62 citations as recorded by crossref.

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2. Widespread natural methane and oil leakage from sub-marine Arctic reservoirs P. Serov et al. 10.1038/s41467-023-37514-9
3. Relevant methane emission to the atmosphere from a geological gas manifestation A. Mazzini et al. 10.1038/s41598-021-83369-9
4. Optically Switched Dual-Wavelength Cavity Ring-Down Spectrometer for High-Precision Isotope Ratio Measurements of Methane δD in the Near Infrared T. Chen et al. 10.1021/acs.analchem.0c05090
5. Preindustrial 14CH4 indicates greater anthropogenic fossil CH4 emissions B. Hmiel et al. 10.1038/s41586-020-1991-8
6. Source and age of dissolved and gaseous carbon in a peatland–riparian–stream continuum: a dual isotope (14C and δ13C) analysis F. Leith et al. 10.1007/s10533-014-9977-y
7. Carbon and hydrogen isotopic composition of methane over the last 1000 years J. Mischler et al. 10.1029/2009GB003460
8. Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2 P. Sperlich et al. 10.1002/2014GB005007
9. Comparative Analysis of Gas-Geochemical Data from Ground-Based and Satellite Observations of the Sakhalin Island and Its Shelf (Northeast Russia): Tectonic Consequences N. Syrbu et al. 10.31857/S0016853X2302008X
10. Comparative Analysis of Gas-Geochemical Data from Ground-Based and Satellite Observations of the Sakhalin Island and Its Shelf (Northeast Russia): Tectonic Consequences N. Syrbu et al. 10.1134/S0016852123020085
11. Methane Isotope Instrument Validation and Source Identification at Four Corners, New Mexico, United States C. Arata et al. 10.1021/acs.jpca.5b12737
12. A 21st-century shift from fossil-fuel to biogenic methane emissions indicated by 13 CH 4 H. Schaefer et al. 10.1126/science.aad2705
13. Rain-fed pulses of methane from East Africa during 2018–2019 contributed to atmospheric growth rate M. Lunt et al. 10.1088/1748-9326/abd8fa
14. Reduced methane growth rate explained by decreased Northern Hemisphere microbial sources F. Kai et al. 10.1038/nature10259
15. Anthropogenic emission is the main contributor to the rise of atmospheric methane during 1993–2017 Z. Zhang et al. 10.1093/nsr/nwab200
16. The global methane budget 2000–2012 M. Saunois et al. 10.5194/essd-8-697-2016
17. Global and Regional Emissions of Radiocarbon from Nuclear Power Plants from 1972 to 2016 G. Zazzeri et al. 10.1017/RDC.2018.42
18. Improved Constraints on Global Methane Emissions and Sinks Using δ13C‐CH4 X. Lan et al. 10.1029/2021GB007000
19. Emissions of anaerobically produced methane by trees A. Rice et al. 10.1029/2009GL041565
20. Effects of granular activated carbon on methane removal performance and methanotrophic community of a lab-scale bioreactor E. Lee et al. 10.1080/10934529.2014.975541
21. Atmospheric 14CH4, 14CO2 and 37Ar measurements around a Swiss pressurized water reactor during an annual revision period C. Espic et al. 10.1016/j.jenvrad.2024.107576
22. A High-precision Measurement System for Carbon and Hydrogen Isotopic Ratios of Atmospheric Methane and Its Application to Air Samples Collected in the Western Pacific Region T. UMEZAWA et al. 10.2151/jmsj.87.365
23. Efficient collection and preparation of methane from low concentration waters for natural abundance radiocarbon analysis K. Sparrow & J. Kessler 10.1002/lom3.10184
24. Enrichment in 13C of atmospheric CH4 during the Younger Dryas termination J. Melton et al. 10.5194/cp-8-1177-2012
25. Very Strong Atmospheric Methane Growth in the 4 Years 2014–2017: Implications for the Paris Agreement E. Nisbet et al. 10.1029/2018GB006009
26. Global Methane Budget 2000–2020 M. Saunois et al. 10.5194/essd-17-1873-2025
27. Role of atmospheric oxidation in recent methane growth M. Rigby et al. 10.1073/pnas.1616426114
28. Strong sensitivity of the isotopic composition of methane to the plausible range of tropospheric chlorine S. Strode et al. 10.5194/acp-20-8405-2020
29. Radiocarbon analysis of methane emitted from the surface of a raised peat bog M. Garnett et al. 10.1016/j.soilbio.2012.03.018
30. Atmospheric methane and nitrous oxide: challenges alongthe path to Net Zero E. Nisbet et al. 10.1098/rsta.2020.0457
31. Extracting a History of Global Fire Emissions for the Past Millennium From Ice Core Records of Acetylene, Ethane, and Methane M. Nicewonger et al. 10.1029/2020JD032932
