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  • Alley, R. B. (2003), Raising paleoceanography, Paleoceanography, 18(4), 1085, doi:10.1029/2003PA000942.
  • Andersson, C., D. A. Warnke, J. E. T. Channell, J. Stoner, and E. Jansen (2002), The mid-Pliocene (4.2–2.6 Ma) benthic stable isotope record of the Southern Ocean: ODP Sites 1092 and 704, Meteor Rise, Palaeogeogr. Palaeoclimatol. Palaeoecol., 182, 165181.
  • Bard, E., B. Hamelin, and R. G. Fairbanks (1990), U-Th ages obtained by mass spectrometry in corals from Barbados: Sea level during the past 130,000 years, Nature, 346, 456458.
  • Bassinot, F. C., L. D. Labeyrie, E. Vincent, X. Quidelleur, N. J. Shackleton, and Y. Lancelot (1994), The astronomical theory of climate and the age of the Brunhes-Matuyama magnetic reversal, Earth Planet. Sci. Lett., 126, 91108.
  • Berger, W. H., and M. F. Loutre (1991), Insolation values for the climate of the last 10 m. y. Quat. Sci. Rev., 10, 297317.
  • Berger, W. H., T. Bickert, H. Schmidt, and G. Wefer (1993), Quaternary oxygen isotope record of pelagic foraminifers: Site 806, Ontong Java Plateau, Proc. Ocean Drill. Program Sci. Results, 130, 381395.
  • Bickert, T., and G. Wefer (1996), Late Quaternary deep water circulation in the South Atlantic: Reconstruction from carbonate dissolution and benthic stable isotopes, in The South Atlantic: Present and Past Circulation, edited by G. Wefer et al., pp. 599620, Springer, New York.
  • Bickert, T., W. B. Curry, and G. Wefer (1997), Late Pliocene to Holocene (2.6–0 Ma) western equatorial Atlantic deep-water circulation: Inferences from benthic stable isotopes, Proc. Ocean Drill. Program Sci. Results, 154, 239254.
  • Billups, K., A. C. Ravelo, and J. C. Zachos (1998), Early Pliocene deep water circulation in the western equatorial Atlantic: Implications for high-latitude climate change, Paleoceanography, 13, 8495.
  • Broecker, W. S., E. Clark, I. Hajdas, and G. Bonani (2004), Glacial ventilation rates for the deep Pacific Ocean, Paleoceanography, 19, PA2002, doi:10.1029/2003PA000974.
  • Cande, S. C., and D. V. Kent (1995), Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic, J. Geophys. Res., 100(B4), 60936095.
  • Chen, J., J. Farrell, D. Murray, and W. Prell (1995), Timescale and paleoceanographic implications of a 3.6 m. y. oxygen isotope record from the northeast Indian Ocean (Ocean Drilling Program site 758), Paleoceanography, 10, 2147.
  • Clemens, S. C., D. W. Murray, and W. L. Prell (1996), Nonstationary phase of the Plio-Pleistocene Asian monsoon, Science, 274, 943948.
  • Curry, W. B., and K. G. Miller (1989), Oxygen and carbon isotopic variation in Pliocene benthic foraminifers in, Proc. Ocean Drill. Program Sci. Results, 138, 157166.
  • deMenocal, P. B., D. W. Oppo, R. G. Fairbanks, and W. L. Prell (1992), Pleistocene δ13C variability of North Atlantic intermediate water, Paleoceanography, 7, 229250.
  • EPICA Community Members (2004), Eight glacial cycles from an Antarctic ice core, Nature, 429, 623628.
  • Flower, B. P., D. W. Oppo, J. F. McManus, K. A. Venz, D. A. Hodell, and J. L. Cullen (2000), North Atlantic intermediate to deep water circulation and chemical stratification during the past 1 Myr, Paleoceanography, 15, 388403.
  • Franz, S.-O. (1999), Pliozäne Zeitreihen zur Rekonstruktion der Tiefenwasserzirkulation und der siliziklastischen Amazonasfracht im äquatorialen Westatlantik (Ceara Schwelle, ODP Leg 154), Rep. 84, Geomar, Kiel, Germany.
