Local and regional trends in Plio-Pleistocene delta super(18)O records from benthic foraminifera

We present new orbital-resolution Pliocene-Pleistocene benthic stable oxygen isotope ( delta super(18)O sub(b)) records from Ocean Drilling Program Sites 1264 and 1267, from Walvis Ridge in the Southeast Atlantic. We compare long-term (>250 kyr) interbasin delta super(18)O sub(b)-gradi ents between Pacific and North Atlantic regional stacks, as well as intra and interbasin gradients from the perspective of Walvis Ridge. The delta super(18)O sub(b) values from Sites 1264 and 1267 are almost always higher than deep North Atlantic and Pacific sites, with large gradients (>0.5ppt) emerging abruptly at 2.4 Ma and persisting until 1.3 Ma. From this, we infer the presence of a new water mass, which resulted from the influence of dense, super(18)O-enriched Nordic sea overflow waters via the abyssal East Atlantic. Meanwhile, long-term average delta super(18)O sub(b) values in the North Atlantic appear to have remained within 0-0.25ppt lower than in the Pacific. However, the magnitude of this difference is sensitive to the inclusion of records from the equatorial West Atlantic. These results, together with constraints based on temperature, salinity, and density, suggest an influence of the seawater delta super(18)O ( delta super(18)O sub(SW)) versus salinity relationship of source waters on delta super(18)O sub(b) values within the Atlantic. In particular, the abrupt emergence at 2.4 Ma of higher delta super(18)O sub(b) values at Sites 1264 and 1267, relative to North Atlantic records, appears to require a low-latitude surface water delta super(18)O sub(SW) signal. This implies a connection between northward heat transport and deep water export into the abyssal East Atlantic. Hence, our results have implications for the interpretation of delta super(18)O sub(b) records and highlight the potential for delta super(18)O sub(b) to constrain deep Atlantic water mass sources and pathways during the Plio-Pleistocene. Key Points * We present two new Pliocene-Pleistocene benthic stable oxygen isotope records * Large intra-Atlantic oxygen isotope gradients are documented * We infer new NADW component with a low-latitude surface water signal