青藏高原高寒草地土壤酶活性海拔地带性特征
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第二次青藏高原综合科学考察研究项目(2019QZKK0307);第二次青藏高原综合科学考察研究项目(2019QZKK0405)


Altitude pattern of soil enzyme activities in alpine grasslands across the Qinghai-Tibet Plateau
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    摘要:

    土壤酶是土壤生态系统中具有催化功能的一类蛋白质,由植物根系分泌物、微生物和动植物残体释放到土壤中,参与了土壤中所有的生物化学过程,其活性的大小可以灵敏地反应土壤中生化反应的方向和强度。青藏高原因海拔高和气候寒冷,被认为是气候变化的敏感区和脆弱区。全球气候变化使土壤酶活性受到强烈的影响,这些影响可能使土壤的质量发生改变,进而对青藏高原高寒草地植被生产力产生一定影响。土壤酶在生态系统物质循环和能量流动中起着关键作用,其格局、功能和转换过程已被广泛的研究,但高寒草地生态系统土壤酶活性的海拔地带性特征还需深入探讨。因此,以青藏高原高寒草地为研究对象,将土壤酶活性海拔梯度研究从站点尺度拓展到样带尺度,分析了与土壤碳循环密切相关的土壤β-1,4-葡萄糖苷酶(βG)、与土壤氮循环密切相关的土壤N-乙酰-β氨基葡萄糖苷酶(NAG)、土壤亮氨酸肌肽酶(LAP)以及与土壤磷循环密切相关的土壤碱性磷酸酶(ALP)的海拔地带性,进一步明晰其主要驱动因子。结果表明:(1)ALP和βG活性在海拔梯度上,展现出显著分异,在约为3546 m和3364 m出现拐点,且低海拔显著高于高海拔(P<0.01)。而NAG和LAP的活性与海拔无显著关系。(2)高低海拔模式下,ALP活性均与年平均降水量显著相关(P<0.01),而不受年平均温度的影响。高海拔模式下,βG活性受降水的影响;低海拔模式下,气候影响不明显。综合而言,海拔变化引起的温度和降水变化会直接或间接地影响土壤酶活性,其中降水是影响青藏高原高寒草地土壤酶活性的关键因子之一, 这种适应性的改变使土壤酶能够在不同的环境条件下适应并发挥其功能,从而影响着土壤生态系统的物质循环和能量转化过程。研究结果可以评估不同海拔地带土壤的养分转化、有机质分解和循环等生态系统功能,为生态系统管理和保护提供科学依据,对理解高寒草地生物地球化学循环过程和机制具有重要意义。

    Abstract:

    Soil enzymes are a class of proteins with catalytic functions in the soil ecosystem. They are secreted into the soil by plant roots, microorganisms, and the decomposition of plant and animal residues, and participate in all biochemical processes in the soil, and their activity levels can sensitively reflect the direction and intensity of biochemical reactions. Due to its high altitude and cold climate, Qinghai-Tibet Plateau is regarded as a sensitive and fragile area to climate change. Global climate change significantly affects soil enzyme activities, and these impacts can potentially modify soil quality, thus affect vegetation productivity in the alpine grasslands of the Qinghai-Tibet Plateau. Soil enzymes play a critical role in the material cycle and energy flow of ecosystems. Their patterns, functions, and conversion processes have been widely studied. Nevertheless, the altitude pattern of soil enzyme activities in alpine grassland ecosystems still needs to be further explored. Therefore, we obtained soil enzymes in the alpine grasslands across the Qinghai-Tibet Plateau, and extended the study on the elevation gradient of soil enzyme activity from the site scale to the transect scale. We analyzed the altitude pattern of soil β-Glucosidase (βG) enzymes closely related to the soil C cycle, soil β-Nacetylglucosaminidase (NAG) enzymes, and soil leucine aminopeptidase (LAP) enzymes closely associated with soil N cycle, soil alkaline phosphatase (ALP) enzymes greatly related to soil P cycle, and further explored their main drivers. The results showed that:(1) the activity of ALP and βG showed significant differences along the altitude gradient, and their thresholds presented at 3546 m and 3364 m, respectively. And the enzyme activity of ALP and βG at low altitudes was significantly higher than that at high altitudes (P<0.01). However, there were no significant relationships between NAG and LAP activities and altitude. (2) The ALP activity was significantly linked to mean annual precipitation (P<0.01), but was not affected by mean annual temperature. At high altitudes, the βG activity was affected by precipitation, but the climate had no significant effect on the βG activity at low altitudes. In conclusion, the change of temperature and precipitation caused by altitude can directly or indirectly affect soil enzyme activities. Precipitation is one of the key factors governing soil enzyme activities in the alpine grassland across the Qinghai-Tibet Plateau. This adaptive change enables soil enzymes to adapt and play their functions under different environmental conditions, thus affecting the material cycle and energy conversion processes of the soil ecosystem. The results can be used to evaluate the ecosystem functions of soil nutrient transformation, organic matter decomposition and circulation at different elevations, and provide a scientific basis for ecosystem management and protection, which is of great significance for understanding the biogeochemical cycle processes and mechanisms in alpine grasslands.

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霍皇煜,米琦,周天财,李洋,张建香,陈俊合,汪亚峰,孙建.青藏高原高寒草地土壤酶活性海拔地带性特征.生态学报,2024,44(1):405~415

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