  • Grootes, P. M., M. Stuvier, J. W. C. White, S. J. Johnsen, and J. Jouzel (1993), Comparison of oxygen isotope records from GISP2 and GRIP Greenland ice cores, Nature, 366, 552554.
  • Hale, W., and U. Pflaumann (1999), Sea-surface temperature estimations using a modern analog technique with foraminiferal assemblages from western Atlantic Quaternary sediments, in Use of Proxies in Paleoceanography—Examples From the South Atlantic, edited by G. Fischer, and G. Wefer, pp. 6990, Springer, New York.
  • Hall, I. R., I. N. McCave, N. J. Shackleton, G. P. Weedon, and S. E. Harris (2001), Intensified deep Pacific inflow and ventilation in Pleistocene glacial times, Nature, 412, 809812.
  • Harris, S. E. (2002), Data report: Late Pliocene-Pleistocene carbon and oxygen stable isotopes from benthic foraminifers at Ocean Drilling Program Site 1123 in the southwest Pacific, Proc. Ocean Drill. Program Sci. Results, 181, 120. (Available at http://www-odp.tamu.edu/publications/181_SR/203/203.htm.).
  • Haug, G. H., and R. Tiedemann (1998), Effect of the formation of the Isthmus of Panama on Atlantic Ocean thermohaline circulation, Nature, 393, 673676.
  • Herbert, T. D., J. D. Schuffert, D. Andreasen, L. Heusser, M. Lyle, A. Mix, A. C. Ravelo, L. D. Stott, and J. C. Herguera (2001), Collapse of the California current during glacial maxima linked to climate change on land, Science, 293, 7176.
  • Hodell, D. A., and K. Venz (1992), Toward a high-resolution stable isotopic record of the Southern Ocean during the Pliocene-Pleistocene (4.8 to 0.8 Ma), in The Antarctic Paleoenvironment: A Perspective on Global Change, Antarct. Res. Ser., vol. 56, edited by J. P. Kennett, and D. A. Warnkepp, pp. 265310, AGU, Washington, D. C.
  • Hodell, D. A., C. D. Charles, and F. J. Sierro (2001), Late Pleistocene evolution of the ocean's carbonate system, Earth Planet. Sci. Lett., 192, 109124.
  • Hodell, D. A., C. D. Charles, J. H. Curtis, P. G. Mortyn, U. S. Ninnemann, and K. A. Venz (2003), Data report: Oxygen isotope stratigraphy of ODP Leg 177 Sites 1088, 1089, 1090, 1093, and 1094, Proc. Ocean Drill. Program Sci. Results, 177, 126. (Available at http://www-odp.tamu.edu/publications/177_SR/volume/chapters/SR177_09.pdf.).
  • Hovan, S. A., D. K. Rea, and N. G. Pisias (1991), Late Pleistocene continental climate and oceanic variability recorded in northwest Pacific sediments, Paleoceanography, 6, 349370.
  • Huybers, P., and C. Wunsch (2004), A depth-derived Pleistocene age model: Uncertainty estimates, sedimentation variability, and nonlinear climate change, Paleoceanography, 19, PA1028, doi:10.1029/2002PA000857.
  • Imbrie, J., and J. Z. Imbrie (1980), Modeling the climatic response to orbital variations, Science, 207, 943953.
  • Imbrie, J., J. D. Hays, D. G. Martinson, A. McIntyre, A. C. Mix, J. J. Morley, N. G. Pisias, W. L. Prell, and N. J. Shackleton (1984), The orbital theory of Pleistocene climate: Support from a revised chronology, of the marine δ18O record, in Milankovitch and Climate, Part 1, edited by A. Berger, pp. 269305, Springer, New York.
  • Imbrie, J., et al. (1992), On the structure and origin of major glaciation cycles: 1. Linear responses to Milankovitch forcing, Paleoceanography, 7, 701738.
  • Jenkins, G. M., and D. G. Watts (1968), Spectral Analysis and Its Applications, 525 pp., Holden-Day, Boca Raton, Fla.
