Microbial carbon monoxide consumption in salt marsh sediments

We have examined sediments from a fringing salt marsh in Maine to further understand marine CO metabolism, about which relatively little is known. Intact cores from the marsh emitted CO during dark oxic incubations, but emission rates were significantly higher during anoxic incubations, which provided evidence for simultaneous production and aerobic consumption in surface sediments. CO emission rates were also elevated when cores were exposed to light, which indicated that photochemical reactions play a role in CO production. A kinetic analysis of marsh surface sediments yielded an apparent K(m) of about 82 ppm, which exceeded values reported for well-aerated soils that consume atmospheric CO (65nM). Surface (0-0.2 cm depth interval) sediment slurries incubated under oxic conditions rapidly consumed CO, and methyl fluoride did not inhibit uptake, which indicated that neither ammonia nor methane oxidizers contributed to the observed activity. In contrast, aerobic CO uptake was inhibited by additions of readily available organic substrates (pyruvate, glucose and glycine), but not by cellulose. CO was also consumed by surface and sub-surface sediment slurries incubated under anaerobic conditions, but rates were less than during aerobic incubations. Molybdate and nitrate or nitrite, but not 2-bromoethanesulfonic acid, partially inhibited anaerobic uptake. These results suggest that sulfidogens and acetogens, but not dissimilatory nitrate reducers or methanogens, actively consume CO. Sediment-free plant roots also oxidized CO aerobically; rates for Spartina patens and Limonium carolinianum roots were significantly higher than rates for Spartina alterniflora roots. Thus plants may also impact CO cycling in estuarine environments.     

Nitrate-dependent anaerobic carbon monoxide oxidation by aerobic CO-oxidizing bacteria

Two dissimilatory nitrate-reducing (Burkholderia xenovorans LB400 and Xanthobacter sp. str. COX) and two denitrifying isolates (Stappia aggregata IAM 12614 and Bradyrhizobium sp. str. CPP), previously characterized as aerobic CO oxidizers, consumed CO at ecologically relevant levels (<100 ppm) under anaerobic conditions in the presence, but not absence, of nitrate. None of the isolates were able to grow anaerobically with CO as a carbon or energy source, however, and nitrate-dependent anaerobic CO oxidation was inhibited by headspace concentrations >100-1000 ppm. Surface soils collected from temperate, subtropical and tropical forests also oxidized CO under anaerobic conditions with no lag. The observed activity was 25-60% less than aerobic CO oxidation rates, and did not appear to depend on nitrate. Chloroform inhibited anaerobic but not aerobic activity, which suggested that acetogenic bacteria may have played a significant role in forest soil anaerobic CO uptake.     

Carbon monoxide uptake kinetics in unamended and long-term nitrogen-amended temperate forest soils

The effect of nitrogen (N) additions on the dynamics of carbon monoxide consumption in temperate forest soils is poorly understood. We measured soil CO profiles, potential rates of CO consumption and uptake kinetics in temperate hardwood and pine control plots and plots amended with 50 and 150 kg N ha-1 year-1 for more than 15 years. Soil profiles of CO concentrations were above atmospheric levels in the high-N plots of both stands, suggesting that in these forest soils the balance between consumption and production may be shifted so that either production is increased or consumption decreased. Highest rates of CO consumption were measured in the organic horizon and decreased with soil depth. In the N-amended plots, CO consumption increased in all but one soil depth of the hardwood stand, but decreased in all soil depths of the pine stand. CO enzyme affinities increased with soil depth in the control plots. However, enzyme affinities in the most active soil depths (organic and 0-5 cm mineral) decreased in response to low levels of N in both stands. In the high-N plots, affinities dramatically-increased in the hardwood stand, but decreased in the organic horizon and increased slightly in the 0-5 cm mineral soil in the pine stand. These findings indicate that long-term N addition either by fertilization or deposition may alter the size, composition and/or physiology of the community of CO consumers so that their ability to act as a sink for atmospheric CO has changed. This change could have a substantial effect on the lifetime of greenhouse gases such as CH4 and therefore the future of Earth's climate.     

