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 *

137 related articles for article (PubMed ID: 28855507)

  • 21. Onset of the aerobic nitrogen cycle during the Great Oxidation Event.
    Zerkle AL; Poulton SW; Newton RJ; Mettam C; Claire MW; Bekker A; Junium CK
    Nature; 2017 Feb; 542(7642):465-467. PubMed ID: 28166535
    [TBL] [Abstract][Full Text] [Related]  

  • 22. The redox structure of Ediacaran and early Cambrian oceans and its controls.
    Li C; Shi W; Cheng M; Jin C; Algeo TJ
    Sci Bull (Beijing); 2020 Dec; 65(24):2141-2149. PubMed ID: 36732967
    [TBL] [Abstract][Full Text] [Related]  

  • 23. Heterogeneous and dynamic marine shelf oxygenation and coupled early animal evolution.
    Li C; Cheng M; Zhu M; Lyons TW
    Emerg Top Life Sci; 2018 Sep; 2(2):279-288. PubMed ID: 32412626
    [TBL] [Abstract][Full Text] [Related]  

  • 24. Molybdenum isotope evidence for widespread anoxia in mid-Proterozoic oceans.
    Arnold GL; Anbar AD; Barling J; Lyons TW
    Science; 2004 Apr; 304(5667):87-90. PubMed ID: 15066776
    [TBL] [Abstract][Full Text] [Related]  

  • 25. The paleoredox context of early eukaryotic evolution: insights from the Tonian Mackenzie Mountains Supergroup, Canada.
    Maloney KM; Halverson GP; Lechte M; Gibson TM; Bui TH; Schiffbauer JD; Laflamme M
    Geobiology; 2024; 22(3):e12598. PubMed ID: 38700417
    [TBL] [Abstract][Full Text] [Related]  

  • 26. Evidence for the early Toarcian Carbon Isotope Excursion (T-CIE) from the shallow marine siliciclastic red beds of Arabia.
    Alnazghah M; Koeshidayatullah A; Al-Hussaini A; Amao A; Song H; Al-Ramadan K
    Sci Rep; 2022 Oct; 12(1):18124. PubMed ID: 36302804
    [TBL] [Abstract][Full Text] [Related]  

  • 27. Fossilized iron bacteria reveal a pathway to the biological origin of banded iron formation.
    Chi Fru E; Ivarsson M; Kilias SP; Bengtson S; Belivanova V; Marone F; Fortin D; Broman C; Stampanoni M
    Nat Commun; 2013; 4():2050. PubMed ID: 23784372
    [TBL] [Abstract][Full Text] [Related]  

  • 28. Evidence for low sulphate and anoxia in a mid-Proterozoic marine basin.
    Shen Y; Knoll AH; Walter MR
    Nature; 2003 Jun; 423(6940):632-5. PubMed ID: 12789336
    [TBL] [Abstract][Full Text] [Related]  

  • 29. Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation.
    Zhang J; Fan T; Zhang Y; Lash GG; Li Y; Wu Y
    Sci Rep; 2017 Aug; 7(1):8550. PubMed ID: 28819268
    [TBL] [Abstract][Full Text] [Related]  

  • 30. Phosphogenesis in the 2460 and 2728 million-year-old banded iron formations as evidence for biological cycling of phosphate in the early biosphere.
    Li YL; Sun S; Chan LS
    Ecol Evol; 2012 Jan; 3(1):115-25. PubMed ID: 23404127
    [TBL] [Abstract][Full Text] [Related]  

  • 31. Biomarker evidence for green and purple sulphur bacteria in a stratified Palaeoproterozoic sea.
    Brocks JJ; Love GD; Summons RE; Knoll AH; Logan GA; Bowden SA
    Nature; 2005 Oct; 437(7060):866-70. PubMed ID: 16208367
    [TBL] [Abstract][Full Text] [Related]  

  • 32. Evolution of the global phosphorus cycle.
    Reinhard CT; Planavsky NJ; Gill BC; Ozaki K; Robbins LJ; Lyons TW; Fischer WW; Wang C; Cole DB; Konhauser KO
    Nature; 2017 Jan; 541(7637):386-389. PubMed ID: 28002400
    [TBL] [Abstract][Full Text] [Related]  

  • 33. Ocean productivity before about 1.9 Gyr ago limited by phosphorus adsorption onto iron oxides.
    Bjerrum CJ; Canfield DE
    Nature; 2002 May; 417(6885):159-62. PubMed ID: 12000956
    [TBL] [Abstract][Full Text] [Related]  

  • 34. 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]  

  • 35. In situ trace metal analysis of Neoarchaean--Ordovician shallow-marine microbial-carbonate-hosted pyrites.
    Gallagher M; Turner EC; Kamber BS
    Geobiology; 2015 Jul; 13(4):316-39. PubMed ID: 25917609
    [TBL] [Abstract][Full Text] [Related]  

  • 36. Subducted banded iron formations as a source of ultralow-velocity zones at the core-mantle boundary.
    Dobson DP; Brodholt JP
    Nature; 2005 Mar; 434(7031):371-4. PubMed ID: 15772658
    [TBL] [Abstract][Full Text] [Related]  

  • 37. Late-Neoproterozoic deep-ocean oxygenation and the rise of animal life.
    Canfield DE; Poulton SW; Narbonne GM
    Science; 2007 Jan; 315(5808):92-5. PubMed ID: 17158290
    [TBL] [Abstract][Full Text] [Related]  

  • 38. Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2.
    Clarkson MO; Stirling CH; Jenkyns HC; Dickson AJ; Porcelli D; Moy CM; Pogge von Strandmann PAE; Cooke IR; Lenton TM
    Proc Natl Acad Sci U S A; 2018 Mar; 115(12):2918-2923. PubMed ID: 29507196
    [TBL] [Abstract][Full Text] [Related]  

  • 39. Iron isotope fractionation during microbial dissimilatory iron oxide reduction in simulated Archaean seawater.
    Percak-Dennett EM; Beard BL; Xu H; Konishi H; Johnson CM; Roden EE
    Geobiology; 2011 May; 9(3):205-20. PubMed ID: 21504536
    [TBL] [Abstract][Full Text] [Related]  

  • 40. 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]  

    [Previous]   [Next]    [New Search]
    of 7.