These tools will no longer be maintained as of December 31, 2024. Archived website can be found here. PubMed4Hh GitHub repository can be found here. Contact NLM Customer Service if you have questions.


BIOMARKERS

Molecular Biopsy of Human Tumors

- a resource for Precision Medicine *

253 related articles for article (PubMed ID: 11201737)

  • 1. Increased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period.
    Erbacher J; Huber BT; Norris RD; Markey M
    Nature; 2001 Jan; 409(6818):325-7. PubMed ID: 11201737
    [TBL] [Abstract][Full Text] [Related]  

  • 2. Warm tropical ocean surface and global anoxia during the mid-Cretaceous period.
    Wilson PA; Norris RD
    Nature; 2001 Jul; 412(6845):425-9. PubMed ID: 11473314
    [TBL] [Abstract][Full Text] [Related]  

  • 3. Oxidation of the Ediacaran ocean.
    Fike DA; Grotzinger JP; Pratt LM; Summons RE
    Nature; 2006 Dec; 444(7120):744-7. PubMed ID: 17151665
    [TBL] [Abstract][Full Text] [Related]  

  • 4. Carbon dioxide release from the North Pacific abyss during the last deglaciation.
    Galbraith ED; Jaccard SL; Pedersen TF; Sigman DM; Haug GH; Cook M; Southon JR; Francois R
    Nature; 2007 Oct; 449(7164):890-3. PubMed ID: 17943127
    [TBL] [Abstract][Full Text] [Related]  

  • 5. Massive expansion of marine archaea during a mid-Cretaceous oceanic anoxic event.
    Kuypers MM; Blokker P; Erbacher J; Kinkel H; Pancost RD; Schouten S; Sinninghe Damste JS
    Science; 2001 Jul; 293(5527):92-5. PubMed ID: 11441180
    [TBL] [Abstract][Full Text] [Related]  

  • 6. Latitudinal variations in plankton delta 13C: implications for CO2 and productivity in past oceans.
    Rau GH; Takahashi T; Des Marais DJ
    Nature; 1989 Oct; 341(6242):516-8. PubMed ID: 11536614
    [TBL] [Abstract][Full Text] [Related]  

  • 7. Cretaceous oceanic anoxic event 2 triggered by a massive magmatic episode.
    Turgeon SC; Creaser RA
    Nature; 2008 Jul; 454(7202):323-6. PubMed ID: 18633415
    [TBL] [Abstract][Full Text] [Related]  

  • 8. Changes in carbon dioxide during an oceanic anoxic event linked to intrusion into Gondwana coals.
    McElwain JC; Wade-Murphy J; Hesselbo SP
    Nature; 2005 May; 435(7041):479-82. PubMed ID: 15917805
    [TBL] [Abstract][Full Text] [Related]  

  • 9. The cause of carbon isotope minimum events on glacial terminations.
    Spero HJ; Lea DW
    Science; 2002 Apr; 296(5567):522-5. PubMed ID: 11964477
    [TBL] [Abstract][Full Text] [Related]  

  • 10. Increased dissolved oxygen in Pacific intermediate waters due to lower rates of carbon oxidation in sediments.
    Stott LD; Berelson W; Douglas R; Gorsline D
    Nature; 2000 Sep; 407(6802):367-70. PubMed ID: 11014190
    [TBL] [Abstract][Full Text] [Related]  

  • 11. Increased productivity in the subantarctic ocean during Heinrich events.
    Sachs JP; Anderson RF
    Nature; 2005 Apr; 434(7037):1118-21. PubMed ID: 15858571
    [TBL] [Abstract][Full Text] [Related]  

  • 12. Comment on "Calcareous nannoplankton response to surface-water acidification around Oceanic Anoxic Event 1a".
    Gibbs SJ; Robinson SA; Bown PR; Jones TD; Henderiks J
    Science; 2011 Apr; 332(6026):175; author reply 175. PubMed ID: 21474738
    [TBL] [Abstract][Full Text] [Related]  

  • 13. Atmospheric carbon dioxide concentrations over the past 60 million years.
    Pearson PN; Palmer MR
    Nature; 2000 Aug; 406(6797):695-9. PubMed ID: 10963587
    [TBL] [Abstract][Full Text] [Related]  

  • 14. The transition to a sulphidic ocean approximately 1.84 billion years ago.
    Poulton SW; Fralick PW; Canfield DE
    Nature; 2004 Sep; 431(7005):173-7. PubMed ID: 15356628
    [TBL] [Abstract][Full Text] [Related]  

  • 15. Mediterranean Sea surface radiocarbon reservoir age changes since the last glacial maximum.
    Siani G; Paterne M; Michel E; Sulpizio R; Sbrana A; Arnold M; Haddad G
    Science; 2001 Nov; 294(5548):1917-20. PubMed ID: 11729315
    [TBL] [Abstract][Full Text] [Related]  

  • 16. High temperatures in the Late Cretaceous Arctic Ocean.
    Jenkyns HC; Forster A; Schouten S; Sinninghe Damsté JS
    Nature; 2004 Dec; 432(7019):888-92. PubMed ID: 15602558
    [TBL] [Abstract][Full Text] [Related]  

  • 17. Tracing the stepwise oxygenation of the Proterozoic ocean.
    Scott C; Lyons TW; Bekker A; Shen Y; Poulton SW; Chu X; Anbar AD
    Nature; 2008 Mar; 452(7186):456-9. PubMed ID: 18368114
    [TBL] [Abstract][Full Text] [Related]  

  • 18. Stable sea surface temperatures in the western Pacific warm pool over the past 1.75 million years.
    de Garidel-Thoron T; Rosenthal Y; Bassinot F; Beaufort L
    Nature; 2005 Jan; 433(7023):294-8. PubMed ID: 15662419
    [TBL] [Abstract][Full Text] [Related]  

  • 19. A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization.
    Boyd PW; Watson AJ; Law CS; Abraham ER; Trull T; Murdoch R; Bakker DC; Bowie AR; Buesseler KO; Chang H; Charette M; Croot P; Downing K; Frew R; Gall M; Hadfield M; Hall J; Harvey M; Jameson G; LaRoche J; Liddicoat M; Ling R; Maldonado MT; McKay RM; Nodder S; Pickmere S; Pridmore R; Rintoul S; Safi K; Sutton P; Strzepek R; Tanneberger K; Turner S; Waite A; Zeldis J
    Nature; 2000 Oct; 407(6805):695-702. PubMed ID: 11048709
    [TBL] [Abstract][Full Text] [Related]  

  • 20. Evidence against dust-mediated control of glacial-interglacial changes in atmospheric CO2.
    Maher BA; Dennis PF
    Nature; 2001 May; 411(6834):176-80. PubMed ID: 11346790
    [TBL] [Abstract][Full Text] [Related]  

    [Next]    [New Search]
    of 13.