Protective effect of carbon monoxide in transplantation

During the last decades due to the development of new immunosuppressive agents and improvements in organ preservation methods, surgical techniques, and postoperative care, organ transplantation has become an ultimate therapeutic option for irreversible organ failure. Early graft survival has significantly improved; however, the long-term outcome remains unsatisfactory. Multiple factors, both immunogenic and non-immunogenic etiologies, are involved in the deterioration of the allografts, and the recent use of expanded criteria donors to overcome the organ shortage may also contribute to the graft losses. Carbon monoxide (CO) is commonly viewed as a poison in high concentrations due to its ability to interfere with oxygen delivery. However, CO is endogenously produced in the body as a byproduct of heme degradation by the heme oxygenase (HO) and has recently received notable attention as a gaseous regulatory molecule. In fact, an augmentation of endogenous CO by induction of HO-1 or exogenously added CO is known to have potent cytoprotective effects in various disease models. Several recent reports have demonstrated that CO provides potent cytoprotective effects in the field of organ and cell transplantation. CO is able to prevent ischemia/reperfusion injury, allograft rejection, and xenograft rejection via its anti-inflammatory, anti-apoptotic and anti-proliferation effects, suggesting that CO might be a valuable therapeutic option in the field of transplantation. Based on the recent advancement of our understanding of CO as a new therapeutic molecule, this review attempts to summarize the functional roles as well as biological and molecular mechanisms of CO in transplantation and discusses potential CO application to the clinical transplant setting.     

内源性一氧化碳在大鼠高血压发病中的作用

本实验研究内源性血红素氧化酶／一氧化碳系统在大鼠高血压发病听作用。２,４二甘油次卟啉锌是体内ＨＯ活必抑制剂 。     

Biohydrogen production from carbon monoxide and water byRhodopseudomonas palustris P4

A reactor-scale hydrogen (H₂) productionvia the water-gas shift reaction of carbon monoxide (CO) and water was studied using the purple nonsulfur bacterium,Rhodopseudomonas palustris P4. The experiment was conducted in a two-step process: an aerobic/chemoheterotrophic cell growth step and a subsequent anaerobic H₂ production step. Important parameters investigated included the agitation speed, inlet CO concentration and gas retention time. P4 showed a stable H₂ production capability with a maximum activity of 41 mmol H₂ g cell⁻¹h⁻¹ during the continuous reactor operation of 400 h. The maximal volumetric H₂ production rate was estimated to be 41 mmol H₂ L¹h⁻¹, which was about nine-fold and fifteen-fold higher than the rates reported for the photosynthetic bacteriaRhodospirillum rubrum andRubrivivax gelatinosus, respectively. This is mainly attributed to the ability of P4 to grow to a high cell density with a high specific H₂ production activity. This study indicates that P4 has an outstanding potential for a continuous H₂ productionvia the water-gas shift reaction once a proper bioreactor system that provides a high rate of gas-liquid mass transfer is developed.     

Impacts of plant roots on soil CO cycling and soil–atmosphere CO exchange

Carbon monoxide (CO) plays a major role in tropospheric chemical dynamics. Accordingly, global CO budgets have been reasonably well documented. Atmospheric CO consumption by soils contributes significantly to these budgets, with the magnitude of the sink generally considered to reflect a balance between microbial uptake and abiological production. However, assays of live fine roots showed that diverse intact plants produced carbon monoxide at net rates ranging from 2 to 3000 mµg gdw⁻⁻¹ d⁻⁻¹. CO production was greater for legumes than nonlegumes, and primarily associated with nodules. Excised roots from woody and herbaceous plants produced CO at comparable rates. CO production rates were similar for roots of intact plants and roots excised from those plants. The magnitude of net CO fluxes from roots was determined in part by the balance between simultaneous production and consumption. Surface sterilization of roots indicated that CO consumption was due, in part, rhizoplane CO-oxidizing bacteria, but maximum CO consumption rates were typically only a small fraction of net production rates. Assays in a Brazilian agroecosystem indicated that root CO production affects soil–atmosphere CO exchange. Estimates of global CO production rates indicated that roots contribute about 170–260 Tg CO to the soil atmosphere annually, an amount comparable to current estimates of atmospheric CO uptake by soils, and much larger than estimates of net abiological soil CO production.     

