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- W1844673023 abstract "Late Quaternary Versus Minimum Ice GeoB 1016 SST Angola margin 0.76 0.64 28 ± 20 3.2 ± 2.3 E45-29/E49-18 SST South Indian fronts 0.86 0.65 27 ± 15 3.1 ± 1.7 PS2082-1 SST South Atlantic fronts 0.92 0.73 18 ± 12 2.1 ± 1.4 PS2489-2 SSST South Atlantic fronts 0.82 0.80 13 ± 15 1.5 ± 1.7 ETP describes summed orbital variance following the convention by Imbrie et al. [1989] using the data of Berger and Loutre [1991]. ODP 1090 SSST data are from Becquey and Gersonde [2002], data of ODP 677 dO are from Shackleton et al. [1990], data of DSDP 607 dC are from Ruddiman et al. [1989] with the stratigraphy of Raymo et al. [1997]. Results for the late Quaternary are taken from the literature. Data of GeoB 1016 (11 460S, 11 410E) are from Schneider et al. [1995], data for E45-29 (44 530S, 106 310E) and E49-18 (46 030S, 90 100E) are from Howard and Prell [1992], PS2082-1 (43 130S, 11 440E) data are from Brathauer and Abelmann [1999], and PS2489-2 (42 520S, 8 580E) data are from Becquey and Gersonde [2003]. All late Quaternary records are crossed with the inverse SPECMAP record [Imbrie et al., 1984], except for PS2489-2 SSST, which is crossed with benthic foraminiferal dO of that core [Becquey and Gersonde, 2003]. A negative phase lag represents a lead. PALEOCEANOGRAPHY, VOL. 20, PA1019, doi:10.1029/2005PA001134, 2005" @default.
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- W1844673023 date "2005-03-01" @default.
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- W1844673023 title "Correction to “Forcing of tropical Atlantic sea surface temperatures during the mid-Pleistocene transition”" @default.
- W1844673023 doi "https://doi.org/10.1029/2005pa001134" @default.
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