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Keppler, F.

Publications and source records attributed to Keppler, F..

6 recordsLinked to original sources

Insights into plant-part specific N2O production in roots and shoots of chicory (C. intybus) using stable isotope labelling

O_LINitrous oxide (N2O) substantially contributes to climate change and stratospheric ozone degradation, yet large uncertainties in its global budget indicate unknown or overlooked sources. Increasing evidence suggests that plants may also produce N2O, though the underlying mechanisms and pathways remain poorly constrained. C_LIO_LITo examine whether plants can form N2O under sterile conditions and to assess the contribution of different plant parts, we applied a novel 15N stable isotope labelling approach using sterile Cichorium intybus root and shoot cultures incubated separately under light and dark conditions. C_LIO_LIAll root/shoot cultures showed N2O formation under dark conditions, whereas shoots under light showed reduced or even uptake of N2O, indicating photosynthetically driven suppression of formation pathways or simultaneous internal degradation of N2O. C_LIO_LIIsotopic analyses revealed distinct formation pathways: roots supplemented with 15NO3- showed position-specific 15N enrichment consistent with N2O formation via nitric oxide as an intermediate, linking root-derived N2O to NO3- reduction. In contrast, root/shoot incubations with 15N-NH4+ supplementation and shoots in darkness emitted N O without clear 15N enrichment suggesting alternative formation pathways independent of these compounds. Our isotopic labelling approach powerfully disentangled N2O formation mechanisms yet highlights necessary further exploration of plant N2O cycling to improve global budgets and enable potential mitigation strategies. C_LI

biochemistry↗

Methylotrophic yeast Candida boidinii enhances the colonization of plant growth-promoting yeast Papiliotrema laurentii in the phyllosphere

Methanol-utilizing microbes are ubiquitous in the phyllosphere, where they assimilate methanol released from pectin, the major component of the plant cell wall. While methylotrophic bacteria Methylobacterium spp. are well studied for their symbiotic relationships with the host plants, the ecology and functional roles of methylotrophic yeasts on plants remain poorly understood. In the effort to isolate yeasts from 26 phyllosphere samples, we identified Candida boidinii as the only methylotrophic yeast, while the remaining isolates, categorized into 17 species in 12 genera, lacked this metabolic trait. To obtain insight into the role of methylotrophic yeasts in the phyllosphere, we investigated the interaction of C. boidinii with a plant growth-promoting yeast (PGPY), Papiliotrema laurentii, one of the identified yeast species during isolation. We found that the colonization of P. laurentii was enhanced by the presence of C. boidinii on Arabidopsis thaliana leaves. Co-cultivation assays revealed that the cell yield of P. laurentii was enhanced by C. boidinii during cultivation on pectin and that the methanol-utilizing ability and pectin methylesterase (PME) activity of C. boidinii contributed to this enhancement. Stable carbon isotope labeling of pectin methylester groups unambiguously confirmed their assimilation by C. boidinii, but not by P. laurentii. These findings suggest that C. boidinii not only survives in the phyllosphere by utilizing pectin-derived methanol but also contributes to the fitness of other yeast species through metabolic cooperation. This study provides new insights into the niche construction and survival strategies of phyllosphere methylotrophic yeasts, highlighting their potential role in shaping microbial community dynamics and promoting beneficial plant-microbe interactions.

microbiology↗

Latitudinal gradients in stable hydrogen isotopes of North American trees

Stable hydrogen isotopes ({delta}2H values) of plant matter provide information about ambient climate conditions and physiological processes.{delta} 2H values of tree stem wood methoxy groups ({delta}2HTM) are increasingly used to reconstruct the isotope composition of precipitation ({delta}2Hprecip) and temperature variability in mid latitudes regions. However, empirical evidence of the basic latitudinal gradients in North America and their inter-continental context are still missing. We sampled 104 tree cores in 13 North American sites ranging from 38{degrees}-69{degrees}N and investigated the relationship between{delta} 2HTM and{delta} 2Hprecip values. Recorded{delta} 2HTM values are highly depleted in 2H relative to meteoric water and align closely with predictions from a biochemical model. Reconstructed temperature changes, derived from{delta} 2HTM values, agree well with instrumental data in North American since 1932. Our results reveal that the latitudinal gradients of{delta} 2HTM values closely resemble{delta} 2Hprecip values across North America. When combining these spatial patterns with{delta} 2HTM and{delta} 2Hprecip data from Europe a strong correlation (R2 = 0.94, p < 0.001) and a consistent fractionation of -193 {+/-} 13 mUr, representative for Northern Hemisphere mid-to-high latitude sites, is established. The validation across North American and European transects serves as a foundational basis for advancing applications in biogeochemistry and paleoclimate research.

