Fig. 4: Meridional distribution of tproj across the Drake Passage during the late, middle and early Holocene.
From: Radiocarbon evidence for the stability of polar ocean overturning during the Holocene

a–c, Meridional distribution of tproj (years) across the Drake Passage during the late (a), middle (b) and early Holocene (c). Multiple age numbers along a single symbol indicate multiple samples from the same location during each period. The white lines in a illustrate the modern neutral density anomalies (GLODAPv2.2019; ref. 49). Lighter background colour illustrates a younger ventilation age. The black dashed arrow indicates the inferred southward migration of the polar front (PF) in the early Holocene. The light blue area at the top of c denotes transiently enhanced mixing of the 14C-enriched signatures from the surface ocean in the early Holocene, probably associated with southward polar front migration and enhanced air–sea gas exchange.