Pre-conditioning induced by carbon monoxide provides neuronal protection against apoptosis

Carbon monoxide (CO) is an endogenous product of mammalian cells generated by heme-oxygenase, presenting anti-apoptotic properties in several tissues. The present work demonstrates the ability of small amounts of exogenous CO to prevent neuronal apoptosis induced by excitotoxicity and oxidative stress in mice primary culture of cerebellar granule cells. Additionally, our data show that endogenous CO is a heme-oxygenase product critical for its anti-apoptotic activity. Despite being neuroprotective, CO also induces reactive oxygen species generation in neurons. These two phenomena suggest that CO induces pre-conditioning (PC) to prevent cell death. The role of several PC mediators, namely soluble guanylyl cyclase, nitric oxide (NO) synthase, and ATP-dependent mitochondrial K channel (mitoK(ATP)) was addressed. Inhibition of soluble guanylyl cyclase or NO synthase activity, or closing of mitoK(ATP) abolishes the protective effect conferred by CO. In addition, CO treatment triggers cGMP and NO production in neurons. Opening of mitoK(ATP), which appears to be critical for CO prevention of apoptosis, might be a later event. We also demonstrated that reactive oxygen species generation and de novo protein synthesis are necessary for CO PC effect and neuroprotection. In conclusion, CO induces PC and prevents neuronal apoptosis, therefore constituting a novel and promising candidate for neuroprotective therapies.     

腹腔注射法制备一氧化碳中毒迟发性脑病大鼠模型

目的：建立可靠的急性一氧化碳（CO）中毒迟发性脑病的动物模型。方法：雄性SD大鼠,分次腹腔注射CO染毒制备模型,动态监测尾血碳氧血红蛋白（HbCO）浓度;Morris水迷宫检测大鼠1-5w逃避潜伏期;尼氏染色及TUNEL原位末端凋亡染色检测大脑皮质及海马细胞损伤及凋亡。结果：染毒后,大鼠出现典型的CO重度中毒症状,体内血液HbCO浓度迅速升高,使用分次腹腔注射法,大鼠可维持长时间（〉12h）高HbCO状态（HbCO〉48%）;中毒组大鼠水迷宫检测认知功能较对照组下降,病理学检查显示大鼠出现脑细胞损伤、凋亡明显。结论：本研究建立了一种较为符合迟发性脑病临床特征的动物模型,具有简单、可靠、重复性好的特点,为深入研究急性CO中毒致迟发性脑损伤的机制提供可靠基础。     

腹腔注射法制备一氧化碳中毒迟发性脑病大鼠模型

目的:建立可靠的急性一氧化碳(CO)中毒迟发性脑病的动物模型。方法:雄性SD大鼠,分次腹腔注射CO染毒制备模型,动态监测尾血碳氧血红蛋白(HbCO)浓度;Morris水迷宫检测大鼠1-5w逃避潜伏期;尼氏染色及TUNEL原位末端凋亡染色检测大脑皮质及海马细胞损伤及凋亡。结果:染毒后,大鼠出现典型的CO重度中毒症状,体内血液HbCO浓度迅速升高,使用分次腹腔注射法,大鼠可维持长时间(>12h)高HbCO状态(HbCO>48%);中毒组大鼠水迷宫检测认知功能较对照组下降,病理学检查显示大鼠出现脑细胞损伤、凋亡明显。结论:本研究建立了一种较为符合迟发性脑病临床特征的动物模型,具有简单、可靠、重复性好的特点,为深入研究急性CO中毒致迟发性脑损伤的机制提供可靠基础。     

一氧化碳在低氧性肺血管收缩反应中的作用

目的和方法 :观察外源性一氧化碳 (CO)对大鼠离体肺动脉环低氧性收缩反应 (HPV)的影响 ,并通过观察血红素氧化酶抑制剂ZnPPIX对HPV的影响 ,探讨内源性一氧化碳在HPV中的作用及机制。结果 :低氧可使苯肾上腺素 (PE)预收缩的肺动脉环出现明显的收缩反应 ,肺动脉cGMP含量下降 ;用ZnPPIX孵育后 ,低氧后的肺动脉cGMP含量增加 ,低氧性肺血管收缩反应 (HPV)受抑 ;外源性CO可明显增加肺动脉cGMP含量 ,HPV明显受抑。结论 :外源性CO及ZnPPIX可增加低氧后的肺动脉cGMP含量 ,抑制HPV ,内源性CO减少导致cGMP含量下降可能是HPV的原因之一     

Photooxidative production of carbon monoxide by phototrophic microorganisms

Net photosynthesis and CO production were measured in cell suspensions of Chlorella fusca. The rate of net photosynthesis showed saturation curves with increasing radiation intensities and CO₂-mixing ratios. Maximum rates were found at 35° C with a sharp decrease at higher temperatures. By contrast, the rate of CO production was proportional to the radiation intensity and did not show any saturation up to 1.5 kW · m^?2 white light. The CO-production rate was higher in blue than in red light and was independent of the CO₂-mixing ratio of the carrier gas within a range of 0–1000 ppmv. We found that the CO-production rate was constant within the physiological temperature range of 10–35° C, but increased considerably at higher temperatures and that CO production by the chlorophyll-deficient mutant of C. fusca was 5 times that of the wild type. In addition, we measured CO production in cell suspensions of Chromatium vinosum, Rhodopseudomonas sphaeroides and Rhodopseudomonas acidophila, which were grown either anaerobically in the light or aerobically in the dark. CO production could only be observed when the cells were incubated in the presence of oxygen and light. Under these conditions more CO was produced by aerobically grown cells than by phototrophically grown cells of R. sphaeroides and R. acidophila. The results obtained indicate that CO was produced by photosensitized oxidations and not by metabolic processes.     

