Seasonal origin of the thermal maxima at the Holocene and the last interglacial

2021/01/27 by Samantha C. Bova, Samantha Bova, Yair Rosenthal +3 · 1 voice · 2 citations
Earth and Planetary Sciences · Environmental Science · #Cryospheric studies and observations #Geology and Paleoclimatology Research #Methane Hydrates and Related Phenomena

paper · doi:10.1038/s41586-020-03155-x

crossref issued 2021/01/27 · crossref published 2021/01/27 · crossref published-online 2021/01/27 · openalex publication_date 2021/01/27 · crossref created 2021/01/27 · crossref published-print 2021/01/28 · crossref deposited 2022/07/29 · openalex created_date 2025/10/10 · crossref indexed 2026/06/19 · openalex updated_date 2026/07/29

Citations

• Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series
• Long-Term Variations of Daily Insolation and Quaternary Climatic Changes
• On the Structure and Origin of Major Glaciation Cycles 1. Linear Responses to Milankovitch Forcing
• IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP
• IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0–50,000 Years cal BP

Cited by

• Globally resolved surface temperatures since the Last Glacial Maximum
• Accelerating the Renewable Energy Revolution to Get Back to the Holocene

Discussions

• Speaking of Bova et al. (2021 doi.org/10.1038/s415...), their study received two independent comments with accompanying authors’ replies (Zhang & Chen, 2021 doi.org/10.1038/s415..., reply doi.org/10.1 [bsky, 1 points, 1 comments]