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Raymo, Maureen E (1997): Stable oxygen isotopes of late Quaternary sediments [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.869100, Supplement to: Raymo, ME (1997): The timing of major climate terminations. Paleoceanography, 12(4), 577-585, https://doi.org/10.1029/97PA01169

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Abstract:
A simple, untuned "constant sedimentation rate" timescale developed using three radiometric age constraints and eleven d18O records longer than 0.8 Myr provides strong support for the validity of the SPECMAP timescale of the late Quaternary (Imbrie et al., 1984). In particular, the present study independently confirms the link between major deglaciations (terminations) and increases in northern hemisphere summer radiation at high latitudes and shows that this correlation is not an artifact of orbital tuning. In addition, the excess ice characteristic of late Quaternary "100-kyr" climate cycles typically accumulates when July insolation at 65°N has been unusually low for more than a full precessional cycle, or >21 kyr, and once established does not last beyond the next increase in summer insolation. Thus, the timing of the growth and decay of large 100-kyr ice sheets, as depicted in the deep sea d18O record, is strongly (and semipredictably) influenced by eccentricity through its modulation of the orbital precession component of northern hemisphere summer insolation.
Further details:
Bassinot, Franck C; Beaufort, Luc; Vincent, Edith; Labeyrie, Laurent D; Rostek, Frauke; Müller, Peter J; Quidelleur, Xavier; Lancelot, Yves (1994): Stable isotope ratios and CaCO3 content of sediment core MD90-963. PANGAEA, https://doi.org/10.1594/PANGAEA.869096
deMenocal, Peter B (1993): Stable isotopes, CaCO3, opal and terrigeneous of ODP Site 108-663 (Table A1). PANGAEA, https://doi.org/10.1594/PANGAEA.208129
Mix, Alan C; Le, Jianning; Shackleton, Nicholas J (1995): (Appendix A) Stable carbon and oxygen isotope ratios of benthic foraminifera from ODP Site 138-846 in the tropical Pacific Ocean. PANGAEA, https://doi.org/10.1594/PANGAEA.60252
Mix, Alan C; Pisias, Nicklas G; Rugh, W D; Wilson, June; Morey, Ann E; Hagelberg, Teresa King (1995): (Appendix A) Stable carbon and oxygen isotope ratios of benthic foraminifera from ODP Site 138-849 on the East Pacifi Rise. PANGAEA, https://doi.org/10.1594/PANGAEA.60255
Raymo, Maureen E; Oppo, Delia W; Curry, William B (1997): Adjusted stable isotope ratios from ODP Site 108-664 in the equatorial Atlantic. PANGAEA, https://doi.org/10.1594/PANGAEA.53160
Ruddiman, William F; Raymo, Maureen E; Martinson, Douglas G; Clement, Bradford M; Backman, Jan (1989): (Table A4) Stacked stable isotope record of sediment cores from the North Atlantic. PANGAEA, https://doi.org/10.1594/PANGAEA.701202
Shackleton, Nicholas J; Opdyke, Neil D (1997): Stable oxygen isotope composition of planktonic foraminifer G. sacculifer in sediment core V28-239. PANGAEA, https://doi.org/10.1594/PANGAEA.52020
Tiedemann, Ralf; Sarnthein, Michael; Shackleton, Nicholas J (1994): Stable oxygen isotope ratios of Cibicidoides wuellerstorfi from ODP Hole 108-659A in the North Atlantic. PANGAEA, https://doi.org/10.1594/PANGAEA.52517
Project(s):
Coverage:
Median Latitude: 2.954008 * Median Longitude: -87.708854 * South-bound Latitude: -3.095000 * West-bound Longitude: 159.361000 * North-bound Latitude: 41.001200 * East-bound Longitude: -2.325566
Date/Time Start: 1971-05-09T00:00:00 * Date/Time End: 1994-02-14T00:00:00
Size:
5 datasets

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Datasets listed in this publication series

  1. Raymo, ME (1997): Stable isotope ratios opf ODP Site 108-664. https://doi.org/10.1594/PANGAEA.869097
  2. Raymo, ME (1997): Stable isotope ratios opf ODP Site 111-677. https://doi.org/10.1594/PANGAEA.869098
  3. Raymo, ME (1997): Stable isotope ratios opf ODP Site 130-806. https://doi.org/10.1594/PANGAEA.869099
  4. Raymo, ME (1997): Stable isotope ratios opf ODP Site 154-925. https://doi.org/10.1594/PANGAEA.869101
  5. Raymo, ME (1997): (Table 2) Termination depths and age estimations of various sediments cores. https://doi.org/10.1594/PANGAEA.869102