124 related articles for article (PubMed ID: 21087157)
1. The formation of sulfate and elemental sulfur aerosols under varying laboratory conditions: implications for early earth.
DeWitt HL; Hasenkopf CA; Trainer MG; Farmer DK; Jimenez JL; McKay CP; Toon OB; Tolbert MA
Astrobiology; 2010 Oct; 10(8):773-81. PubMed ID: 21087157
[TBL] [Abstract][Full Text] [Related]
2. Reduction in haze formation rate on prebiotic Earth in the presence of hydrogen.
DeWitt HL; Trainer MG; Pavlov AA; Hasenkopf CA; Aiken AC; Jimenez JL; McKay CP; Toon OB; Tolbert MA
Astrobiology; 2009 Jun; 9(5):447-53. PubMed ID: 19566425
[TBL] [Abstract][Full Text] [Related]
3. Haze aerosols in the atmosphere of early Earth: manna from heaven.
Trainer MG; Pavlov AA; Curtis DB; McKay CP; Worsnop DR; Delia AE; Toohey DW; Toon OB; Tolbert MA
Astrobiology; 2004; 4(4):409-19. PubMed ID: 15684721
[TBL] [Abstract][Full Text] [Related]
4. Follow the Carbon: Isotopic Labeling Studies of Early Earth Aerosol.
Hicks RK; Day DA; Jimenez JL; Tolbert MA
Astrobiology; 2016 Nov; 16(11):822-830. PubMed ID: 27870584
[TBL] [Abstract][Full Text] [Related]
5. Mass-independent fractionation of sulfur isotopes in Archean sediments: strong evidence for an anoxic Archean atmosphere.
Pavlov AA; Kasting JF
Astrobiology; 2002; 2(1):27-41. PubMed ID: 12449853
[TBL] [Abstract][Full Text] [Related]
6. Organic Haze as a Biosignature in Anoxic Earth-like Atmospheres.
Arney G; Domagal-Goldman SD; Meadows VS
Astrobiology; 2018 Mar; 18(3):311-329. PubMed ID: 29189040
[TBL] [Abstract][Full Text] [Related]
7. 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]
8. Nitrogen incorporation in CH(4)-N(2) photochemical aerosol produced by far ultraviolet irradiation.
Trainer MG; Jimenez JL; Yung YL; Toon OB; Tolbert MA
Astrobiology; 2012 Apr; 12(4):315-26. PubMed ID: 22519972
[TBL] [Abstract][Full Text] [Related]
9. Explaining the structure of the Archean mass-independent sulfur isotope record.
Halevy I; Johnston DT; Schrag DP
Science; 2010 Jul; 329(5988):204-7. PubMed ID: 20508089
[TBL] [Abstract][Full Text] [Related]
10. Five-S-isotope evidence of two distinct mass-independent sulfur isotope effects and implications for the modern and Archean atmospheres.
Lin M; Zhang X; Li M; Xu Y; Zhang Z; Tao J; Su B; Liu L; Shen Y; Thiemens MH
Proc Natl Acad Sci U S A; 2018 Aug; 115(34):8541-8546. PubMed ID: 30082380
[TBL] [Abstract][Full Text] [Related]
11. Sulphur isotope evidence for an oxic Archaean atmosphere.
Ohmoto H; Watanabe Y; Ikemi H; Poulson SR; Taylor BE
Nature; 2006 Aug; 442(7105):908-11. PubMed ID: 16929296
[TBL] [Abstract][Full Text] [Related]
12. Sulfur radical formation from the tropospheric irradiation of aqueous sulfate aerosols.
Cope JD; Bates KH; Tran LN; Abellar KA; Nguyen TB
Proc Natl Acad Sci U S A; 2022 Sep; 119(36):e2202857119. PubMed ID: 36037345
[TBL] [Abstract][Full Text] [Related]
13. Biogenic methane, hydrogen escape, and the irreversible oxidation of early Earth.
Catling DC; Zahnle KJ; McKay C
Science; 2001 Aug; 293(5531):839-43. PubMed ID: 11486082
[TBL] [Abstract][Full Text] [Related]
14. Pressure dependent aerosol formation from the cyclohexene gas-phase ozonolysis in the presence and absence of sulfur dioxide: a new perspective on the stabilisation of the initial clusters.
Carlsson PT; Dege JE; Keunecke C; Krüger BC; Wolf JL; Zeuch T
Phys Chem Chem Phys; 2012 Sep; 14(33):11695-705. PubMed ID: 22825796
[TBL] [Abstract][Full Text] [Related]
15. Anomalous fractionations of sulfur isotopes during thermochemical sulfate reduction.
Watanabe Y; Farquhar J; Ohmoto H
Science; 2009 Apr; 324(5925):370-3. PubMed ID: 19372427
[TBL] [Abstract][Full Text] [Related]
16. Aqueous-phase secondary organic aerosol and organosulfate formation in atmospheric aerosols: a modeling study.
McNeill VF; Woo JL; Kim DD; Schwier AN; Wannell NJ; Sumner AJ; Barakat JM
Environ Sci Technol; 2012 Aug; 46(15):8075-81. PubMed ID: 22788757
[TBL] [Abstract][Full Text] [Related]
17. Formation of nitrogenated organic aerosols in the Titan upper atmosphere.
Imanaka H; Smith MA
Proc Natl Acad Sci U S A; 2010 Jul; 107(28):12423-8. PubMed ID: 20616074
[TBL] [Abstract][Full Text] [Related]
18. Atmospheric evolution of sulfur emissions from Kı̅lauea: real-time measurements of oxidation, dilution, and neutralization within a volcanic plume.
Kroll JH; Cross ES; Hunter JF; Pai S; ; ; Wallace LM; Croteau PL; Jayne JT; Worsnop DR; Heald CL; Murphy JG; Frankel SL
Environ Sci Technol; 2015 Apr; 49(7):4129-37. PubMed ID: 25734883
[TBL] [Abstract][Full Text] [Related]
19. Atmospheric record in the Hadean Eon from multiple sulfur isotope measurements in Nuvvuagittuq Greenstone Belt (Nunavik, Quebec).
Thomassot E; O'Neil J; Francis D; Cartigny P; Wing BA
Proc Natl Acad Sci U S A; 2015 Jan; 112(3):707-12. PubMed ID: 25561552
[TBL] [Abstract][Full Text] [Related]
20. Recombination reactions as a possible mechanism of mass-independent fractionation of sulfur isotopes in the Archean atmosphere of Earth.
Babikov D
Proc Natl Acad Sci U S A; 2017 Mar; 114(12):3062-3067. PubMed ID: 28258172
[TBL] [Abstract][Full Text] [Related]
[Next] [New Search]
