@article{discovery10081633,
           title = {Consistently dated Atlantic sediment cores over the last 40 thousand years},
            year = {2019},
          volume = {6},
           month = {September},
         journal = {Scientific Data},
            note = {This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.},
            issn = {2052-4463},
             url = {https://doi.org/10.1038/s41597-019-0173-8},
        abstract = {Rapid changes in ocean circulation and climate have been observed in marine-sediment and
ice cores over the last glacial period and deglaciation, highlighting the non-linear character
of the climate system and underlining the possibility of rapid climate shifts in response to
anthropogenic greenhouse gas forcing. To date, these rapid changes in climate and ocean
circulation are still not fully explained. One obstacle hindering progress in our understanding
of the interactions between past ocean circulation and climate changes is the difculty of
accurately dating marine cores. Here, we present a set of 92 marine sediment cores from the
Atlantic Ocean for which we have established age-depth models that are consistent with the
Greenland GICC05 ice core chronology, and computed the associated dating uncertainties,
using a new deposition modeling technique. This is the frst set of consistently dated marine
sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation
and climate changes over vast regions of the Atlantic Ocean. Moreover, this data set is of
direct use in paleoclimate modeling studies.},
          author = {Waelbroeck, C and Lougheed, BC and Vazquez Riveiros, N and Missiaen, L and Pedro, J and Dokken, T and Hajdas, I and Wacker, L and Abbott, P and Dumoulin, J-P and Thil, F and Eynaud, F and Rossignol, L and Fersi, W and Albuquerque, AL and Arz, H and Austin, WEN and Came, R and Carlson, AE and Collins, JA and Dennielou, B and Desprat, S and Dickson, A and Elliot, M and Farmer, C and Giraudeau, J and Gottschalk, J and Henderiks, J and Hughen, K and Jung, S and Knutz, P and Lebreiro, S and Lund, DC and Lynch-Stieglitz, J and Malaiz{\'e}, B and Marchitto, T and Mart{\'i}nez-M{\'e}ndez, G and Mollenhauer, G and Naughton, F and Nave, S and N{\"u}rnberg, D and Oppo, D and Peck, V and Peeters, FJC and Penaud, A and Portilho-Ramos, RDC and Repschl{\"a}ger, J and Roberts, J and R{\"u}hlemann, C and Salgueiro, E and Sanchez Goni, MF and Sch{\"o}nfeld, J and Scussolini, P and Skinner, LC and Skonieczny, C and Thornalley, D and Toucanne, S and Rooij, DV and Vidal, L and Voelker, AHL and Wary, M and Weldeab, S and Ziegler, M}
}