plant biology↗

Methane formation driven by light and heat prior to the origin of life

Methane is a potent greenhouse gas, which likely enabled the evolution of life by keeping the early Earth warm. Here, we demonstrate new routes towards abiotic methane formation under early-earth conditions from methylated sulfur and nitrogen compounds with prebiotic origin. These compounds are demethylated in Fenton reactions governed by ferrous iron and reactive oxygen species, produced by light and heat in aqueous environments. The reactions generate methyl radicals and ultimately release methane and ethane. Organic iron chelators enhance reaction rates and recycle ferric to ferrous complexes via ligand-to-metal charge transfer, establishing a light-driven iron redox cycle. This abiotic reaction facilitates methane and ethane formation across Earths humid realm, thereby shaping the chemical evolution of the atmosphere prior to the origin of life and beyond. One-Sentence SummaryUnder suboxic and anoxic conditions, iron and reactive oxygen species drive the global formation of methane in aqueous environments.

evolutionary biology↗

COVID19-vaccination affects breath methane dynamics

Methane (CH4) is well known as a component in the exhaled breath of humans. It has been assumed for a long time that formation of CH4 in humans occurs exclusively by anaerobic microbial activity (methanogenesis) in the gastrointestinal tract. A fraction of the produced CH4 is excreted via the lungs and can then be detected in the breath. However, recent studies challenge this view by showing that CH4 might also be produced endogenously in cells by oxidative-reductive stress reactions. Thus, an increased and fluctuating level of breath CH4 compared to the base level of an individual might also indicate enhanced oxidative stress levels. Thus, monitoring breath CH4 levels might have great potential for in vivo diagnostics. Generally, vaccines generate a strong immune response including the production of pro-inflammatory cytokines. To evaluate the effect from current vaccines against COVID-19 on breath CH4 dynamics, breath CH4 was monitored from 12 subjects prior and after the injection of several COVID-vaccines. Prior to COVID-19 vaccination the concentration of breath CH4 was frequently measured by gas chromatograph flame ionization detection (GC-FID, with analytical precision better than 10 parts per billion, ppbv) to obtain the individual variation range of breath CH4 for each subject. Following vaccination, CH4 breath samples were collected at high frequency for a period of 14 days. All subjects monitored showed a strong response in breath CH4 release within 1 to 72 hours after vaccination including shifts and high fluctuations with maximum peaks showing a factor of up to {+/-}100 compared to base values. Thus, it is highly likely that the observed changes in breath CH4 are coupled to immune responses following Covid-19 vaccination. These preliminary results strongly support the hypothesis that non-microbial methane liberation and utilisation in the human body might be also linked to cellular processes and stress responses independent of classical microbial methanogenesis. Thus, CH4 might be used as a breath biomarker for specific immune responses and individual immune states.

biochemistry↗

Widespread formation of methane by Cyanobacteria in aquatic and terrestrial environments

Evidence is accumulating to challenge the paradigm that biogenic methanogenesis, traditionally considered a strictly anerobic process, is exclusive to Archaea. Here we demonstrate that Cyanobacteria living in marine, freshwater and terrestrial environments produce methane at substantial rates under light and dark oxic and anoxic conditions, forming a link between light driven primary productivity and methane production in globally relevant group of phototrophs. Biogenic methane production was enhanced during oxygenic photosynthesis and directly attributed to the cyanobacteria by applying stable isotope labelling techniques. We suggest that formation of methane by Cyanobacteria may contribute to methane accumulation in oxygen-saturated surface waters of marine and freshwater ecosystems. Moreover, in these environments, cyanobacterial blooms already do, and might further occur more frequently during future global warming and thus have a direct feedback on climate change. We further highlight that cyanobacterial methane production not only affects recent and future global methane budgets, but also has implications for inferences on Earths methane budget for the last 3.5 billion years, when this phylum is thought to have first evolved.

microbiology↗