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  1. Consequences of twenty-first-century policy for multi-millennial climate and sea-level change

    To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Nature...

  2. Climate Sensitivity Estimated From Temperature Reconstructions of the Last Glacial Maximum

    This is the author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by the American Association for the Advancement of Science and can be found at:...

  3. Climatically driven changes in oceanic processes throughout the equatorial Pacific

    Copyright 2004 by the American Geophysical Union

  4. Planktonic foraminifera, sea surface temperatures, and mechanisms of oceanic change in the Peru and south equatorial...

    Copyright 2003 by the American Geophysical Union

  5. Leg 202 summary

    Shipboard scientific party : Chapter 1, Leg 202 Summary

  6. Foraminiferal faunal estimates of paleotemperature: Circumventing the no-analog problem yields cool ice age tropics

    Copyright 1999 by the American Geophysical Union

  7. Benthic foraminifer stable isotope record from Site 849 (0 - 5 Ma) : local and global climate changes

    Benthic foraminifer and δ¹³C data from Site 849, on the west flank of the East Pacific Rise (0°11'N, 110°3l'W; 3851 m), give

  8. Leg 202 synthesis: Southeast Pacific paleoceangraphy

    Ocean Drilling Program (ODP) Leg 202 has opened a new window

  9. Eastern Pacific Warm Pool paleosalinity and climate variability: 0–30 kyr

    Multiproxy geologic records of δ18O and Mg/Ca in fossil foraminifera from sediments under the Eastern Pacific Warm Pool (EPWP) region west of Central America document variations in upper ocean temperature,...

  10. Biogenic and terrigenous sedimetations at Ceara rise, western tropical Altantic, supports Pliocene - Pleistocene deep - water...

    Calcium carbonate percentages at five Ceara Rise sites were estimated at 1- to 2-k.y. intervals over the past 5 m.y., using

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