Heme oxygenase-1 derived carbon monoxide permits maturation of myeloid cells

Critical functions of the immune system are maintained by the ability of myeloid progenitors to differentiate and mature into macrophages. We hypothesized that the cytoprotective gas molecule carbon monoxide (CO), generated endogenously by heme oxygenases (HO), promotes differentiation of progenitors into functional macrophages. Deletion of HO-1, specifically in the myeloid lineage (Lyz-Cre:Hmox1^flfl), attenuated the ability of myeloid progenitors to differentiate toward macrophages and decreased the expression of macrophage markers, CD14 and macrophage colony-stimulating factor receptor (MCSFR). We showed that HO-1 and CO induced CD14 expression and efficiently increased expansion and differentiation of myeloid cells into macrophages. Further, CO sensitized myeloid cells to treatment with MCSF at low doses by increasing MCSFR expression, mediated partially through a PI3K-Akt-dependent mechanism. Exposure of mice to CO in a model of marginal bone marrow transplantation significantly improved donor myeloid cell engraftment efficiency, expansion and differentiation, which corresponded to increased serum levels of GM-CSF, IL-1α and MCP-1. Collectively, we conclude that HO-1 and CO in part are critical for myeloid cell differentiation. CO may prove to be a novel therapeutic agent to improve functional recovery of bone marrow cells in patients undergoing irradiation, chemotherapy and/or bone marrow transplantation.     

Effect of dietary protein, zinc, and carbon monoxide on fetal zinc concentration in mice

Dietary protein and zinc deficiencies known to be detrimental to the developing fetus are common in pregnant women in developing countries. Everyone in modern society is at risk of exposure to carbon monoxide (CO). This study was conducted to observe the effect of dietary protein, zinc, and exposure to CO on the fetal zinc concentrations by factorial experimentation. Pregnant mice of CD-1 strain were maintained on 17% (control) or 9% (deficient) protein diets mixed with deficient, normal (control), or supplemental zinc throughout gestation. The dams in each dietary group were exposed to air (control) or 500 ppm CO in air in environmental chambers from gestation day 8 to gestational day 18. The dams were sacrificed on d 18 and fetal zinc levels were measured by atomic absorption spectrophotometry. Carbon monoxide levels used in this study had no significant effect on fetal zinc concentration in any treatment group. When both dietary protein and zinc levels were normal, the mean fetal zinc concentrations were higher than all other dietary protein/zinc combinations (15.2±6.0 and 14.2±4.1 μg Zn/g of tissue for 0 and 500 ppm CO levels). However, when dietary protein levels were deficient, supplemental zinc increased the fetal zinc concentrations significantly (12.7±3.8 and 13.1±0.3.6 μg Zn/g of tissue, in 0 and 500 ppm CO groups) as compared to zinc-deficient groups (8.7±3.0 and 10.0±3.3 μg Zn/g of tissue in 0 and 500 ppm CO groups). The results of this study may be relevant to populations that experience both marginal zinc and protein diets during gestation.     

Over-expression of carbon monoxide dehydrogenase-I with an accessory protein co-expression: a key enzyme for carbon dioxide reduction

Carbon monoxide dehydrogenase-I (CODH-I) from the CO-utilizing bacterium Carboxydothermus hydrogenoformans are expected to be utilized as a part of reproducible carbon dioxide photoreduction system. However, the over-expression system for CODH-I remains to be constructed. CODH-I constitutes a hydrogenase/CODH gene cluster including a gene encoding a Ni-insertion accessory protein, CooC (cooC3). Through co-expression of CooC3, we found an over-expression system with higher activity. The Rec-CODH-I with the co-expression exhibits 8060?U/mg which was approximately threefold than that without co-expression (2270?U/mg). In addition, co-expression resulted in Ni²⁺ content increase; the amount of Ni atoms of Rec-CODH-I was approximately thrice than that without co-expression.     