  • Jian, Z., Q. Zhao, X. Cheng, J. Wang, P. Wang, and X. Su (2003), Pliocene-Pleistocene stable isotope and paleoceanographic changes in the northern South China Sea, Palaeogeogr. Palaeoclimatol. Palaeoecol., 193, 425442.
  • Johnsen, S. J., H. B. Clausen, W. Dansgaard, N. Fuhrer, N. S. Gundestrup, C. U. Hammer, P. Iverson, J. Jouzel, B. Stauffer, and J. P. Steffensen (1992), Irregular glacial interstadials recorded in a new Greenland ice core, Nature, 364, 218220.
  • Karner, D. B., J. Levine, B. P. Medeiros, and R. A. Muller (2002), Constructing a stacked benthic δ18O record, Paleoceanography, 17(3), 1030, doi:10.1029/2001PA000667.
  • Keigwin, L. D., and M. A. Schlegel (2002), Ocean ventilation and sedimentation since the glacial maximum at 3 km in the western North Atlantic, Geochem. Geophys. Geosyst., 3(6), 1034, doi:10.1029/2001GC000283.
  • Laskar, J., F. Joutel, and F. Boudin (1993), Orbital, precessional and insolation quantities for the Earth from −20 Myr to +10 Myr, Astron. d Astrophys., 270, 522533.
  • Lisiecki, L. E., and P. A. Lisiecki (2002), Application of dynamic programming to the correlation of paleoclimate records, Paleoceanography, 17(4), 1049, doi:10.1029/2001PA000733.
  • Lourens, L. J., A. Andtonarakou, F. J. Hilgen, A. A. M. Van Hoof, C. Vergnaud-Grazzini, and W. J. Zachariasse (1996), Evaluation of the Plio-Pleistocene astronomical timescale, Paleoceanogrphy, 11, 391413.
  • Loutre, M. F., and A. Berger (2003), Marine isotope stage 11 as an analogue for the present interglacial, Global Planet. Change, 36, 209217.
  • Mc Intyre, K., A. C. Ravelo, and M. L. Delaney (1999), North Atlantic Intermediate Waters in the late Pliocene to early Pleistocene, Paleoceanography, 14, 324335.
  • Mc Intyre, K., M. L. Delaney, and A. C. Ravelo (2001), Millenial-scale climate change and oceanic processes in the late Pliocene and early Pleistocene, Paleoceanography, 16, 535543.
  • McManus, J. F., D. W. Oppo, and J. Cullen (1999), A 0.5-million-year record of millennial-scale climate variability in the North Atlantic, Science, 283, 971975.
  • Mix, A. C., N. G. Pisias, R. Zahn, W. Rugh, C. Lopez, and K. Nelson (1991), Carbon-13 in Pacific deep and intermediate waters, 0–370 ka: Implications for ocean circulation and Pleistocene carbon dioxide, Paleoceanography, 6, 205226.
  • Mix, A. C., J. Le, and N. J. Shackleton (1995a), Benthic foraminiferal stable isotope stratigraphy from Site 846: 0–1.8 Ma, Proc. Ocean Drill. Program Sci. Results, 138, 839847.
  • Mix, A. C., N. G. Pisias, W. Rugh, J. Wilson, A. Morey, and T. K. Hagelberg (1995b), Benthic foraminifer stable isotope record from Site 849 (0–5 Ma): Local and global climate changes, Proc. Ocean Drill. Program Sci. Results, 138, 371412.
  • Murray, R. W., C. Knowlton, M. Leinen, A. C. Mix, and C. H. Polsky (2000), Export production and carbonate dissolution in the central equatorial Pacific Ocean over the past 1 Ma, Paleoceanography, 15, 570592.
  • Ninkovitch, D., and N. J. Shackleton (1975), Distribution, stratigraphic position and age of ash layer “L,” in the Panama Basin region, Earth Planet. Sci. Lett., 27, 2034.
  • Oppo, D. W., R. G. Fairbanks, A. L. Gordon, and N. J. Shackleton (1990), Late Pleistocene Southern Ocean 13C variability, Paleoceanography, 5, 4354.
