The Early–Middle Pleistocene Transition in the Gulf of Cadiz (NE Atlantic) – an interplay between subtropical gyre and extremely cold surface waters
- Figure 2 shows the % G. truncatulinoides distribution in the North Atlantic, in support to the related text added in the "Material and methods" section.
- Figure 4 reveals the differences between the age models used in this paper and the previously published Bajo et al. (2020) speleothem ages; as discussed in the "Results" section on the chronostratigraphy.
Data sets
Oxygen isotope of planktic foraminifera Globigerina bulloides from IODP Site 339-U1387 https://doi.org/10.1594/PANGAEA.914401
SST and synchronized ages from IODP Site 339-U1387 https://doi.org/10.1594/PANGAEA.914400
Planktonic foraminifera faunal data and sea-surface temperatures for the Marine Isotope Stage (MIS) 18 to MIS 28 interval of IODP Site 339-U1387 https://doi.org/10.1594/PANGAEA.974451
Temperature reconstruction for the Mid-Pleistocene Transition based on deep-dwelling foraminifera of IODP Site339-U1385 https://doi.org/10.1594/PANGAEA.882374
Oxgyen and carbon isotope data for the planktonic foraminifera Globigerina bulloides at IODP Site 339-U1385 https://doi.org/10.1594/PANGAEA.951386
A 1 Ma record of Sea Surface Temperature and extreme cooling events in the North Atlantic: A perspective from the Iberian Margin https://doi.org/10.1594/PANGAEA.921577
Planktonic foraminifera faunal data and sea-surface temperatures for the Marine Isotope Stage (MIS) 18 to MIS 28 interval of IODP Site 339-U1387 https://doi.org/10.1594/PANGAEA.974451
Model code and software
Ocean Data View https://odv.awi.de/