Articles | Volume 8, issue 4
https://doi.org/10.5194/cp-8-1177-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-8-1177-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Enrichment in 13C of atmospheric CH4 during the Younger Dryas termination
J. R. Melton
School of Earth and Ocean Sciences, University of Victoria, P.O. Box 3065 STN CSC, Victoria, BC V8W 3V6, Canada
now at: Canadian Centre for Climate Modelling and Analysis, Environment Canada, Victoria, BC, V8W 2Y2, Canada
H. Schaefer
National Institute of Water and Atmospheric Research Ltd., 301 Evans Bay Pde, Wellington, 6021, New Zealand
M. J. Whiticar
School of Earth and Ocean Sciences, University of Victoria, P.O. Box 3065 STN CSC, Victoria, BC V8W 3V6, Canada
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15 citations as recorded by crossref.
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- The interaction of climate change and methane hydrates C. Ruppel & J. Kessler https://doi.org/10.1002/2016RG000534
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- Atmospheric Methane: Comparison Between Methane's Record in 2006–2022 and During Glacial Terminations E. Nisbet et al. https://doi.org/10.1029/2023GB007875
- The relative importance of methane sources and sinks over the Last Interglacial period and into the last glaciation A. Quiquet et al. https://doi.org/10.1016/j.quascirev.2015.01.004
- Paleo-Perspectives on Potential Future Changes in the Oxidative Capacity of the Atmosphere Due to Climate Change and Anthropogenic Emissions B. Alexander & L. Mickley https://doi.org/10.1007/s40726-015-0006-0
- Mechanisms of Methane Hydrate Formation in Geological Systems K. You et al. https://doi.org/10.1029/2018RG000638
- Pronounced methane cycling in northern lakes coincided with a rapid rise in atmospheric CH 4 during the last deglacial warming X. Yan et al. https://doi.org/10.1126/sciadv.adt2561
- Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2 P. Sperlich et al. https://doi.org/10.1002/2014GB005007
- Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4ice core records M. Bock et al. https://doi.org/10.1073/pnas.1613883114
- 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. https://doi.org/10.5194/amt-6-2027-2013
- Assessment of diffusive isotopic fractionation in polar firn, and application to ice core trace gas records C. Buizert et al. https://doi.org/10.1016/j.epsl.2012.11.039
15 citations as recorded by crossref.
- On the interference of Kr during carbon isotope analysis of methane using continuous-flow combustion–isotope ratio mass spectrometry J. Schmitt et al. https://doi.org/10.5194/amt-6-1425-2013
- The global methane budget 2000–2012 M. Saunois et al. https://doi.org/10.5194/essd-8-697-2016
- The interaction of climate change and methane hydrates C. Ruppel & J. Kessler https://doi.org/10.1002/2016RG000534
- 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. https://doi.org/10.5194/cp-9-149-2013
- Soil microbial community structure and function in permafrost regions: progress and perspectives X. Yang et al. https://doi.org/10.1360/CSB-2025-5328
- Limited response of peatland CH4 emissions to abrupt Atlantic Ocean circulation changes in glacial climates P. Hopcroft et al. https://doi.org/10.5194/cp-10-137-2014
- Atmospheric Methane: Comparison Between Methane's Record in 2006–2022 and During Glacial Terminations E. Nisbet et al. https://doi.org/10.1029/2023GB007875
- The relative importance of methane sources and sinks over the Last Interglacial period and into the last glaciation A. Quiquet et al. https://doi.org/10.1016/j.quascirev.2015.01.004
- Paleo-Perspectives on Potential Future Changes in the Oxidative Capacity of the Atmosphere Due to Climate Change and Anthropogenic Emissions B. Alexander & L. Mickley https://doi.org/10.1007/s40726-015-0006-0
- Mechanisms of Methane Hydrate Formation in Geological Systems K. You et al. https://doi.org/10.1029/2018RG000638
- Pronounced methane cycling in northern lakes coincided with a rapid rise in atmospheric CH 4 during the last deglacial warming X. Yan et al. https://doi.org/10.1126/sciadv.adt2561
- Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2 P. Sperlich et al. https://doi.org/10.1002/2014GB005007
- Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4ice core records M. Bock et al. https://doi.org/10.1073/pnas.1613883114
- 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. https://doi.org/10.5194/amt-6-2027-2013
- Assessment of diffusive isotopic fractionation in polar firn, and application to ice core trace gas records C. Buizert et al. https://doi.org/10.1016/j.epsl.2012.11.039
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