  • Oppo, D. W., J. F. McManus, and J. L. Cullen (1998), Abrupt climate events 500,000 to 340,000 years ago: Evidence from subpolar North Atlantic sediments, Science, 279, 13351338.
  • Pierre, C., J. F. Saliege, M. J. Urrutiaguer, and J. Giraudeau (2001), Stable isotope record of the last 500 k.y. at Site 1087 (Southern Cape Basin), Proc. Ocean Drill. Program Sci. Results, 175, 122. (Available at http://www-odp.tamu.edu/publications/175_SR/chap_12/chap_12.htm.).
  • Pisias, N. G., D. G. Martinson, T. C. Moore Jr., N. J. Shackleton, W. Prell, J. Hays, and G. Boden (1984), High resolution stratigraphic correlation of benthic oxygen isotope records spanning the last 300,000 years, Mar. Geol., 56, 119136.
  • Pisias, N. G., A. C. Mix, and R. Zahn (1990), Nonlinear response in the global climate system: Evidence from benthic oxygen isotopic record in core RC13-110, Paleoceanography, 5, 147160.
  • Prell, W. L., J. Imbrie, D. G. Martinson, J. J. Morley, N. G. Pisias, N. J. Shackleton, and H. F. Streeter (1986), Graphic correlation of oxygen isotope stratigraphy: Application to the Late Quaternary, Paleoceanography, 1, 137162.
  • Raymo, M. E. (1997), The timing of major climate terminations, Paleoceanography, 12, 577585.
  • Raymo, M. E., W. F. Ruddiman, and B. M. Clement (1986), Plio-Pleistocene paleoceanography of the North Atlantic at Deep Sea Drilling Project Site 609, Initial Rep. Deep Sea Drill. Proj., 94, 895901.
  • Raymo, M. E., W. F. Ruddiman, J. Backman, B. M. Clement, and D. G. Martinson (1989), Late Pliocene variation in Northern Hemisphere ice sheets and North Atlantic Deep Water circulation, Paleoceanography, 4, 413446.
  • Raymo, M. E., W. F. Ruddiman, N. J. Shackleton, and D. W. Oppo (1990), Evolution of Atlantic-Pacific δ13C gradients over the last 2.5 m. y. Earth Planet. Sci. Lett., 97, 353368.
  • Raymo, M. E., D. Hodell, and E. Jansen (1992), Response of deep ocean circulation to initiation of Northern Hemisphere glaciation (3–2 MA), Paleoceanography, 7, 645672.
  • Raymo, M. E., D. W. Oppo, and W. Curry (1997), The mid-Pleistocene climate transition: A deep sea carbon isotopic perspective, Paleoceanography, 12, 546559.
  • Raymo, M. E., D. W. Oppo, B. P. Flower, D. A. Hodell, J. F. McManus, K. A. Venz, K. F. Kleiven, and K. McIntyre (2004), Stability of North Atlantic water masses in face of pronounced climate variability during the Pleistocene, Paleoceanography, 19, PA2008, doi:10.1029/2003PA000921.
  • Ruddiman, W. F., M. E. Raymo, D. G. Martinson, B. M. Clement, and J. Backman (1989), Pleistocene evolution of Northern Hemisphere climate, Paleoceanography, 4, 353412.
  • Sarnthein, M., K. Winn, S. J. A. Jung, J. C. Duplessy, L. D. Labeyrie, H. Erlenkeuser, and G. Ganssen (1994), Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions, Paleoceanography, 9, 209267.
  • Shackleton, N. J. (1995), New data on the evolution of Pliocene climate variability, in Paleoclimate and Evolution, With Emphasis on Human Origins, edited by E. S. Vrba et al., pp. 242248, Yale Univ. Press, New Haven, Ct.
  • Shackleton, N. J., and M. A. Hall (1984), Oxygen and carbon isotope stratigraphy of DSDP Hole 552A: Plio-Pleistocene glacial history, Initial Rep. Deep Sea Drill. Project, 81, 599609.
