the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 18 Jun 2025
Global inventory of doubly substituted isotopologues of methane (Δ13CH3D and Δ12CH2D2)
Abstract. Measurements of methane (CH4) molecules containing two rare isotopes (13CH3D and 12CH2D2), also termed doubly substituted or ‘clumped’ isotopologues, have the potential to provide two additional isotopic dimensions to help investigating mechanisms producing the recent global trends and CH4 budget over decadal timescale. In this work, we summarise the current state of research on doubly substituted CH4 isotopologues, with an emphasis on compiling results of all relevant work. The database comprises 1475 records compiled from the literature published until April 2025 (https://dx.doi.org/10.5285/51ae627da5fb41b8a767ee6c653f83e6). For field samples, 40 % of records were sourced from natural gas reservoirs, while microbial terrestrial (e.g., agriculture, lake, wetland) samples account only for 12.5 %. Lakes samples contribute 75 % to collected microbial terrestrial samples. There is limited or no representation of samples coming from significant microbial CH4 sources to the atmosphere, like wetlands, agriculture and landfill. To date, laboratory experiments were mostly focused on microbial (28 % of samples from laboratory experiments) and pyrogenic (15 %) methanogenesis or anaerobic (16 %), and aerobic (8 %) CH4 oxidation, and only a single contribution to studies of photochemical oxidation via OH and Cl (5 %). The distinct ranges of Δ13CH3D and Δ12CH2D2 values measured in these studies suggests their potential to improve our understanding of atmospheric CH4. This work provides an overview of the major gaps in measurements and identifies where further studies should be focussed to enable the highest immediate impact on understanding global CH4.
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RC1: 'Comment on essd-2025-41', Anonymous Referee #1, 04 Sep 2025
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This paper seeks to organize all measurements of methane clumped isotope measurements published to date. The introduction, explanations, and discussions are complete and it was a pleasure to read.
I have only two larger suggestions for the authors. I leave it to the authors to decide if they want to follow these suggestions.
First, I would suggest providing plots of dD and d13C vs the 13CD and D2 measurements as well as dD vs. d13C – I would provide in the background prior databases for bulk so the data here can be compared to that. This is a way of showing whether the data set assembled here compares well to prior data measured or if there are gaps. Second, I think it is important to consider the clumped data in general in the context of prior bulk isotope measurements such that interpretations of clumping are considered in conjunction with standard measurements.
Second, in the database, I strongly suggest providing the additional 'metadata' such as, for surficial samples, the dD of waters, d13C of CO2 etc. For experiments, such would also be extremely helpful and, where known, the isotopic composition of the organic molecules provided (where relevant). For the thermogenic samples, I would suggest providing the gas compositions and isotopic composition of other molecules (where know). I know this will be annoying to do, but this is the kind of information that makes the database become extremely useful as, any study using this data, will likely need that as well. And so future authors will be stuck compiling this other information over and over again. I note, maybe this is provided, but I only saw a cell indicating what metadata exists.
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A few minor comments:
Line 101-102: clumping is only independent of bulk composition for an equilibrated system. It is a strong function of bulk composition for many non-equilibrium processes (mixing, chemical kinetics, distillation, etc.).
Line 113: In terms of history — there are older attempts to do methane clumping for 12CD4 and claims of exceptional values. Eiler 2007 summarizes this. Ma et al (2008 https://doi.org/10.1016/j.gca.2008.08.014) discussed the idea of the measurement. Tsuji et al. (2012 https://doi.org/10.1016/j.saa.2012.08.028) also attempted this and developed a method, but I wasn’t applied to measurements of environmental samples as far as I recall.
Line 379-383. I understood that there is an emerging understanding that for thermogenic methane, it likely forms out of clumped equilibrium but, at high enough temperatures, rapidly reequilibrates so it reflects peak formation temperature prior to expulsion. This is discussed as far as I remember it the cited papers from Dong, Eldridge, and Xie et al. This is a nuance, but is different from methane representing formation temperatures and formation in equilibrium but rather represents rapid kinetics of H exchange post methane formation and then quenching of the reaction. I recommend checking those papers to verify what they said (or asking them as two are on this paper).
For figure 6, what are the catalytic equilibration samples that are +30 to+40‰? Are those labeled experiments where 13CD was added to a sample then removed during equilibration to verify the catalyst was working? If so, I might not include as they are spiked experiments. I would in general avoid including anything in which labels were added.
Citation: https://doi.org/10.5194/essd-2025-41-RC1
Data sets
Methane doubly substituted (clumped) isotopologues database Sara M. Defratyka, Julianne M. Fernandez, Tim Arnold https://dx.doi.org/10.5285/51ae627da5fb41b8a767ee6c653f83e6
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