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Responses of Phenol Oxidase Activity to Water Level Changes in Peatlands: Implications for Global Carbon Cycling

机译:酚醛氧化酶活性对水平变化的蛋白质的反应:全球碳循环的影响

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Phenol oxidase is expected to play a “latch” role in the responses of carbon cycling in peatlands to global climate change. The effects of water level changes on phenol oxidase activity and phenolic substances were examined in two typical peatlands, bog and swamp, located in Hsiao Hsinganling, Heilongjiang province, north China. The results indicted the ratio of measured phenol oxidase activity to phenolics concentration is an effective index mark illustrating the impacts of water level changes on phenol oxidase involved carbon cycling processes. The responses of phenol oxidase activities to water level changes are subject to not only oxygen restrictions but also acidification/drought stress. For swamp, biogeochemical processes at upmost surface (0-10 cm) act as a pivotal role in responses of carbon cycling to water level changes. Nevertheless, biogeochemical responses in deeper bog peat (10-18 cm) to water level depression can not be neglected in assessing the impacts of moisture condition changes on enzyme-involved soil organic matter decomposition.
机译:预计酚氧化酶将在泥炭地对全球气候变化的碳循环的响应中发挥“闩锁”作用。在两种典型的泥炭地,沼泽和沼泽地区,在黑龙江省,黑龙江省北京,普罗隆江苏省,水位对酚氧化酶活性和酚类物质的影响。结果表明测得的酚氧化酶活性与酚素浓度的比例是有效指标标记,其示出了水位变化对苯酚氧化酶涉及碳循环过程的影响。酚氧化酶活性与水位变化的反应不仅受到氧气限制,还受氧气限制,而且是酸化/干旱胁迫。对于沼泽,在最上面表面(0-10cm)的生物地球化学过程充当碳循环到水位变化的致态作用。然而,在评估酶促性能变化对酶的土壤有机质分解的影响时,不能忽视进入水平抑制的生物地球化学反应在水平抑制中不能忽视。

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