32. A survey of methane isotope abundance (14C, 13C, 2H) from five nearshore marine basins that reveals unusual radiocarbon levels in subsurface waters J. Kessler et al. 10.1029/2008JC004822
33. From biota to chemistry and climate: towards a comprehensive description of trace gas exchange between the biosphere and atmosphere A. Arneth et al. 10.5194/bg-7-121-2010
34. Kinetic isotope effects of 12CH3D  + OH and 13CH3D  + OH from 278 to 313 K L. Joelsson et al. 10.5194/acp-16-4439-2016
35. Missing methane emissions from leaves of terrestrial plants D. BEERLING et al. 10.1111/j.1365-2486.2008.01607.x
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37. Methane Emissions from Wastewater, Wetlands, Mangroves and Hydroelectric Dams: Developing Appropriate Emission Factors for Region-Specific GHGS (ERG) J. Pandey et al. 10.1177/097324701000600103
38. Optimal estimation of the present‐day global methane budget L. Neef et al. 10.1029/2009GB003661
39. Simulating idealized Dansgaard-Oeschger events and their potential impacts on the global methane cycle P. Hopcroft et al. 10.1016/j.quascirev.2011.08.012
40. Detection of Fossil and Biogenic Methane at Regional Scales Using Atmospheric Radiocarbon H. Graven et al. 10.1029/2018EF001064
41. The atmospheric cycling of radiomethane and the "fossil fraction" of the methane source K. Lassey et al. 10.5194/acp-7-2141-2007
42. A novel approach to rapidly tracking whole-farm methane emissions H. Chen et al. 10.1088/1748-9326/adb1f6
43. The Global Methane Budget 2000–2017 M. Saunois et al. 10.5194/essd-12-1561-2020
44. Recent changes in methane mixing ratio and its13C content observed in the southwest Pacific region K. Lassey et al. 10.1080/19438151003621441
45. Constraints on the Late Holocene Anthropogenic Contribution to the Atmospheric Methane Budget L. Mitchell et al. 10.1126/science.1238920
46. Assessment of the theoretical limit in instrumental detectability of northern high-latitude methane sources using δ13CCH4 atmospheric signals T. Thonat et al. 10.5194/acp-19-12141-2019
47. Interpreting methane variations in the past two decades using measurements of CH4 mixing ratio and isotopic composition G. Monteil et al. 10.5194/acp-11-9141-2011
48. Isotopic source signatures: Impact of regional variability on theδ13CH4trend and spatial distribution A. Feinberg et al. 10.1016/j.atmosenv.2017.11.037
49. Application of stable isotope analysis for improved understanding of the methane budget: comparison of TROICA measurements with TM3 model simulations O. Tarasova et al. 10.1007/s10874-010-9157-y
50. Balancing the global methane budget: constraints imposed by isotopes and anthropogenic emission inventories K. Lassey & S. Ragnauth 10.1080/19438151003680843
51. Inhibitory effects of sulfur compounds on methane oxidation by a methane-oxidizing consortium E. Lee et al. 10.1016/j.jbiosc.2015.04.006
52. Aircraft Emissions of Methane and Nitrous Oxide during the Alternative Aviation Fuel Experiment G. Santoni et al. 10.1021/es200897h
53. Global and Regional CH4 Emissions for 1995–2013 Derived From Atmospheric CH4, δ13C‐CH4, and δD‐CH4 Observations and a Chemical Transport Model R. Fujita et al. 10.1029/2020JD032903
54. Revisiting enteric methane emissions from domestic ruminants and their δ13CCH4 source signature J. Chang et al. 10.1038/s41467-019-11066-3
55. Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
56. A Structured Approach for the Mitigation of Natural Methane Emissions—Lessons Learned from Anthropogenic Emissions J. Johannisson & M. Hiete 10.3390/c6020024
57. Increasing anthropogenic methane emissions arise equally from agricultural and fossil fuel sources R. Jackson et al. 10.1088/1748-9326/ab9ed2
58. Variations in global methane sources and sinks during 1910–2010 A. Ghosh et al. 10.5194/acp-15-2595-2015
59. Revised records of atmospheric trace gases CO2, CH4, N2O, and δ13C-CO2 over the last 2000 years from Law Dome, Antarctica M. Rubino et al. 10.5194/essd-11-473-2019
60. 14CO2 ACTIVITY IN AIR SAMPLES AND DILUTION FACTOR EVALUATION OF KAKRAPAR GUJARAT SITE, INDIA A. Chandrakar et al. 10.1017/RDC.2023.68
61. Early anthropogenic CH4 emissions and the variation of CH4 and 13CH4 over the last millennium S. Houweling et al. 10.1029/2007GB002961
62. Methane carbon isotope effects caused by atomic chlorine in the marine boundary layer: Global model results compared with Southern Hemisphere measurements W. Allan et al. 10.1029/2006JD007369