Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years

Research output: Contribution to journalJournal articleResearchpeer-review

  • Laetitia Loulergue
  • Adrian Schilt
  • Renato Spahni
  • Valérie Masson-Delmotte
  • Blunier, Thomas
  • Bénédicte Lemieux
  • Jean-Marc Barnola
  • Dominique Raynaud
  • Thomas F Stocker
  • Jérôme Chappellaz
Atmospheric methane is an important greenhouse gas and a sensitive indicator of climate change and millennial-scale temperature variability. Its concentrations over the past 650,000 years have varied between approximately 350 and approximately 800 parts per 10(9) by volume (p.p.b.v.) during glacial and interglacial periods, respectively. In comparison, present-day methane levels of approximately 1,770 p.p.b.v. have been reported. Insights into the external forcing factors and internal feedbacks controlling atmospheric methane are essential for predicting the methane budget in a warmer world. Here we present a detailed atmospheric methane record from the EPICA Dome C ice core that extends the history of this greenhouse gas to 800,000 yr before present. The average time resolution of the new data is approximately 380 yr and permits the identification of orbital and millennial-scale features. Spectral analyses indicate that the long-term variability in atmospheric methane levels is dominated by approximately 100,000 yr glacial-interglacial cycles up to approximately 400,000 yr ago with an increasing contribution of the precessional component during the four more recent climatic cycles. We suggest that changes in the strength of tropical methane sources and sinks (wetlands, atmospheric oxidation), possibly influenced by changes in monsoon systems and the position of the intertropical convergence zone, controlled the atmospheric methane budget, with an additional source input during major terminations as the retreat of the northern ice sheet allowed higher methane emissions from extending periglacial wetlands. Millennial-scale changes in methane levels identified in our record as being associated with Antarctic isotope maxima events are indicative of ubiquitous millennial-scale temperature variability during the past eight glacial cycles.
Original languageEnglish
Issue number7193
Pages (from-to)383-6
Number of pages3
Publication statusPublished - 2008

Bibliographical note

Keywords: Atmosphere; Greenhouse Effect; History, Ancient; Ice Cover; Methane; Temperature; Time Factors; Tropical Climate; Wetlands

ID: 9224179