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 · 5 citations
Earth and Planetary Sciences · Engineering · Environmental Science · #Geology and Paleoclimatology Research #Hydrocarbon exploration and reservoir analysis #Methane Hydrates and Related Phenomena

paper · doi:10.1038/nature13799

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

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
• WAIS Divide [wikipedia]