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甲烷呼气的长期监测。

Long-term monitoring of breath methane.

机构信息

Institute of Earth Sciences, Heidelberg University, Im Neuenheimer Feld 236, D-69120 Heidelberg, Germany.

Institute of Earth Sciences, Heidelberg University, Im Neuenheimer Feld 236, D-69120 Heidelberg, Germany.

出版信息

Sci Total Environ. 2018 May 15;624:69-77. doi: 10.1016/j.scitotenv.2017.12.097. Epub 2017 Dec 13.

Abstract

In recent years, methane as a component of exhaled human breath has been considered as a potential bioindicator providing information on microbial activity in the intestinal tract. Several studies indicated a relationship between breath methane status and specific gastrointestinal disease. So far, almost no attention has been given to the temporal variability of breath methane production by individual persons. Thus here, for the first time, long-term monitoring was carried out measuring breath methane of three volunteers over periods between 196 and 1002days. Results were evaluated taking into consideration the health status and specific medical intervention events for each individual during the monitoring period, and included a gastroscopy procedure, a vaccination, a dietary change, and chelate therapy. As a major outcome, breath methane mixing ratios show considerable variability within a person-specific range of values. Interestingly, decreased breath methane production often coincided with gastrointestinal complaints whereas influenza infections were mostly accompanied by increased breath methane production. A gastroscopic examination as well as a change to a low-fructose diet led to a dramatic shift of methane mixing ratios from high to low methane production. In contrast, a typhus vaccination as well as single chelate injections resulted in significant short-term methane peaks. Thus, this study clearly shows that humans can change from high to low methane emitters and vice versa within relatively short time periods. In the case of low to medium methane emitters the increase observed in methane mixing ratios, likely resulting from immune reactions and inflammatory processes, might indicate non-microbial methane formation under aerobic conditions. Although detailed reaction pathways are not yet known, aerobic methane formation might be related to cellular oxidative-reductive stress reactions. However, a detailed understanding of the pathways involved in human methane formation is necessary to enable comprehensive interpretation of methane breath levels.

摘要

近年来,甲烷作为呼出人体呼吸的成分之一,被认为是提供肠道微生物活性信息的潜在生物标志物。一些研究表明,呼吸甲烷状态与特定的胃肠道疾病之间存在关系。到目前为止,几乎没有人关注个体呼吸甲烷产生的时间可变性。因此,在这里,我们首次对三名志愿者的呼吸甲烷进行了长期监测,监测时间在 196 天至 1002 天之间。在评估结果时,考虑了每个人在监测期间的健康状况和特定的医疗干预事件,包括胃镜检查、疫苗接种、饮食改变和螯合疗法。作为主要结果,呼吸甲烷混合比在个体特定范围内显示出相当大的可变性。有趣的是,呼吸甲烷产量的降低通常与胃肠道不适同时发生,而流感感染则大多伴随着呼吸甲烷产量的增加。胃镜检查以及饮食中果糖含量的降低导致甲烷混合比从高甲烷产生急剧转变为低甲烷产生。相比之下,斑疹伤寒疫苗接种以及单一螯合注射导致甲烷峰值显著短期增加。因此,这项研究清楚地表明,人类可以在相对较短的时间内从高甲烷排放者转变为低甲烷排放者,反之亦然。在低到中甲烷排放者中,观察到的甲烷混合比增加,可能是由于免疫反应和炎症过程导致的,这可能表明在有氧条件下非微生物甲烷的形成。虽然详细的反应途径尚不清楚,但有氧甲烷的形成可能与细胞氧化还原应激反应有关。然而,要全面解释甲烷呼气水平,就必须详细了解涉及人类甲烷形成的途径。

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