Author Correction: Relatively warm deep-water formation persisted in the Last Glacial Maximum

Key Points

• Warm deep-water formation occurred during the Last Glacial Maximum, suggesting unexpected climatic phenomena.
• This correction emphasizes the role of ocean circulation in climate during glacial periods, with implications for understanding climate patterns.
• Observational analysis of sediment cores revealed insights into past ocean temperatures and conditions during the Last Glacial Maximum.
• Highlights potential gaps in previous climate models, indicating the need for further research on glacial climate dynamics.