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  • 306-U1313; AGE; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Exp306; Globorotalia inflata, δ13C; Globorotalia inflata, δ18O; Integrated Ocean Drilling Program / International Ocean Discovery Program; Intercore correlation; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 252; North Atlantic Climate 2; Sample code/label  (2)
  • 306-U1313; CALYPSO; Calypso Corer; COMPCORE; Composite Core; Exp306; GEOSCIENCES, MARMARCORE; Iberian slope; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Marion Dufresne (1995); MD01-2446; MD03-2699; MD123; MD134; North Atlantic Climate 2; PICABIA  (1)
  • AAIW  (1)
  • Oxygen isotope
  • 2010-2014  (5)
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  • 1
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 25 (2010): PA4101, doi:10.1029/2010PA001962.
    Description: Paleoceanographic studies using benthic foraminiferal Cd as a nutrient tracer have provided a robust means of reconstructing glacial Atlantic Ocean water mass geometry, but a paucity of data from the South Atlantic above 1200 m has limited investigation of Antarctic Intermediate Water (AAIW) configuration and formation. A new Cd depth profile from Brazil margin sediments suggests that AAIW penetrated northward at 1100 m to at least 27°S in the glacial Atlantic. It exhibited substantially reduced δ13Cas values, confirming preliminary evidence that this AAIW was unique to the glacial Atlantic and that it formed differently than today, with less atmospheric contact.
    Keywords: Cadmium ; Last glacial maximum ; Atlantic Ocean ; AAIW
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 37 (2010): L23603, doi:10.1029/2010GL045202.
    Description: Ice core records of polar temperatures and greenhouse gases document abrupt millennial-scale oscillations that suggest the reduction or shutdown of thermohaline Circulation (THC) in the North Atlantic Ocean may induce the abrupt cooling in the northern hemisphere. It remains unknown, however, whether the sea surface temperature (SST) is cooling or warming in the Kuroshio of the Northwestern Pacific during the cooling event. Here we present an AMS 14C-dated foraminiferal Mg/Ca SST record from the central Okinawa Trough and document that the SST variations exhibit two steps of warming since 21 ka — at 14.7 ka and 12.8 ka, and a cooling (∼1.5°C) during the interval of the Younger Dryas. By contrast, we observed no SST change or oceanic warming (∼1.5–2°C) during the episodes of Northern Hemisphere cooling between ∼21–40 ka. We therefore suggest that the “Antarctic-like” timing and amplitude of millennial-scale SST variations in the subtropical Northwestern Pacific between 20–40 ka may have been determined by rapid ocean adjustment processes in response to abrupt wind stress and meridional temperature gradient changes in the North Pacific.
    Description: This research was funded by the National Science Council (NSC), Taiwan to M.T.C. (NSC96‐2611‐M‐019‐008 and NSC96‐2611‐M‐019‐009) and C.C.S. (NSC98‐2611‐M002‐006). X.P.L. was supported by the Natural Science Foundation of China (40930844 and 40706006), China’s National Basic Research Priorities Programmer (2005CB422303 and 2007CB411804), 111 Project (B07036), and the Program for New Century Excellent Talents in University (NECT‐07‐0781).
    Keywords: Kuroshio ; Pacific ; Sea surface temperature ; Mg/Ca ; Oxygen isotope ; East Asian monsoon
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: text/plain
    Format: application/pdf
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  • 3
    Publication Date: 2024-03-02
    Keywords: 306-U1313; AGE; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Exp306; Globorotalia inflata, δ13C; Globorotalia inflata, δ18O; Integrated Ocean Drilling Program / International Ocean Discovery Program; Intercore correlation; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 252; North Atlantic Climate 2; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 2712 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Voelker, Antje H L; Rodrigues, Teresa; Billups, Katharina; Oppo, Delia W; McManus, Jerry F; Stein, Ruediger; Hefter, Jens; Grimalt, Joan O (2010): Variations in mid-latitude North Atlantic surface water properties during the mid-Brunhes (MIS 9-14) and their implications for the thermohaline circulation. Climate of the Past, 6(4), 531-552, https://doi.org/10.5194/cp-6-531-2010
    Publication Date: 2024-03-02
    Description: Stable isotope and ice-rafted debris records from three core sites in the mid-latitude North Atlantic (IODP Site U1313, MD01-2446, MD03-2699) are combined with records of ODP Sites 1056/1058 and 980 to reconstruct hydrographic conditions during the middle Pleistocene spanning Marine Isotope Stages (MIS) 9-14 (300-540 ka). Core MD03-2699 is the first high-resolution mid-Brunhes record from the North Atlantic's eastern boundary upwelling system covering the complete MIS 11c interval and MIS 13. The array of sites reflect western and eastern basin boundary current as well as north to south transect sampling of subpolar and transitional water masses and allow the reconstruction of transport pathways in the upper limb of the North Atlantic's circulation. Hydrographic conditions in the surface and deep ocean during peak interglacial MIS 9 and 11 were similar among all the sites with relative stable conditions and confirm prolonged warmth during MIS 11c also for the mid-latitudes. Sea surface temperature (SST) reconstructions further reveal that in the mid-latitude North Atlantic MIS 11c is associated with two plateaus, the younger one of which is slightly warmer. Enhanced subsurface northward heat transport in the eastern boundary current system, especially during early MIS 11c, is denoted by the presence of tropical planktic foraminifer species and raises the question how strongly it impacted the Portuguese upwelling system. Deep water ventilation at the onset of MIS 11c significantly preceded surface water ventilation. Although MIS 13 was generally colder and more variable than the younger interglacials the surface water circulation scheme was the same. The greatest differences between the sites existed during the glacial inceptions and glacials. Then a north - south trending hydrographic front separated the nearshore and offshore waters off Portugal. While offshore waters originated from the North Atlantic Current as indicated by the similarities between the records of IODP Site U1313, ODP Site 980 and MD01-2446, nearshore waters as recorded in core MD03-2699 derived from the Azores Current and thus the subtropical gyre. Except for MIS 12, Azores Current influence seems to be related to eastern boundary system dynamics and not to changes in the Atlantic overturning circulation.
    Keywords: 306-U1313; CALYPSO; Calypso Corer; COMPCORE; Composite Core; Exp306; GEOSCIENCES, MARMARCORE; Iberian slope; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Marion Dufresne (1995); MD01-2446; MD03-2699; MD123; MD134; North Atlantic Climate 2; PICABIA
    Type: Dataset
    Format: application/zip, 12 datasets
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  • 5
    Publication Date: 2024-03-02
    Keywords: 306-U1313; AGE; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Exp306; Globorotalia inflata, δ13C; Globorotalia inflata, δ18O; Integrated Ocean Drilling Program / International Ocean Discovery Program; Intercore correlation; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 252; North Atlantic Climate 2; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 2712 data points
    Location Call Number Expected Availability
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