Bassinot, Franck C; Labeyrie, Laurent D; Vincent, Edith; Quidelleur, Xavier; Shackleton, Nicholas J; Lancelot, Yves (1994): A low-latitude Upper Pleistocene oxygen isotope stack. PANGAEA, https://doi.org/10.1594/PANGAEA.715006, Supplement to: Bassinot, FC et al. (1994): The astronomical theory of climate and the age of the Brunhes-Matuyama magnetic reversal. Earth and Planetary Science Letters, 126(1-3), 91-108, https://doi.org/10.1016/0012-821X(94)90244-5
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Below oxygen isotope stage 16, the orbitally derived time-scale developed by Shackleton et al. (1990) from ODP site 677 in the equatorial Pacific differs significantly from previous ones (e.g. Kominz and Pisias, 1979 doi:10.1126/science.204.4389.171; Morley and Hays, 1981 doi:10.1016/0012-821X(81)90034-0, Imbrie et al. 1984), yielding estimated ages for the last Earth magnetic reversals that are 5-7% older than the K/Ar values (Mankinen and Dalrymple, 1979 doi:10.1029/JB084iB02p00615; Berggren et al., 1985; Harland and Armstrong, 1989) but are in good agreement with recent Ar/Ar dating (Baksi et al., 1991; 1992 doi:10.1126/science.256.5055.356; Spell and McDougall, 1992 doi:10.1029/92GL01125). These results suggest that in the lower Brunhes and upper Matuyama chronozones most deep-sea climatic records retrieved so far apparently missed or misinterpreted several oscillations predicted by the astronomical theory of climate. To test this hypothesis, we studied a high-resolution oxygen isotope record from giant piston core MD900963 (Maldives area, tropical Indian Ocean) in which precession-related oscillations in delta18O are particularly well expressed, owing to the superimposition of a local salinity signal on the global ice volume signal (Rostek et al., 1993 doi:10.1038/364319a0). Three additional precession-related cycles are observed in oxygen isotope stages 17 and 18 of core MD900963, compared to the SPECMAP composite curves (Imbrie et al., 1984; Prell et al., 1986 doi:10.1029/PA001i002p00137), and stage 21 clearly presents three precession oscillations, as predicted by Shackleton et al. (1990). The precession peaks found in the delta18O record from core MD900963 are in excellent agreement with climatic oscillations predicted by the astronomical theory of climate. Our delta18O record therefore permits the development of an accurate astronomical time-scale. Based on our age model, the Brunhes-Matuyama reversal is dated at 775 +/- 10 ka, in good agreement with the age estimate of 780 ka obtained by Shackleton et al. (1990) and recent radiochronological Ar/Ar datings on lavas (Baksi et al., 1991; 1992; Spell and McDougall, 1992). We developed a new low-latitude, Upper Pleistocene delta18O reference record by stacking and tuning the delta18O records from core MD900963 and site 677 to orbital forcing functions.
Latitude: 5.040000 * Longitude: 73.530000
Date/Time Start: 1990-09-12T00:00:00 * Date/Time End: 1990-09-12T00:00:00
Datasets listed in this Collection
- Bassinot, FC; Labeyrie, LD; Vincent, E et al. (1994): (Table 1) Age model of sediment core MD90-963. https://doi.org/10.1594/PANGAEA.60025
- Bassinot, FC; Labeyrie, LD; Vincent, E et al. (1994): (Table 2) Stable oxygen isotope ratios of Globigerinoides ruber white of sediment core MD90-963. https://doi.org/10.1594/PANGAEA.60026
- Bassinot, FC; Labeyrie, LD; Vincent, E et al. (1994): (Table 3) Stable oxygen isotope stack. https://doi.org/10.1594/PANGAEA.60027
- Bassinot, FC; Labeyrie, LD; Vincent, E et al. (1994): (Table 4) Isotopic event stack. https://doi.org/10.1594/PANGAEA.60028