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Journal Abstract Search

533 related items for PubMed ID: 19005552

  • 1. Transient nature of late Pleistocene climate variability.
    Crowley TJ, Hyde WT.
    Nature; 2008 Nov 13; 456(7219):226-30. PubMed ID: 19005552
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  • 2. High-latitude influence on the eastern equatorial Pacific climate in the early Pleistocene epoch.
    Liu Z, Herbert TD.
    Nature; 2004 Feb 19; 427(6976):720-3. PubMed ID: 14973481
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  • 4. Thresholds for Cenozoic bipolar glaciation.
    Deconto RM, Pollard D, Wilson PA, Pälike H, Lear CH, Pagani M.
    Nature; 2008 Oct 02; 455(7213):652-6. PubMed ID: 18833277
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  • 5. Global cooling during the eocene-oligocene climate transition.
    Liu Z, Pagani M, Zinniker D, Deconto R, Huber M, Brinkhuis H, Shah SR, Leckie RM, Pearson A.
    Science; 2009 Feb 27; 323(5918):1187-90. PubMed ID: 19251622
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  • 7. Eocene bipolar glaciation associated with global carbon cycle changes.
    Tripati A, Backman J, Elderfield H, Ferretti P.
    Nature; 2005 Jul 21; 436(7049):341-6. PubMed ID: 16034408
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  • 9. Early onset and tropical forcing of 100,000-year Pleistocene glacial cycles.
    Rutherford S, D'Hondt S.
    Nature; 2000 Nov 02; 408(6808):72-5. PubMed ID: 11081508
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  • 10. Muted climate variations in continental Siberia during the mid-Pleistocene epoch.
    Prokopenko AA, Williams DF, Kuzmin MI, Karabanov EB, Khursevich GK, Peck JA.
    Nature; 2002 Jul 04; 418(6893):65-8. PubMed ID: 12097906
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  • 11. Regional climate shifts caused by gradual global cooling in the Pliocene epoch.
    Ravelo AC, Andreasen DH, Lyle M, Olivarez Lyle A, Wara MW.
    Nature; 2004 May 20; 429(6989):263-7. PubMed ID: 15152244
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  • 12. North American ice-sheet dynamics and the onset of 100,000-year glacial cycles.
    Bintanja R, van de Wal RS.
    Nature; 2008 Aug 14; 454(7206):869-72. PubMed ID: 18704083
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  • 13. Impacts of orbital forcing and atmospheric carbon dioxide on Miocene ice-sheet expansion.
    Holbourn A, Kuhnt W, Schulz M, Erlenkeuser H.
    Nature; 2005 Nov 24; 438(7067):483-7. PubMed ID: 16306989
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  • 17. Low-latitude glaciation and rapid changes in the Earth's obliquity explained by obliquity-oblateness feedback.
    Williams DM, Kasting JF, Frakes LA.
    Nature; 1998 Dec 03; 396(6710):453-5. PubMed ID: 9853751
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  • 19. Coupling of CO2 and ice sheet stability over major climate transitions of the last 20 million years.
    Tripati AK, Roberts CD, Eagle RA.
    Science; 2009 Dec 04; 326(5958):1394-7. PubMed ID: 19815724
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