4.8 Article

Old carbon reservoirs were not important in the deglacial methane budget

Journal

SCIENCE
Volume 367, Issue 6480, Pages 907-+

Publisher

AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.aax0504

Keywords

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Funding

  1. NSF [PLR-1245659, PLR-1245821, PLR-1246148]
  2. Packard Fellowship for Science and Engineering
  3. European Research Council (ERC) under the European Union's Seventh Framework Programme FP7/2007-2013 ERC Grant [226172]
  4. Swiss National Science Foundation [200020_172506]
  5. Australian Government for the Centre for Accelerator Science at ANSTO through the National Collaborative Research Infrastructure Strategy
  6. National Institute of Water and Atmospheric Research through the Greenhouse Gases, Emissions and Carbon Cycle Science Program
  7. NERC [bas0100034] Funding Source: UKRI
  8. Swiss National Science Foundation (SNF) [200020_172506] Funding Source: Swiss National Science Foundation (SNF)

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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 (Delta C-14, delta C-13, and delta D) 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.

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