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首页> 外文期刊>Global change biology >Interactive biotic and abiotic regulators of soil carbon cycling: evidence from controlled climate experiments on peatland and boreal soils
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Interactive biotic and abiotic regulators of soil carbon cycling: evidence from controlled climate experiments on peatland and boreal soils

机译:土壤碳循环的生物和非生物相互作用调节剂:泥炭地和北方土壤的受控气候实验的证据

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Partially decomposed plant and animal remains have been accumulating in organic soils (i.e. >40% C content) for millennia, making them the largest terrestrial carbon store. There is growing concern that, in a warming world, soil biotic processing will accelerate and release greenhouse gases that further exacerbate climate change. However, the magnitude of this response remains uncertain as the constraints are abiotic, biotic and interactive. Here, we examined the influence of resource quality and biological activity on the temperature sensitivity of soil respiration under different soil moisture regimes. Organic soils were sampled from 13 boreal and peatland ecosystems located in the United Kingdom, Ireland, Spain, Finland and Sweden, representing a natural resource quality range of C, N and P. They were incubated at four temperatures (4, 10, 15 and 20 degrees C) at either 60% or 100% water holding capacity (WHC). Our results showed that chemical and biological properties play an important role in determining soil respiration responses to temperature and moisture changes. High soil C : P and C : N ratios were symptomatic of slow C turnover and long-term C accumulation. In boreal soils, low bacterial to fungal ratios were related to greater temperature sensitivity of respiration, which was amplified in drier conditions. This contrasted with peatland soils which were dominated by bacterial communities and enchytraeid grazing, resulting in a more rapid C turnover under warmer and wetter conditions. The unexpected acceleration of C mineralization under high moisture contents was possibly linked to the primarily role of fermented organic matter, instead of oxygen, in mediating microbial decomposition. We conclude that to improve C model simulations of soil respiration, a better resolution of the interactions occurring between climate, resource quality and the decomposer community will be required.
机译:几千年来,部分分解的动植物残留物积聚在有机土壤中(即碳含量> 40%),使其成为最大的陆地碳库。人们越来越担心,在变暖的世界中,土壤生物处理将加速并释放温室气体,从而进一步加剧气候变化。但是,由于限制因素是非生物的,生物的和相互作用的,因此这种反应的程度仍然不确定。在这里,我们研究了资源质量和生物活性对不同土壤水分制度下土壤呼吸温度敏感性的影响。从位于英国,爱尔兰,西班牙,芬兰和瑞典的13个寒带和泥炭地生态系统中采样了有机土壤,代表了自然资源质量范围C,N和P。将它们在四个温度下分别温育(4、10、15和15)。持水量(WHC)为60%或100%时为20摄氏度)。我们的结果表明,化学和生物学特性在确定土壤呼吸对温度和湿度变化的响应中起着重要作用。较高的土壤C:P和C:N比代表缓慢的C周转和长期的C积累。在北方土壤中,细菌与真菌的比例低与呼吸的温度敏感性更高有关,而在干燥的条件下这种敏感性会增强。与之相反的是,泥炭地土壤以细菌群落和囊虫放牧为主导,在温暖和潮湿的条件下导致更快速的碳更新。高水分含量下碳矿化的意外加速可能与发酵的有机物而不是氧气在介导微生物分解中的主要作用有关。我们得出结论,为改善土壤呼吸的C模型模拟,将需要更好地解决气候,资源质量与分解者群落之间相互作用的问题。

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