@misc{lippold2009utap, author={J\"{o}rg {Lippold} and Jens {Gruetzner} and Diane M {Winter} and Yann {Lahaye} and Augusto {Mangini} and Marcus {Christl}}, title={{Uranium, Thorium and Protactinium isotopes of ODP Site 172-1063}}, year={2009}, doi={10.1594/PANGAEA.763199}, url={https://doi.org/10.1594/PANGAEA.763199}, note={Supplement to: Lippold, J et al. (2009): Does sedimentary 231Pa/230Th from the Bermuda Rise monitor past Atlantic Meridional Overtuning Circulation? Geophysical Research Letters, 36, L12601, https://doi.org/10.1029/2009GL038068}, abstract={Ocean circulation may have undergone reductions and reinvigorations in the past closely tied to regional climate changes. Measurements of 231Pa/230Th ratios in a sediment core from the Bermuda Rise have been interpreted as evidence that the Atlantic Meridional Overturning Circulation (AMOC) was weakened or completely eliminated during a period of catastrophic iceberg discharges (Heinrich-Event 1, H1). Here we present new data from the Bermuda Rise that show further 231Pa/230Th peaks during Heinrich-2 (H2) and Heinrich-3 (H3). Additionally, a tight correlation between diatom abundances (biogenic silica) and 231Pa/230Th is discovered in this core. Our results redirect the interpretation of 231Pa/230Th from the Bermuda Rise as a proxy for ocean circulation towards a proxy that reacts highly sensitive to changes of particle composition and water mass properties.}, type={data set}, publisher={PANGAEA} }