192 related articles for article (PubMed ID: 25684783)
1. 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]
2. 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]
3. Geochemical evidence for widespread euxinia in the later Cambrian ocean.
Gill BC; Lyons TW; Young SA; Kump LR; Knoll AH; Saltzman MR
Nature; 2011 Jan; 469(7328):80-3. PubMed ID: 21209662
[TBL] [Abstract][Full Text] [Related]
4. Abrupt global-ocean anoxia during the Late Ordovician-early Silurian detected using uranium isotopes of marine carbonates.
Bartlett R; Elrick M; Wheeley JR; Polyak V; Desrochers A; Asmerom Y
Proc Natl Acad Sci U S A; 2018 Jun; 115(23):5896-5901. PubMed ID: 29784792
[TBL] [Abstract][Full Text] [Related]
5. Carbonate uranium isotopes record global expansion of marine anoxia during the Toarcian Oceanic Anoxic Event.
Remírez MN; Gilleaudeau GJ; Gan T; Kipp MA; Tissot FLH; Kaufman AJ; Parente M
Proc Natl Acad Sci U S A; 2024 Jul; 121(27):e2406032121. PubMed ID: 38913904
[TBL] [Abstract][Full Text] [Related]
6. Evidence for the development of local anoxia during the Cambrian SPICE event in eastern North America.
LeRoy MA; Gill BC
Geobiology; 2019 Jul; 17(4):381-400. PubMed ID: 30729650
[TBL] [Abstract][Full Text] [Related]
7. Thallium isotopes reveal protracted anoxia during the Toarcian (Early Jurassic) associated with volcanism, carbon burial, and mass extinction.
Them TR; Gill BC; Caruthers AH; Gerhardt AM; Gröcke DR; Lyons TW; Marroquín SM; Nielsen SG; Trabucho Alexandre JP; Owens JD
Proc Natl Acad Sci U S A; 2018 Jun; 115(26):6596-6601. PubMed ID: 29891692
[TBL] [Abstract][Full Text] [Related]
8. 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]
9. 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]
10. Constraining oceanic oxygenation during the Shuram excursion in South China using thallium isotopes.
Fan H; Nielsen SG; Owens JD; Auro M; Shu Y; Hardisty DS; Horner TJ; Bowman CN; Young SA; Wen H
Geobiology; 2020 May; 18(3):348-365. PubMed ID: 32011800
[TBL] [Abstract][Full Text] [Related]
11. 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]
12. Paleo-marine redox environment fluctuation during the early Cambrian: Insight from iron isotope in the Tarim Basin, China.
Ai Y; Zhu G; Li T; Zhang Z; Zhang Y; Duan P; Liu J; Zhao K; Li X
Sci Total Environ; 2024 Feb; 912():169277. PubMed ID: 38110098
[TBL] [Abstract][Full Text] [Related]
13. Pulse of atmospheric oxygen during the late Cambrian.
Saltzman MR; Young SA; Kump LR; Gill BC; Lyons TW; Runnegar B
Proc Natl Acad Sci U S A; 2011 Mar; 108(10):3876-81. PubMed ID: 21368152
[TBL] [Abstract][Full Text] [Related]
14. A new model for atmospheric oxygen over Phanerozoic time.
Berner RA; Canfield DE
Am J Sci; 1989 Apr; 289(4):333-61. PubMed ID: 11539776
[TBL] [Abstract][Full Text] [Related]
15. Isotopic compositions of carbonates and organic carbon from upper Proterozoic successions in Namibia: stratigraphic variation and the effects of diagenesis and metamorphism.
Kaufman AJ; Hayes JM; Knoll AH; Germs GJ
Precambrian Res; 1991; 49():301-27. PubMed ID: 11538647
[TBL] [Abstract][Full Text] [Related]
16. Bioturbation and directionality in Earth's carbon isotope record across the Neoproterozoic-Cambrian transition.
Boyle RA; Dahl TW; Bjerrum CJ; Canfield DE
Geobiology; 2018 May; 16(3):252-278. PubMed ID: 29498810
[TBL] [Abstract][Full Text] [Related]
17. Oceanic oxygenation events in the anoxic Ediacaran ocean.
Sahoo SK; Planavsky NJ; Jiang G; Kendall B; Owens JD; Wang X; Shi X; Anbar AD; Lyons TW
Geobiology; 2016 Sep; 14(5):457-68. PubMed ID: 27027776
[TBL] [Abstract][Full Text] [Related]
18. An enormous sulfur isotope excursion indicates marine anoxia during the end-Triassic mass extinction.
He T; Dal Corso J; Newton RJ; Wignall PB; Mills BJW; Todaro S; Di Stefano P; Turner EC; Jamieson RA; Randazzo V; Rigo M; Jones RE; Dunhill AM
Sci Adv; 2020 Sep; 6(37):. PubMed ID: 32917684
[TBL] [Abstract][Full Text] [Related]
19. Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy of the Ediacaran Lantian Formation in South China: Spatial gradient, ocean redox oscillation, and fossil distribution.
Wang W; Guan C; Zhou C; Peng Y; Pratt LM; Chen X; Chen L; Chen Z; Yuan X; Xiao S
Geobiology; 2017 Jul; 15(4):552-571. PubMed ID: 28063179
[TBL] [Abstract][Full Text] [Related]
20. 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]
[Next] [New Search]
