@misc{arz2007rdoi, author={Helge Wolfgang {Arz} and Frank {Lamy} and Andrey {Ganopolski} and Norbert R {Nowaczyk} and J\"{u}rgen {P\"{a}tzold}}, title={{Radiocarbon dating, oxygen isotopes, and sea-level reconstruction of sediment core GeoB5844-2 from the northern end of the Red Sea}}, year={2007}, doi={10.1594/PANGAEA.797464}, url={https://doi.org/10.1594/PANGAEA.797464}, note={Supplement to: Arz, HW et al. (2007): Dominant Northern Hemisphere climate control over millennial-scale glacial sea-level variability. Quaternary Science Reviews, 26(3-4), 312-321, https://doi.org/10.1016/j.quascirev.2006.07.016}, abstract={Based on a radiocarbon and paleomagnetically dated sediment record from the northern Red Sea and the exceptional sensitivity of the regional changes in the oxygen isotope composition of sea water to the sea-level-dependent water exchange with the Indian Ocean, we provide a new global sea-level reconstruction spanning the last glacial period. The sea-level record has been extracted from the temperature-corrected benthic stable oxygen isotopes using coral-based sea-level data as constraints for the sea-level/oxygen isotope relationship. Although, the general features of this millennial-scale sea-level records have strong similarities to the rather symmetric and gradual Southern Hemisphere climate patterns, we observe, in constrast to previous findings, pronounced sea level rises of up to 25 m to generally correspond with Northern Hemisphere warmings as recorded in Greenland ice-core interstadial intervals whereas sea-level lowstands mostly occur during cold phases. Corroborated by CLIMBER-2 model results, the close connection of millennial-scale sea-level changes to Northern Hemisphere temperature variations indicates a primary climatic control on the mass balance of the major Northern Hemisphere ice sheets and does not require a considerable Antarctic contribution.}, type={data set}, publisher={PANGAEA} }