14 citations as recorded by crossref.

1. On the interference of Kr during carbon isotope analysis of methane using continuous-flow combustion–isotope ratio mass spectrometry J. Schmitt et al. 10.5194/amt-6-1425-2013
2. The global methane budget 2000–2012 M. Saunois et al. 10.5194/essd-8-697-2016
3. The interaction of climate change and methane hydrates C. Ruppel & J. Kessler 10.1002/2016RG000534
4. Response of methane emissions from wetlands to the Last Glacial Maximum and an idealized Dansgaard–Oeschger climate event: insights from two models of different complexity B. Ringeval et al. 10.5194/cp-9-149-2013
5. Limited response of peatland CH4 emissions to abrupt Atlantic Ocean circulation changes in glacial climates P. Hopcroft et al. 10.5194/cp-10-137-2014
6. Atmospheric Methane: Comparison Between Methane's Record in 2006–2022 and During Glacial Terminations E. Nisbet et al. 10.1029/2023GB007875
7. The relative importance of methane sources and sinks over the Last Interglacial period and into the last glaciation A. Quiquet et al. 10.1016/j.quascirev.2015.01.004
8. Paleo-Perspectives on Potential Future Changes in the Oxidative Capacity of the Atmosphere Due to Climate Change and Anthropogenic Emissions B. Alexander & L. Mickley 10.1007/s40726-015-0006-0
9. Mechanisms of Methane Hydrate Formation in Geological Systems K. You et al. 10.1029/2018RG000638
10. Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2 P. Sperlich et al. 10.1002/2014GB005007
11. Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4ice core records M. Bock et al. 10.1073/pnas.1613883114
12. An automated GC-C-GC-IRMS setup to measure palaeoatmospheric δ13C-CH4, δ15N-N2O and δ18O-N2O in one ice core sample P. Sperlich et al. 10.5194/amt-6-2027-2013
13. Assessment of diffusive isotopic fractionation in polar firn, and application to ice core trace gas records C. Buizert et al. 10.1016/j.epsl.2012.11.039
14. Using the deuterium isotope composition of permafrost meltwater to constrain thermokarst lake contributions to atmospheric CH4during the last deglaciation L. Brosius et al. 10.1029/2011JG001810