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 *

125 related articles for article (PubMed ID: 36781894)

  • 21. Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction.
    Zhang F; Romaniello SJ; Algeo TJ; Lau KV; Clapham ME; Richoz S; Herrmann AD; Smith H; Horacek M; Anbar AD
    Sci Adv; 2018 Apr; 4(4):e1602921. PubMed ID: 29651454
    [TBL] [Abstract][Full Text] [Related]  

  • 22. Evidence for rapid weathering response to climatic warming during the Toarcian Oceanic Anoxic Event.
    Them TR; Gill BC; Selby D; Gröcke DR; Friedman RM; Owens JD
    Sci Rep; 2017 Jul; 7(1):5003. PubMed ID: 28694487
    [TBL] [Abstract][Full Text] [Related]  

  • 23. Transient cooling episodes during Cretaceous Oceanic Anoxic Events with special reference to OAE 1a (Early Aptian).
    Jenkyns HC
    Philos Trans A Math Phys Eng Sci; 2018 Oct; 376(2130):. PubMed ID: 30177559
    [TBL] [Abstract][Full Text] [Related]  

  • 24. Assessing the importance of thermogenic degassing from the Karoo Large Igneous Province (LIP) in driving Toarcian carbon cycle perturbations.
    Heimdal TH; Goddéris Y; Jones MT; Svensen HH
    Nat Commun; 2021 Oct; 12(1):6221. PubMed ID: 34711826
    [TBL] [Abstract][Full Text] [Related]  

  • 25. Biomarker and compound-specific isotope records across the Toarcian CIE at the Dormettingen section in SW Germany.
    Ajuaba S; Sachsenhofer RF; Bechtel A; Galasso F; Gross D; Misch D; Schneebeli-Hermann E
    Int J Earth Sci; 2022; 111(5):1631-1661. PubMed ID: 35707060
    [TBL] [Abstract][Full Text] [Related]  

  • 26. Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery.
    Clarkson MO; Wood RA; Poulton SW; Richoz S; Newton RJ; Kasemann SA; Bowyer F; Krystyn L
    Nat Commun; 2016 Jul; 7():12236. PubMed ID: 27433855
    [TBL] [Abstract][Full Text] [Related]  

  • 27. Volume and rate of volcanic CO
    Jiang Q; Jourdan F; Olierook HKH; Merle RE; Bourdet J; Fougerouse D; Godel B; Walker AT
    Proc Natl Acad Sci U S A; 2022 Aug; 119(31):e2202039119. PubMed ID: 35878029
    [TBL] [Abstract][Full Text] [Related]  

  • 28. Global controls on phosphatization of fossils during the toarcian oceanic anoxic event.
    Sinha S; Muscente AD; Schiffbauer JD; Williams M; Schweigert G; Martindale RC
    Sci Rep; 2021 Dec; 11(1):24087. PubMed ID: 34916533
    [TBL] [Abstract][Full Text] [Related]  

  • 29. Mechanisms and drivers of belemnite body-size dynamics across the Pliensbachian-Toarcian crisis.
    Rita P; Nätscher P; Duarte LV; Weis R; De Baets K
    R Soc Open Sci; 2019 Dec; 6(12):190494. PubMed ID: 31903197
    [TBL] [Abstract][Full Text] [Related]  

  • 30. Evidence for rapid climate change in the Mesozoic-Palaeogene greenhouse world.
    Jenkyns HC
    Philos Trans A Math Phys Eng Sci; 2003 Sep; 361(1810):1885-916; discussion 1916. PubMed ID: 14558900
    [TBL] [Abstract][Full Text] [Related]  

  • 31. Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event.
    Hesselbo SP; Grocke DR; Jenkyns HC; Bjerrum CJ; Farrimond P; Morgans Bell HS ; Green OR
    Nature; 2000 Jul; 406(6794):392-5. PubMed ID: 10935632
    [TBL] [Abstract][Full Text] [Related]  

  • 32. Evidence for local carbon-cycle perturbations superimposed on the Toarcian carbon isotope excursion.
    Wang Y; Ossa Ossa F; Wille M; Schurr S; Saussele ME; Schmid-Röhl A; Schoenberg R
    Geobiology; 2020 Nov; 18(6):682-709. PubMed ID: 32783292
    [TBL] [Abstract][Full Text] [Related]  

  • 33. Warm afterglow from the Toarcian Oceanic Anoxic Event drives the success of deep-adapted brachiopods.
    Ullmann CV; Boyle R; Duarte LV; Hesselbo SP; Kasemann SA; Klein T; Lenton TM; Piazza V; Aberhan M
    Sci Rep; 2020 Apr; 10(1):6549. PubMed ID: 32300235
    [TBL] [Abstract][Full Text] [Related]  

  • 34. A major sea-level drop briefly precedes the Toarcian oceanic anoxic event: implication for Early Jurassic climate and carbon cycle.
    Krencker FN; Lindström S; Bodin S
    Sci Rep; 2019 Aug; 9(1):12518. PubMed ID: 31467345
    [TBL] [Abstract][Full Text] [Related]  

  • 35. 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]  

  • 36. Extensive marine anoxia during the terminal Ediacaran Period.
    Zhang F; Xiao S; Kendall B; Romaniello SJ; Cui H; Meyer M; Gilleaudeau GJ; Kaufman AJ; Anbar AD
    Sci Adv; 2018 Jun; 4(6):eaan8983. PubMed ID: 29938217
    [TBL] [Abstract][Full Text] [Related]  

  • 37. What the ~1.4 Ga Xiamaling Formation can and cannot tell us about the mid-Proterozoic ocean.
    Diamond CW; Planavsky NJ; Wang C; Lyons TW
    Geobiology; 2018 May; 16(3):219-236. PubMed ID: 29577549
    [TBL] [Abstract][Full Text] [Related]  

  • 38. Eutrophication, microbial-sulfate reduction and mass extinctions.
    Schobben M; Stebbins A; Ghaderi A; Strauss H; Korn D; Korte C
    Commun Integr Biol; 2016; 9(1):e1115162. PubMed ID: 27066181
    [TBL] [Abstract][Full Text] [Related]  

  • 39. Persistent global marine euxinia in the early Silurian.
    Stockey RG; Cole DB; Planavsky NJ; Loydell DK; Frýda J; Sperling EA
    Nat Commun; 2020 Apr; 11(1):1804. PubMed ID: 32286253
    [TBL] [Abstract][Full Text] [Related]  

  • 40. Isotopic evidence of environmental changes during the Devonian-Carboniferous transition in South China and its implications for the biotic crisis.
    Cao H; Hu L; Wang Z; He W; Chen F; Hou Q; Chen C
    Geobiology; 2023 Sep; 21(5):592-611. PubMed ID: 37194680
    [TBL] [Abstract][Full Text] [Related]  

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