  • Shackleton, N. J., and N. G. Pisias (1985), Atmospheric carbon dioxide, orbital forcing, and climate, in The Carbon Cycle and Atmospheric CO2: Natural Variations Archean to Present, Geophys. Monogr. Ser., vol. 32, edited by E. Sundquist, and W. S. Broecker, pp. 303317, AGU, Washington, D. C.
  • Shackleton, N. J., A. Berger, and W. R. Peltier (1990), An alternative astronomical calibration of the Lower Pleistocene timescale based on ODP Site 677, Trans. R. Soc. Edinburgh Earth Sci., 81, 251261.
  • Shackleton, N. J., M. A. Hall, and D. Pate (1995a), Pliocene stable isotope stratigraphy of ODP Site 846, Proc. Ocean Drill. Program Sci. Results, 138, 337356.
  • Shackleton, N. J., S. Crowhurst, T. Hagelberg, N. G. Pisias, and D. A. Schneider (1995b), A new late Neogene time scale: Application to Leg 138 sites, Proc. Ocean Drill. Program Sci. Results, 138, 73101.
  • Shackleton, N. J., M. A. Hall, and E. Vincent (2000), Phase relationships between millennial-scale events 64,000–24,000 years ago, Paleoceanography, 15, 565569.
  • Skinner, L. C., and I. N. McCave (2003), Analysis and modeling of gravity- and piston-coring based on soil mechanics, Mar. Geol., 199, 181204.
  • Stein, M., G. J. Wasserburg, P. Aharon, J. H. Chen, Z. R. Zhu, A. Bloom, and J. Chappell (1993), TIMS U-series dating and stable isotopes of the last interglacial event in Papua New Guinea, Geochim. Cosmochim. Acta, 57, 25412554.
  • Tian, J., P. Wang, X. Cheng, and Q. Ling (2002), Astronomically tuned Plio-Pleistocene 18O record from South China Sea and Atlantic-Pacific comparison, Earth Planet. Sci. Lett., 203, 10151029.
  • Tiedemann, R. (1991), Acht Millionen Jahre Klimageschichte von Nordwest Afrika und Paläo-Ozeanographie des angrenzenden Atlantiks, Ber. Rep. 46, 190 pp., Geol.-Paläontol. Inst. und Mus., Christian-Albrechts-Univ., Kiel, Germany.
  • Tiedemann, R., and S. O. Franz (1997), Deep-water cicurlation, chemistry, and terrigenous sediment supply in the equatorial Atlantic during the Pliocene, 3.3–2.6 Ma and 5–4.5 Ma, Proc. Ocean Drill. Program Sci. Results, 154, 299318.
  • Tiedemann, R., M. Sarnthein, and N. J. Shackleton (1994), Astronomic timescale for the Pliocene Atlantic δ18O and dust flux records of Ocean Drilling Program site 659, Paleoceanography, 9, 619638.
  • Venz, K. A., and D. A. Hodell (2002), New evidence for changes in Plio-Pleistocene deep water circulation from Southern Ocean ODP Leg 177 Site 1090, Palaeogeogr. Palaeoclimatol. Palaeoecol., 182, 197220.
  • Venz, K. A., D. A. Hodell, C. Stanton, and D. A. Warnke (1999), A 1.0 Myr record of Glacial North Atlantic Intermediate Water variability from ODP site 982 in the northeast Atlantic, Paleoceanography, 14, 4252.
  • Waelbroeck, C., J.-C. Duplessy, E. Michel, L. Labeyrie, D. Paillard, and J. Duprat (2001), The timing of the last deglaciation in North Atlantic climate records, Nature, 412, 724727.
  • Williams, D. F., R. C. Thunell, E. Tappa, D. Rio, and I. Raffi (1988), Chronology of the Pleistocene oxygen isotope record: 0–1.88 m. y. B. P. Palaeogeogr. Palaeoclimatol. Palaeoecol., 64, 221240.
  • Zabel, M., T. Bickert, L. Dittert, and R. R. Haese (1999), The significance of the sedimentary Al/Ti ratio as indicator for reconstructions of the terrestrial input to the equatorial Atlantic, Paleoceanography, 14, 789799.