%0 Journal Article
%@ 2052-4463
%A Waelbroeck, C
%A Lougheed, BC
%A Vazquez Riveiros, N
%A Missiaen, L
%A Pedro, J
%A Dokken, T
%A Hajdas, I
%A Wacker, L
%A Abbott, P
%A Dumoulin, J-P
%A Thil, F
%A Eynaud, F
%A Rossignol, L
%A Fersi, W
%A Albuquerque, AL
%A Arz, H
%A Austin, WEN
%A Came, R
%A Carlson, AE
%A Collins, JA
%A Dennielou, B
%A Desprat, S
%A Dickson, A
%A Elliot, M
%A Farmer, C
%A Giraudeau, J
%A Gottschalk, J
%A Henderiks, J
%A Hughen, K
%A Jung, S
%A Knutz, P
%A Lebreiro, S
%A Lund, DC
%A Lynch-Stieglitz, J
%A Malaizé, B
%A Marchitto, T
%A Martínez-Méndez, G
%A Mollenhauer, G
%A Naughton, F
%A Nave, S
%A Nürnberg, D
%A Oppo, D
%A Peck, V
%A Peeters, FJC
%A Penaud, A
%A Portilho-Ramos, RDC
%A Repschläger, J
%A Roberts, J
%A Rühlemann, C
%A Salgueiro, E
%A Sanchez Goni, MF
%A Schönfeld, J
%A Scussolini, P
%A Skinner, LC
%A Skonieczny, C
%A Thornalley, D
%A Toucanne, S
%A Rooij, DV
%A Vidal, L
%A Voelker, AHL
%A Wary, M
%A Weldeab, S
%A Ziegler, M
%D 2019
%F discovery:10081633
%J Scientific Data
%T Consistently dated Atlantic sediment cores over the last 40 thousand years
%U https://discovery.ucl.ac.uk/id/eprint/10081633/
%V 6
%X 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.
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