在不同的分解阶段,吸收性根屑诱导升温效应的积极反应一致,但微生物机制不一致

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE
Dongmei Wu , Xiaohong Wang , Ailian Fan , Yuqi Chen , Zhijie Yang , Maokui Lyu , Xiaodong Yao , Jianfen Guo , Yusheng Yang , Guangshui Chen
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引用次数: 0

摘要

新碳(C)对土壤有机碳(SOC)分解的启动效应(PE)对全球碳循环至关重要。气候变暖会提高吸收根的产量和周转率,进而增加吸收根垃圾(ABRL)的输入。因此,亟需了解气候变暖下吸收性根系垃圾诱导的PE。我们进行了一项为期 210 天的实验,在 C4 土壤中添加秃杉的 ABRL,并分别在 19 °C 和 23 °C 下培养。我们发现,在整个培养过程中,添加 ABRL 都会引起正的 PE。在早期阶段(ES:前 30 天),可溶性 C 化合物主导了 ABRL 的分解,发现 ABRL 处理中的溶解有机 C(DOC)、微生物生物量 C(MBC)和绝对水解酶活性显著高于对照组。这些结果证明,可溶性 C 输入可刺激微生物的生长和酶活性,并通过共代谢产生正 PE。在后期阶段(LS:180 天后),结构性 C 化合物的释放主导了 ABRL 的分解,发现 ABRL 处理中的可用氮(N)显著低于对照组,特定潜在氮获取酶(Nacq)显著高于对照组。这些结果表明,在氮限制条件下,微生物利用 C 作为能量来增加 Nacq 酶,以分解 SOC 开采氮,从而诱导了正 PE。升温明显增加了两个阶段的 PEs。在 ES 阶段,升温增加了 MBC,但以 DOC 为代价,这表明升温加强了微生物的协同代谢。在 LS 阶段,气候变暖明显降低了可用氮,增加了绝对潜在氧化酶活性,这表明对富含氮的难降解 SOC 的氮限制和氧化增加,即促进了微生物的氮开采。然而,与对照组相比,我们没有观察到添加 ABRL 对 SOC 分解的温度敏感性有显著影响。这项研究提供了一个有价值的见解,即升温可持续增加 ABRL 诱导的 PE,但在分解过程中会通过不同的微生物机制进行。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Consistent positive response but inconsistent microbial mechanisms of absorptive root litter-induced priming effect to warming at different decomposition stages

Consistent positive response but inconsistent microbial mechanisms of absorptive root litter-induced priming effect to warming at different decomposition stages
The fresh carbon (C) induced priming effect (PE) on soil organic C (SOC) decomposition is critical for global C cycling. Climate warming could raise absorptive roots production and turnover, and then increase the input of absorptive roots litter (ABRL). Therefore, it is urgent to understand the PE induced by ABRL under warming. We conducted a 210-day experiment by adding ABRL of Cunninghamia lanceolata into a C4 soil and incubating them at 19 °C and 23 °C. We found that adding ABRL caused positive PE throughout the incubation. At the early stage (ES: first 30 days), labile C compounds dominated the decomposition of ABRL, significantly higher dissolved organic C (DOC), microbial biomass C (MBC), and absolute hydrolase activities were found in the ABRL treatment than in the control. These results supports that labile C inputs stimulating microbial growth, enzyme activities and cause positive PE via co-metabolic. At the later stage (LS: after 180 days), the release of structural C compounds dominated the decomposition of ABRL, a significantly lower available nitrogen (N) and a significantly higher specific potential N-acquisition (Nacq) enzymes were found in the ABRL treatment than in the control. These results suggests that microbes utilizing the C as energy to increase Nacq enzymes to decompose SOC for N mining under N limitation induced positive PE. Warming significantly increased the PEs at both stages. At the ES, warming increased the MBC at the cost of DOC, suggesting that warming intensifies the microbial co-metabolism. At the LS, warming significantly decreased the available N and increases the absolute potential oxidases activities, suggesting an increased N limitation and oxidation for N-rich recalcitrant SOC, i.e., a promoted microbial N mining. Nevertheless, we did not observe a significant effect of ABRL addition on the temperature sensitivity of SOC decomposition compared to the control. This study provides a valuable insight that warming could consistently increase the ABRL induced PE but through different microbial mechanisms along with the decomposition processing.
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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