Author Correction: Evidence for oxygen-conserving diamond formation in redox-buffered subducted oceanic crust sampled as eclogite

Key Points

• Diamond formation occurs under specific conditions within subducted oceanic crust, indicating unique geochemical processes.
• Eclogite samples demonstrate evidence of oxygen-conserving diamond formation, highlighting the role of redox conditions.
• The observational analysis focuses on redox-buffered environments, revealing significant mineralogical transformations.
• This work emphasizes the necessity of reevaluating known geochemical models associated with subduction processes.