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Original Articles

The atmospheric CH4 increase since the Last Glacial Maximum

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Pages 242-257 | Received 10 Mar 1992, Accepted 02 Nov 1992, Published online: 18 Jan 2017

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Casper Labuschagne, Brett Kuyper, Ernst-Günther Brunke, Thumeka Mokolo, Danie van der Spuy, Lynwill Martin, Ernst Mbambalala, Bhawoodien Parker, M. Anwar H. Khan, Michael T. Davies-Coleman, Dudley E. Shallcross & Warren Joubert. (2018) A review of four decades of atmospheric trace gas measurements at Cape Point, South Africa. Transactions of the Royal Society of South Africa 73:2, pages 113-132.
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JéÔme A. Chappellaz, Inez Y. Fung & Anne M. Thompson. (1993) The atmospheric CH4 increase since the Last Glacial Maximum. Tellus B: Chemical and Physical Meteorology 45:3, pages 228-241.
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Articles from other publishers (27)

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James E. Lee, Jon S. Edwards, Jochen Schmitt, Hubertus Fischer, Michael Bock & Edward J. Brook. (2020) Excess methane in Greenland ice cores associated with high dust concentrations. Geochimica et Cosmochimica Acta 270, pages 409-430.
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R. B. Shakirov, M. G. Valitov, A. I. Obzhirov, V. F. Mishukov, A. V. Yatsuk, N. S. Syrbu & O. V. Mishukova. (2019) Methane anomalies, its flux on the sea–atmosphere interface and their relations to the geological structure of the South-Tatar sedimentary basin (Tatar Strait, the Sea of Japan). Marine Geophysical Research 40:4, pages 581-600.
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V. Ramaswamy, W. Collins, J. Haywood, J. LeanN. Mahowald, G. Myhre, V. Naik, K. P. Shine, B. Soden, G. Stenchikov & T. Storelvmo. (2019) Radiative Forcing of Climate: The Historical Evolution of the Radiative Forcing Concept, the Forcing Agents and their Quantification, and Applications. Meteorological Monographs 59, pages 14.1-14.101.
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A. Quiquet, A.T. Archibald, A.D. Friend, J. Chappellaz, J.G. Levine, E.J. Stone, P.J. Telford & J.A. Pyle. (2015) The relative importance of methane sources and sinks over the Last Interglacial period and into the last glaciation. Quaternary Science Reviews 112, pages 1-16.
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J. R. Melton, H. Schaefer & M. J. Whiticar. (2012) Enrichment in <sup>13</sup>C of atmospheric CH<sub>4</sub> during the Younger Dryas termination. Climate of the Past 8:4, pages 1177-1197.
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Joël Savarino & Samuel Morin. 2012. Handbook of Environmental Isotope Geochemistry. Handbook of Environmental Isotope Geochemistry 835 864 .
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S. A. Kunasek, B. Alexander, E. J. Steig, M. G. Hastings, D. J. Gleason & J. C. Jarvis. (2008) Measurements and modeling of Δ 17 O of nitrate in snowpits from Summit, Greenland . Journal of Geophysical Research 113:D24.
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Hinrich SchaeferMichael J. WhiticarEdward J. BrookVasilii V. PetrenkoDominic F. FerrettiJeffrey P. Severinghaus. (2006) Ice Record of δ 13 C for Atmospheric CH 4 Across the Younger Dryas-Preboreal Transition . Science 313:5790, pages 1109-1112.
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Malcolm Possell, C. Nicholas Hewitt & David J. Beerling. (2005) The effects of glacial atmospheric CO2 concentrations and climate on isoprene emissions by vascular plants. Global Change Biology 11:1, pages 60-69.
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Jed O. Kaplan. (2002) Wetlands at the Last Glacial Maximum: Distribution and methane emissions. Geophysical Research Letters 29:6, pages 3-1-3-4.
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Edward J. BrookTodd SowersJoe Orchardo. (1996) Rapid Variations in Atmospheric Methane Concentration During the Past 110,000 Years. Science 273:5278, pages 1087-1091.
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Robert M. Kalin & John L. Jirikowic. (2016) A plausible hydrological scenario for the Bølling-Allerød atmospheric methane increase. The Holocene 6:1, pages 111-118.
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