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温度对泥炭沼泽中以泥炭藓为主的 δ C 值和甲烷营养菌相关藿烷类分布的影响。

Influence of temperature on the δ C values and distribution of methanotroph-related hopanoids in Sphagnum-dominated peat bogs.

机构信息

Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, The Netherlands.

School of Civil Engineering and Geoscience, Newcastle University, Newcastle upon Tyne, UK.

出版信息

Geobiology. 2020 Jul;18(4):497-507. doi: 10.1111/gbi.12389. Epub 2020 Mar 16.

Abstract

Methane emissions from peat bogs are mitigated by methanotrophs, which live in symbiosis with peat moss (e.g. Sphagnum). Here, we investigate the influence of temperature and resultant changes in methane fluxes on Sphagnum and methanotroph-related biomarkers, evaluating their potential as proxies in ancient bogs. A pulse-chase experiment using C-labelled methane in the field clearly showed label uptake in diploptene, a biomarker for methanotrophs, demonstrating in situ methanotrophic activity in Sphagnum under natural conditions. Peat cores containing live Sphagnum were incubated at 5, 10, 15, 20 and 25°C for two months, causing differences in net methane fluxes. The natural δ C values of diploptene extracted from Sphagnum showed a strong correlation with temperature and methane production. The δ C values ranged from -34‰ at 5°C to -41‰ at 25°C. These results are best explained by enhanced expression of the methanotrophic enzymatic isotope effect at higher methane concentrations. Hence, δ C values of diploptene, or its diagenetic products, potentially provide a useful tool to assess methanotrophic activity in past environments. Increased methane fluxes towards Sphagnum did not affect δ C values of bulk Sphagnum and its specific marker, the C n-alkane. The concentration of methanotroph-specific bacteriohopanepolyols (BHPs), aminobacteriohopanetetrol (aminotetrol, characteristic for type II and to a lesser extent type I methanotrophs) and aminobacteriohopanepentol (aminopentol, a marker for type I methanotrophs) showed a non-linear response to increased methane fluxes, with relatively high abundances at 25°C compared to those at 20°C or below. Aminotetrol was more abundant than aminopentol, in contrast to similar abundances of aminotetrol and aminopentol in fresh Sphagnum. This probably indicates that type II methanotrophs became prevalent under the experimental conditions relative to type I methanotrophs. Even though BHP concentrations may not directly reflect bacterial activity, they may provide insight into the presence of different types of methanotrophs.

摘要

泥炭沼泽中的甲烷排放受到与泥炭藓(例如水藓属)共生的甲烷营养菌的缓解。在这里,我们研究了温度的影响以及甲烷通量的变化对水藓和甲烷营养菌相关生物标志物的影响,评估了它们作为古代沼泽中指标的潜力。在野外使用 C 标记的甲烷进行的脉冲追踪实验清楚地表明,双萜烯(甲烷营养菌的生物标志物)吸收了标记物,证明了在自然条件下水藓中的原位甲烷营养活性。含有活水藓的泥炭芯在 5、10、15、20 和 25°C 下孵育两个月,导致净甲烷通量的差异。从水藓中提取的双萜烯的天然 δ C 值与温度和甲烷产量呈强相关。δ C 值范围从 5°C 的-34‰到 25°C 的-41‰。这些结果最好通过在较高甲烷浓度下增强甲烷营养酶的同位素效应的表达来解释。因此,双萜烯或其成岩产物的 δ C 值可能提供了一种评估过去环境中甲烷营养活性的有用工具。向水藓增加的甲烷通量不会影响大块水藓及其特定标志物,即 C n-正烷烃的 δ C 值。甲烷营养菌特异性杆菌醇(BHP)、氨杆菌萜四醇(特征为 II 型,在较小程度上为 I 型甲烷营养菌)和氨杆菌五醇(I 型甲烷营养菌的标志物)的浓度对增加的甲烷通量呈非线性响应,与 20°C 或以下相比,25°C 时相对较高。氨杆菌萜四醇的丰度高于氨杆菌五醇,与新鲜水藓中氨杆菌萜四醇和氨杆菌五醇的丰度相似。这可能表明,与 I 型甲烷营养菌相比,在实验条件下,II 型甲烷营养菌变得更为普遍。尽管 BHP 浓度可能不会直接反映细菌活性,但它们可能提供有关不同类型的甲烷营养菌存在的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/927a/7383571/6ea7e62e94be/GBI-18-497-g001.jpg

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