated N losses in lower Himalaya.
机译:尽管提供了广泛的价值服务,但土壤生态系统预计将面临气候极端。评估这些生态系统的恢复程度在评估其功能稳定性方面是一体的。本研究研究了潜在的硝化活性(PNA)的抵抗力和抗性,并在两个热水干旱极端(低(40℃)和高(40℃下48小时)上(40℃,氨氧化细菌 - Aob)和涉及公会(氨氧化细菌 - Aob)的抵抗力和抗性))在较低喜马拉雅州三种不同土壤生态系统(耕地,森林)的1,7,14,28天的间隔。结果表明,三种土壤差异差异,与耕种土壤(〜20-55%降低PNA)差异,具有耕地,显示出高抗性(持续〜55.3%PNA)和低弹性(〜82-85%)。 AOB的基因丰富揭示了群落规模在热干旱(高达50.1%)上显着降低,并且不能最终恢复显示不完全的弹性。与耕地相比,草原和森林土壤在观察到的第28天的PNA恢复性较好(93.4和91.4%)。相关分析表明AOB对PNA特别是耕地的强阳性关系。草地和森林土壤展示的高弹性暗示,尽管Aob数量减少,功能冗余可能会推断出增加的弹性,表明,在应力期结束后,这些土壤可以恢复这些土壤。这项工作强调了不同土壤的功能稳定性,硝化潜力突出了恢复力和阻力观点在土壤N循环循环和较低HIMALAYA中的相关N损失中的预测气候循环唤醒的相关性。

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