Department of Ecology and Evolutionary Biology, University of California, Irvine, CA, USA.
Department of Earth System Science, University of California, Irvine, CA, USA.
Glob Chang Biol. 2018 Jul;24(7):2884-2897. doi: 10.1111/gcb.14045. Epub 2018 Feb 6.
The magnitude and direction of carbon cycle feedbacks under climate warming remain uncertain due to insufficient knowledge about the temperature sensitivities of soil microbial processes. Enzymatic rates could increase at higher temperatures, but this response could change over time if soil microbes adapt to warming. We used the Arrhenius relationship, biochemical transition state theory, and thermal physiology theory to predict the responses of extracellular enzyme V and K to temperature. Based on these concepts, we hypothesized that V and K would correlate positively with each other and show positive temperature sensitivities. For enzymes from warmer environments, we expected to find lower V , K , and K temperature sensitivity but higher V temperature sensitivity. We tested these hypotheses with isolates of the filamentous fungus Neurospora discreta collected from around the globe and with decomposing leaf litter from a warming experiment in Alaskan boreal forest. For Neurospora extracellular enzymes, V Q ranged from 1.48 to 2.25, and K Q ranged from 0.71 to 2.80. In agreement with theory, V and K were positively correlated for some enzymes, and V declined under experimental warming in Alaskan litter. However, the temperature sensitivities of V and K did not vary as expected with warming. We also found no relationship between temperature sensitivity of V or K and mean annual temperature of the isolation site for Neurospora strains. Declining V in the Alaskan warming treatment implies a short-term negative feedback to climate change, but the Neurospora results suggest that climate-driven changes in plant inputs and soil properties are important controls on enzyme kinetics in the long term. Our empirical data on enzyme V , K , and temperature sensitivities should be useful for parameterizing existing biogeochemical models, but they reveal a need to develop new theory on thermal adaptation mechanisms.
由于对土壤微生物过程的温度敏感性了解不足,气候变暖下碳循环反馈的幅度和方向仍不确定。在较高的温度下,酶的反应速率可能会增加,但如果土壤微生物适应了变暖,这种反应可能会随着时间的推移而改变。我们使用 Arrhenius 关系、生化过渡态理论和热生理理论来预测胞外酶 V 和 K 对温度的响应。基于这些概念,我们假设 V 和 K 之间会呈正相关,并表现出正的温度敏感性。对于来自温暖环境的酶,我们预计会发现 V 、 K 和 K 温度敏感性较低,但 V 温度敏感性较高。我们使用从全球各地收集的丝状真菌 Neurospora discreta 的分离物以及阿拉斯加北方森林变暖实验中的分解叶凋落物来检验这些假设。对于 Neurospora 的胞外酶,V Q 的范围从 1.48 到 2.25,K Q 的范围从 0.71 到 2.80。与理论一致,对于一些酶,V 和 K 呈正相关,并且在阿拉斯加凋落物的实验变暖下 V 下降。然而,V 和 K 的温度敏感性并没有像预期的那样随变暖而变化。我们还没有发现 Neurospora 菌株的 V 或 K 的温度敏感性与分离地点的年平均温度之间存在关系。在阿拉斯加变暖处理中 V 的下降意味着对气候变化的短期负反馈,但 Neurospora 的结果表明,植物输入和土壤特性的气候变化是长期控制酶动力学的重要因素。我们关于酶 V 、 K 和温度敏感性的经验数据对于参数化现有的生物地球化学模型应该是有用的,但它们表明需要开发关于热适应机制的新理论。