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Biotic degradation at night, abiotic degradation at day: positive feedbacks on litter decomposition in drylands

机译:夜间生物退化、白天非生物退化:旱地凋落物分解的正反馈

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The arid and semi-arid drylands of the world are increasingly recognized for their role in the terrestrial net carbon dioxide (CO2) uptake, which depends largely on plant litter decomposition and the subsequent release of CO2 back to the atmosphere. Observed decomposition rates in drylands are higher than predictions by biogeochemical models, which are traditionally based on microbial (biotic) degradation enabled by precipitation as the main mechanism of litter decomposition. Consequently, recent research in drylands has focused on abiotic mechanisms, mainly photochemical and thermal degradation, but they only partly explain litter decomposition under dry conditions, suggesting the operation of an additional mechanism. Here we show that in the absence of precipitation, absorption of dew and water vapor by litter in the field enables microbial degradation at night. By experimentally manipulating solar irradiance and nighttime air humidity, we estimated that most of the litter CO2 efflux and decay occurring in the dry season was due to nighttime microbial degradation, with considerable additional contributions from photochemical and thermal degradation during the daytime. In a complementary study, at three sites across the Mediterranean Basin, litter CO2 efflux was largely explained by litter moisture driving microbial degradation and ultraviolet radiation driving photodegradation. We further observed mutual enhancement of microbial activity and photodegradation at a daily scale. Identifying the interplay of decay mechanisms enhances our understanding of carbon turnover in drylands, which should improve the predictions of the long-term trend of global carbon sequestration.
机译:世界上干旱和半干旱干旱地区因其在陆地净二氧化碳(CO2)吸收中的作用而日益得到人们的承认,这在很大程度上取决于植物凋落物的分解和随后将CO2释放回大气中。在旱地观测到的分解速率高于生物地球化学模型的预测,生物地球化学模型传统上基于降水导致的微生物(生物)降解作为凋落物分解的主要机制。因此,最近在旱地的研究集中在非生物机制上,主要是光化学和热降解,但它们只能部分解释干旱条件下的凋落物分解,这表明还有另一种机制在起作用。在这里,我们表明,在没有降水的情况下,田间垃圾吸收露水和水蒸气使微生物在夜间降解。通过实验操纵太阳辐照度和夜间空气湿度,我们估计旱季发生的大部分凋落物CO2外排和衰变是由于夜间微生物降解造成的,白天的光化学和热降解也贡献了相当大的额外作用。在一项补充研究中,在地中海盆地的三个地点,凋落物CO2外排主要是由凋落物水分驱动微生物降解和紫外线辐射驱动光降解来解释的。我们进一步观察到微生物活性和光降解在每日尺度上的相互增强。确定衰变机制的相互作用可以增强我们对旱地碳周转的理解,这应该会改善对全球碳封存长期趋势的预测。

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