一氧化碳对大鼠离体肺动脉的舒张作用

本研究观察了一氧化碳 (CO)对离体大鼠肺动脉的舒张作用。制备Wistar大鼠肺动脉环 ,作出ACh浓度效应曲线之后 ,肺动脉环用一氧化氮合成酶抑制剂L NAME 3 0 μmol/L (n =10 )或血红素氧化酶抑制剂ZnPPIX 10μmol/L +L NAME 3 0 μmol/L (n =10 )孵育 3 0min ,再制备一个ACh的浓度效应曲线 ,观察ZnPPIX对ACh的浓度效应曲线的影响。另取一组肺动脉环 ,分为内皮完整组和去内皮组 ,观察外源性CO对肺动脉环张力的影响。结果表明 ,用L NAME孵育后 ,ACh的血管舒张反应受抑 ,最大抑制率为 5 0 4± 9 2 % ;用ZnPPIX +L NAME孵育后 ,ACh的血管舒张反应进一步受抑 ,最大抑制率为 84 4± 11 2 %。外源性CO无论对内皮完整组还是去内皮组肺动脉都有舒张作用。本研究提示 ,ZnPPIX可抑制ACh的内皮依赖性肺动脉舒张反应 ,CO是一个内皮源性的血管舒张因子 ,外源性CO可舒张肺动脉     

吸入一氧化碳防治肢体缺血／再灌注所致肝脏损伤的实验研究

目的：观察吸入外源性一氧化碳（CO）对肢体缺血／再灌注（I／R）所致肝脏损伤的防治作用。方法：健康SD大鼠100只,随机分为假手术（S）、假手术吸入CO（SC）、I／R、I／R吸入CO（RC）组。通过夹闭股动脉4h、再开放6—72h、10d复制肢体L／R致肝脏损伤模型。S、I／R组吸入普通医用空气,SC、RC组吸入含CO（体积分数为0．05％）的医用空气。光镜观察肝组织病理学变化,全自动生化分析仪检测血谷丙转氨酶（GPT）,流式细胞仪检测肝细胞凋亡百分比及bax、bcl-2的表达水平。结果：S组与SC组比较,各项观察指标无显著差别;与SC组比较,I/R及RC组肝组织呈病理改变,血清GPT及肝细胞凋亡百分比明显升高;I／R组肝细胞bax蛋白的表达水平明显升高。和L／R组相比。RC组肝组织损伤程度减轻,血清GPT、肝细胞凋亡百分比及bax蛋白的表达水平明显降低,而肝细胞bcl-2蛋白的表达水平显著升高。结论：吸入适量外源性CO对肢体I／R所致肝脏损伤有防治效应。     

Influence of carbon monoxide on metabolite formation in Methanosarcina acetivorans

Methanogenic archaea conserve energy for growth by reducing some one- and two-carbon compounds to methane and concomitantly generating an ion motive force. Growth of Methanosarcina acetivorans on carbon monoxide (CO) is peculiar as it involves formation of, besides methane, formate, acetate and methylated thiols. It has been argued that methane formation is partially inhibited under carboxidotrophic conditions and that the other products result from either detoxification of CO or from bypassing methanogenesis with other pathways for energy conservation. To gain a deeper understanding of the CO-dependent physiology of M. acetivorans we analyzed metabolite formation in resting cells. The initial rates of methane, acetate, formate, and dimethylsulfide formation increased differentially with increasing CO concentrations but were maximal already at the same moderate CO partial pressure. Strikingly, further increase of the amount of CO was not inhibitory. The maximal rate of methane formation from CO was approximately fivefold lower than that from methanol, consistent with the previously observed significant downregulation of the energy converting sodium-dependent methyltransferase. The rate of dimethylsulfide formation from CO was only 1–2% of that of methane formation under any conditions tested. Implications of the data presented for previously proposed pathways of CO utilization are discussed.     

内源性一氧化碳对内毒素休克肺组织和肾组织保护作用的实验研究

目的：研究内毒素休克时内源性一氧化碳（CO）对肺组织和肾组织的保护作用及其机制;方法：采用盲肠结扎穿孔（CLP）的方法建立大鼠内毒素休克模型,通过免疫组化、光镜下组织形态学观察及超氧化物岐化酶活性、丙二醛含量的测定进行研究;结果：治疗组肺组织和肾组织病变明显减轻,炎症反应及脂质过氧化程度减轻;结论：内毒素休克时内源性CO对肺组织和肾组织具有保护作用,且此保护作用与其抑制炎症反应和抗氧化作用有重要关系。