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Nitrogen fixation and diurnal changes of photosynthetic activity in Arctic soil crusts at different development stage

机译:不同发展阶段北极土壳光合活性的氮素固定与昼夜变化

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Nitrogen fixation and photosynthesis provided by microbial phototrophs (cyanobacteria and eukaryotic microalgae) are important processes occurring in Arctic soil crusts. Here, we describe and compare these processes in biological soil crusts from Central Svalbard at different stages of development. The gradient from poorly-developed to well-developed soil crusts was accompanied by the changes in biovolume of microbial phototrophs, nitrogenase and photosynthetic activity. The lowest biovolume of microbial phototrophs was detected in poorly-developed soil crusts as a consequence of the initial stage of soil colonization. The biovolume initially increased during the soil crust development but decreased in well developed lichenized soil crusts. However, nitrogenase activity decreased from poorly to more developed soil crusts. Diurnal courses of photosynthetic activity differed among the soil crust types showing shifts in diurnal minima and maxima; the poorly-developed soil crust reacted faster to changes in temperature and PAR. In spite of different microclimatic conditions during the measurements, temperature was the main factor influencing photosynthetic activity while the effect of PAR was not significant. Higher temperatures led to inhibition of photosynthetic activity and increased energy dissipation, indicating acclimation/adaptation of the soil crust photosynthetic microorganisms to a cold environment. (C) 2017 Elsevier Masson SAS. All rights reserved.
机译:微生物光学术(蓝藻和真核微藻)提供的氮固定和光合作用是北极土壳中发生的重要过程。在这里,我们描述了在不同发展阶段的中央斯瓦尔巴特的生物土壳中的这些过程。从发达良好的土壤外壳的梯度伴随着微生物光学术,氮酶和光合活性的生物弱的变化。由于土壤殖民化的初始阶段,在较为显着的土壳中检测到最低的微生物光学疗法。在土壤地壳开发期间,生物玉米最初增加,但发达的后期土壤结壳良好地减少。然而,氮酶活性从更差到更突出的土壤地壳下降。昼夜光合作用的景观不同的土壤地壳类型在昼夜最小值和最大值的变化中不同;较为良好的土壤地壳会使温度变化更快,并降低。尽管测量过程中的微跨度条件不同,但温度是影响光合作用的主要因素,而PAR的效果并不重要。较高的温度导致抑制光合活动和增加的能量耗散,表明土壤地壳光合微生物对冷环境的适应/适应。 (c)2017年Elsevier Masson SAS。版权所有。

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