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Waelbroeck, Claire; Lougheed, Bryan C; Vázquez Riveiros, Natalia; Missiaen, Lise; Pedro, Joel B; Dokken, Trond; Hajdas, Irka; Wacker, Lukas; Abbott, Peter M; Dumoulin, Jean-Pascal; Thil, François; Eynaud, Frédérique; Rossignol, Linda; Fersi, Wiem; Albuquerque, Ana Luiza Spadano; Arz, Helge Wolfgang; Austin, William EN; Came, Rosemarie E; Carlson, Anders Eskil; Collins, James A; Dennielou, Bernard; Desprat, Stéphanie; Dickson, Alex; Elliot, Mary; Farmer, Christa; Giraudeau, Jacques; Gottschalk, Julia; Henderiks, Jorijntje; Hughen, Konrad A; Jung, Simon; Knutz, Paul Cornils; Lebreiro, Susana Martin; Lund, David C; Lynch-Stieglitz, Jean; Malaizé, Bruno; Marchitto, Thomas M; Martínez Méndez, Gema; Mollenhauer, Gesine; Naughton, Filipa; Nave, Silvia Osorio; Nürnberg, Dirk; Oppo, Delia W; Peck, Victoria L; Peeters, Frank J C; Penaud, Aurélie; Portilho-Ramos, Rodrigo Costa; Repschläger, Janne; Roberts, Jenny; Rühlemann, Carsten; Salgueiro, Emilia; Sanchez Goñi, Maria Fernanda; Schönfeld, Joachim; Scussolini, Paolo; Skinner, Luke C; Skonieczny, Charlotte; Thornalley, David J R; Toucanne, Samuel; Van Rooij, David; Vidal, Laurence; Voelker, Antje H L; Wary, Mélanie; Weldeab, Syee; Ziegler, Martin (2019): A summary of consistently dated Atlantic sediment cores over the last 40 thousand years. PANGAEA, https://doi.org/10.1594/PANGAEA.899490, In: Waelbroeck, C et al. (2019): Consistently dated Atlantic sediment cores. PANGAEA, https://doi.org/10.1594/PANGAEA.900073

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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 difficulty 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 first 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.
Keyword(s):
Atlantic sediment cores; consistent dating; last 40 ky
Further details:
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Coverage:
Median Latitude: 21.456630 * Median Longitude: -25.634783 * South-bound Latitude: -53.010000 * West-bound Longitude: -87.120000 * North-bound Latitude: 67.870000 * East-bound Longitude: 29.240000
Date/Time Start: 1971-12-03T00:00:00 * Date/Time End: 2012-03-08T16:07:00
Minimum ALTITUDE: -5010 m * Maximum ALTITUDE: -426 m
Event(s):
94-609 * Latitude: 49.877800 * Longitude: -24.238200 * Date/Time: 1983-07-22T00:00:00 * Elevation: -3884.0 m * Penetration: 399.4 m * Recovery: 301.4 m * Location: North Atlantic/FLANK * Campaign: Leg94 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 40 cores; 380.2 m cored; 19.2 m drilled; 79.3 % recovery
162-983 * Latitude: 60.403500 * Longitude: -23.640667 * Date/Time Start: 1995-07-21T00:00:00 * Date/Time End: 1995-07-24T00:00:00 * Elevation: -1983.7 m * Penetration: 766.5 m * Recovery: 798 m * Location: South Atlantic Ocean * Campaign: Leg162 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 82 cores; 766.5 m cored; 0 m drilled; 104.1% recovery
165-1002 * Latitude: 10.706100 * Longitude: -65.169617 * Date/Time Start: 1996-02-18T00:00:00 * Date/Time End: 1996-02-20T00:00:00 * Elevation: -892.9 m * Penetration: 516.6 m * Recovery: 529.3 m * Location: Cayman Rise, Caribbean Sea * Campaign: Leg165 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 57 cores; 516.6 m cored; 0 m drilled; 102.5% recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventWaelbroeck, Claire
2CoreCoreWaelbroeck, Claire
3LATITUDELatitudeWaelbroeck, ClaireGeocode
4LONGITUDELongitudeWaelbroeck, ClaireGeocode
5ALTITUDEAltitudemWaelbroeck, ClaireGeocode – depth
6CommentCommentWaelbroeck, ClaireBased on deep sea coral data given in Roberts et al., 2016
7Method commentMethod commWaelbroeck, ClaireEntirely AMS-based
8Method commentMethod commWaelbroeck, ClaireSST alignment to NGRIP
9Method commentMethod commWaelbroeck, ClaireMS aligment to NGRIP
10Method commentMethod commWaelbroeck, ClaireSST alignment to EDML
11Method commentMethod commWaelbroeck, ClaireCombined AMS + SST alignment to NGRIP
12Method commentMethod commWaelbroeck, ClaireCombined AMS + alignment to speleothems
13Method commentMethod commWaelbroeck, ClaireUse of tephra chronological markers
14Persistent IdentifierPersistent IdentifierWaelbroeck, ClaireAge-depth model
15Uniform resource locator/link to graphicURL graphicWaelbroeck, ClaireAge model input
16Uniform resource locator/link to graphicURL graphicWaelbroeck, ClaireAge model
17Reference/sourceReferenceWaelbroeck, Claire
Size:
563 data points

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