Centennial-scale changes in the global carbon cycle during the last deglaciation

2014/10/28 by Shaun A. Marcott, Thomas Bauska, Thomas K. Bauska +16 · 615 citations
Earth and Planetary Sciences · Engineering · Environmental Science · #Archaeology #Biology #Carbon cycle #Centennial #Climatology #Deglaciation #Earth science #Ecology #Ecosystem #Environmental science #Geography #Geology #Geology and Paleoclimatology Research #Holocene #Hydrocarbon exploration and reservoir analysis #Methane Hydrates and Related Phenomena #Oceanography #Physical geography #Scale (ratio)

paper · doi:10.1038/nature13799

published in Nature 514(7524), 616-619 (Nature Portfolio)

openalex publication_date 2014/10/28 · crossref created 2014/10/28 · crossref issued 2014/10/29 · crossref published 2014/10/29 · crossref published-online 2014/10/29 · crossref published-print 2014/10/30 · crossref deposited 2024/06/04 · openalex created_date 2025/10/10 · crossref indexed 2026/07/23 · openalex updated_date 2026/07/29

Citations

• Midlatitude westerlies, atmospheric CO2, and climate change during the ice ages
• Onset of deglacial warming in West Antarctica driven by local orbital forcing
• Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes
• An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka
• Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation

Cited by

• The WAIS Divide deep ice core WD2014 chronology – Part 1: Methane synchronization (68–31 ka BP) and the gas age–ice age difference
• The WAIS Divide deep ice core WD2014 chronology – Part 2: Annual-layer counting (0–31 ka BP)
• Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise
• Radiocarbon: A key tracer for studying Earth’s dynamo, climate system, carbon cycle, and Sun
• Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 °C global warming is highly dangerous
• Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation
• Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion
• Antarctic temperature and CO 2 : near-synchrony yet variable phasing during the last deglaciation
• A Horizontal Ice Core From Taylor Glacier, Its Implications for Antarctic Climate History, and an Improved Taylor Dome Ice Core Time Scale
• Consequences of twenty-first-century policy for multi-millennial climate and sea-level change
• WAIS Divide [wikipedia]