Old carbon reservoirs were not important in the deglacial methane budget
dc.contributor.author | Dyonisius, MN | en_AU |
dc.contributor.author | Petrenko, VV | en_AU |
dc.contributor.author | Smith, AM | en_AU |
dc.contributor.author | Hua, Q | en_AU |
dc.contributor.author | Yang, B | en_AU |
dc.contributor.author | Schmitt, J | en_AU |
dc.contributor.author | Beck, J | en_AU |
dc.contributor.author | Seth, B | en_AU |
dc.contributor.author | Bock, M | en_AU |
dc.contributor.author | Hmiel, B | en_AU |
dc.contributor.author | Vimont, I | en_AU |
dc.contributor.author | Menking, JA | en_AU |
dc.contributor.author | Shackleton, SA | en_AU |
dc.contributor.author | Baggenstos, D | en_AU |
dc.contributor.author | Bauska, TK | en_AU |
dc.contributor.author | Rhodes, RH | en_AU |
dc.contributor.author | Sperlich, P | en_AU |
dc.contributor.author | Beaudette, R | en_AU |
dc.contributor.author | Harth, CM | en_AU |
dc.contributor.author | Kalk, M | en_AU |
dc.contributor.author | Brook, EJ | en_AU |
dc.contributor.author | Fischer, H | en_AU |
dc.contributor.author | Severinghaus, JP | en_AU |
dc.contributor.author | Weiss, RF | en_AU |
dc.date.accessioned | 2021-07-08T04:02:27Z | en_AU |
dc.date.available | 2021-07-08T04:02:27Z | en_AU |
dc.date.issued | 2020-02-21 | en_AU |
dc.date.statistics | 2021-07-01 | en_AU |
dc.description | Copyright © 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. This is an article distributed under the terms of the Science Journals Default License. | en_AU |
dc.description.abstract | Permafrost and methane hydrates are large, climate-sensitive old carbon reservoirs that have the potential to emit large quantities of methane, a potent greenhouse gas, as the Earth continues to warm. We present ice core isotopic measurements of methane (Δ14C, δ13C, and δD) from the last deglaciation, which is a partial analog for modern warming. Our results show that methane emissions from old carbon reservoirs in response to deglacial warming were small (<19 teragrams of methane per year, 95% confidence interval) and argue against similar methane emissions in response to future warming. Our results also indicate that methane emissions from biomass burning in the pre-Industrial Holocene were 22 to 56 teragrams of methane per year (95% confidence interval), which is comparable to today. Copyright © 2020 The Authors | en_AU |
dc.identifier.citation | Dyonisius, M. N., Petrenko, V. V., Smith, A. M., Hua, Q., Yang, B., Schmitt, J., Beck, J., Seth, B., Bock, M., Hmiel, B., Vimont, I., Menking, J. A., Shackleton, S. A., Baggenstos, D., Bauska, T. K., Rhodes, R. H., Sperlich, P., Beaudette, R., Harth, C. M., Kalk, M., Brook, E. J., Fischer, H., Severinghaus, J. P. & Weiss, R. F. (2020). Old carbon reservoirs were not important in the deglacial methane budget. Science, 367(6480), 907-910. doi:10.1126/science.aax0504 | en_AU |
dc.identifier.issn | 1095-9203 | en_AU |
dc.identifier.issue | 6480 | en_AU |
dc.identifier.journaltitle | Science | en_AU |
dc.identifier.pagination | 907-910 | en_AU |
dc.identifier.uri | https://doi.org/10.1126/science.aax0504 | en_AU |
dc.identifier.uri | https://apo.ansto.gov.au/dspace/handle/10238/11032 | en_AU |
dc.identifier.volume | 367 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | AAAS | en_AU |
dc.subject | Methane | en_AU |
dc.subject | Carbon | en_AU |
dc.subject | Gas hydrates | en_AU |
dc.subject | Permafrost | en_AU |
dc.subject | Greenhouse gases | en_AU |
dc.subject | Earth atmosphere | en_AU |
dc.subject | Ice | en_AU |
dc.subject | Drill cores | en_AU |
dc.subject | Quaternary period | en_AU |
dc.title | Old carbon reservoirs were not important in the deglacial methane budget | en_AU |
dc.type | Journal Article | en_AU |