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 *

157 related articles for article (PubMed ID: 27447895)

  • 1. Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth.
    Sansjofre P; Cartigny P; Trindade RI; Nogueira AC; Agrinier P; Ader M
    Nat Commun; 2016 Jul; 7():12192. PubMed ID: 27447895
    [TBL] [Abstract][Full Text] [Related]  

  • 2. Episode of intense chemical weathering during the termination of the 635 Ma Marinoan glaciation.
    Huang KJ; Teng FZ; Shen B; Xiao S; Lang X; Ma HR; Fu Y; Peng Y
    Proc Natl Acad Sci U S A; 2016 Dec; 113(52):14904-14909. PubMed ID: 27956606
    [TBL] [Abstract][Full Text] [Related]  

  • 3. Ocean oxygenation in the wake of the Marinoan glaciation.
    Sahoo SK; Planavsky NJ; Kendall B; Wang X; Shi X; Scott C; Anbar AD; Lyons TW; Jiang G
    Nature; 2012 Sep; 489(7417):546-9. PubMed ID: 23018964
    [TBL] [Abstract][Full Text] [Related]  

  • 4. A transient peak in marine sulfate after the 635-Ma snowball Earth.
    Peng Y; Bao H; Jiang G; Crockford P; Feng D; Xiao S; Kaufman AJ; Wang J
    Proc Natl Acad Sci U S A; 2022 May; 119(19):e2117341119. PubMed ID: 35500113
    [TBL] [Abstract][Full Text] [Related]  

  • 5. Neoproterozoic syn-glacial carbonate precipitation and implications for a snowball Earth.
    Hood AVS; Penman DE; Lechte MA; Wallace MW; Giddings JA; Planavsky NJ
    Geobiology; 2022 Mar; 20(2):175-193. PubMed ID: 34528380
    [TBL] [Abstract][Full Text] [Related]  

  • 6. Sulfur record of rising and falling marine oxygen and sulfate levels during the Lomagundi event.
    Planavsky NJ; Bekker A; Hofmann A; Owens JD; Lyons TW
    Proc Natl Acad Sci U S A; 2012 Nov; 109(45):18300-5. PubMed ID: 23090989
    [TBL] [Abstract][Full Text] [Related]  

  • 7. Snowball Earth termination by destabilization of equatorial permafrost methane clathrate.
    Kennedy M; Mrofka D; von der Borch C
    Nature; 2008 May; 453(7195):642-5. PubMed ID: 18509441
    [TBL] [Abstract][Full Text] [Related]  

  • 8. Uranium isotopes distinguish two geochemically distinct stages during the later Cambrian SPICE event.
    Dahl TW; Boyle RA; Canfield DE; Connelly JN; Gill BC; Lenton TM; Bizzarro M
    Earth Planet Sci Lett; 2014 Sep; 401():313-326. PubMed ID: 25684783
    [TBL] [Abstract][Full Text] [Related]  

  • 9. Rapid sea level rise in the aftermath of a Neoproterozoic snowball Earth.
    Myrow PM; Lamb MP; Ewing RC
    Science; 2018 May; 360(6389):649-651. PubMed ID: 29674430
    [TBL] [Abstract][Full Text] [Related]  

  • 10. Transient marine euxinia at the end of the terminal Cryogenian glaciation.
    Lang X; Shen B; Peng Y; Xiao S; Zhou C; Bao H; Kaufman AJ; Huang K; Crockford PW; Liu Y; Tang W; Ma H
    Nat Commun; 2018 Aug; 9(1):3019. PubMed ID: 30068999
    [TBL] [Abstract][Full Text] [Related]  

  • 11. Sulfur isotopes track the global extent and dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2.
    Owens JD; Gill BC; Jenkyns HC; Bates SM; Severmann S; Kuypers MM; Woodfine RG; Lyons TW
    Proc Natl Acad Sci U S A; 2013 Nov; 110(46):18407-12. PubMed ID: 24170863
    [TBL] [Abstract][Full Text] [Related]  

  • 12. Pyrite sulfur isotopes reveal glacial-interglacial environmental changes.
    Pasquier V; Sansjofre P; Rabineau M; Revillon S; Houghton J; Fike DA
    Proc Natl Acad Sci U S A; 2017 Jun; 114(23):5941-5945. PubMed ID: 28533378
    [TBL] [Abstract][Full Text] [Related]  

  • 13. Isotopically anomalous organic carbon in the aftermath of the Marinoan snowball Earth.
    Liljestrand FL; Laakso TA; Macdonald FA; Schrag DP; Johnston DT
    Geobiology; 2020 Jul; 18(4):476-485. PubMed ID: 32562514
    [TBL] [Abstract][Full Text] [Related]  

  • 14. The carbon isotope composition of ancient CO2 based on higher-plant organic matter.
    Gröcke DR
    Philos Trans A Math Phys Eng Sci; 2002 Apr; 360(1793):633-58. PubMed ID: 12804297
    [TBL] [Abstract][Full Text] [Related]  

  • 15. Triple oxygen isotope evidence for elevated CO2 levels after a Neoproterozoic glaciation.
    Bao H; Lyons JR; Zhou C
    Nature; 2008 May; 453(7194):504-6. PubMed ID: 18497821
    [TBL] [Abstract][Full Text] [Related]  

  • 16. Extreme winds and waves in the aftermath of a Neoproterozoic glaciation.
    Allen PA; Hoffman PF
    Nature; 2005 Jan; 433(7022):123-7. PubMed ID: 15650730
    [TBL] [Abstract][Full Text] [Related]  

  • 17. Rapid oxygenation of Earth's atmosphere 2.33 billion years ago.
    Luo G; Ono S; Beukes NJ; Wang DT; Xie S; Summons RE
    Sci Adv; 2016 May; 2(5):e1600134. PubMed ID: 27386544
    [TBL] [Abstract][Full Text] [Related]  

  • 18. Sedimentary constraints on the duration of the Marinoan Oxygen-17 Depletion (MOSD) event.
    Killingsworth BA; Hayles JA; Zhou C; Bao H
    Proc Natl Acad Sci U S A; 2013 Oct; 110(44):17686-90. PubMed ID: 23386719
    [TBL] [Abstract][Full Text] [Related]  

  • 19. Multiple sulfur-isotope signatures in Archean sulfates and their implications for the chemistry and dynamics of the early atmosphere.
    Muller É; Philippot P; Rollion-Bard C; Cartigny P
    Proc Natl Acad Sci U S A; 2016 Jul; 113(27):7432-7. PubMed ID: 27330111
    [TBL] [Abstract][Full Text] [Related]  

  • 20. Selenium isotope evidence for progressive oxidation of the Neoproterozoic biosphere.
    Pogge von Strandmann PA; Stüeken EE; Elliott T; Poulton SW; Dehler CM; Canfield DE; Catling DC
    Nat Commun; 2015 Dec; 6():10157. PubMed ID: 26679529
    [TBL] [Abstract][Full Text] [Related]  

    [Next]    [New Search]
    of 8.