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.
139 related articles for article (PubMed ID: 36200974)
1. The deposition and significance of an Ediacaran non-glacial iron formation. Yang X; Mao J; Li R; Jiang Z; Yu M; Xu L; Reershemius T; Planavsky NJ Geobiology; 2023 Jan; 21(1):44-65. PubMed ID: 36200974 [TBL] [Abstract][Full Text] [Related]
2. Highly Siderophile Elements and Coupled Fe-Os Isotope Signatures in the Temagami Iron Formation, Canada: Possible Signatures of Neoarchean Seawater Chemistry and Earth's Oxygenation History. Schulz T; Viehmann S; Hezel DC; Koeberl C; Bau M Astrobiology; 2021 Aug; 21(8):924-939. PubMed ID: 34406808 [TBL] [Abstract][Full Text] [Related]
3. Biologically recycled continental iron is a major component in banded iron formations. Li W; Beard BL; Johnson CM Proc Natl Acad Sci U S A; 2015 Jul; 112(27):8193-8. PubMed ID: 26109570 [TBL] [Abstract][Full Text] [Related]
4. A stratified redox model for the Ediacaran ocean. Li C; Love GD; Lyons TW; Fike DA; Sessions AL; Chu X Science; 2010 Apr; 328(5974):80-3. PubMed ID: 20150442 [TBL] [Abstract][Full Text] [Related]
5. Products of the iron cycle on the early Earth. Tosca NJ; Jiang CZ; Rasmussen B; Muhling J Free Radic Biol Med; 2019 Aug; 140():138-153. PubMed ID: 31071438 [TBL] [Abstract][Full Text] [Related]
8. Earth's youngest banded iron formation implies ferruginous conditions in the Early Cambrian ocean. Li ZQ; Zhang LC; Xue CJ; Zheng MT; Zhu MT; Robbins LJ; Slack JF; Planavsky NJ; Konhauser KO Sci Rep; 2018 Jul; 8(1):9970. PubMed ID: 29967405 [TBL] [Abstract][Full Text] [Related]
9. 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]
10. Low oxygen levels with high redox heterogeneity in the late Ediacaran shallow ocean: Constraints from I/(Ca + Mg) and Ce/Ce* of the Dengying Formation, South China. Ding Y; Sun W; Liu S; Xie J; Tang D; Zhou X; Zhou L; Li Z; Song J; Li Z; Xu H; Tang P; Liu K; Li W; Chen D Geobiology; 2022 Nov; 20(6):790-809. PubMed ID: 36250398 [TBL] [Abstract][Full Text] [Related]
11. 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]
12. Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater. Swanner ED; Maisch M; Wu W; Kappler A Sci Rep; 2018 Mar; 8(1):4238. PubMed ID: 29523861 [TBL] [Abstract][Full Text] [Related]
13. Geochemical Characteristics of Trace Elements and Mineralization Model of the Ediacaran-Early Cambrian Phosphorites, South China. Zhang L; Zhang M; Zhu G ACS Omega; 2024 Mar; 9(12):13483-13493. PubMed ID: 38559950 [TBL] [Abstract][Full Text] [Related]
14. Microaerophilic Fe-oxidizing micro-organisms in Middle Jurassic ferruginous stromatolites and the paleoenvironmental context of their formation (Southern Carpathians, Romania). Grădinaru M; Lazăr I; Ducea MN; Petrescu L Geobiology; 2020 May; 18(3):366-393. PubMed ID: 31944551 [TBL] [Abstract][Full Text] [Related]
15. Isotopic reconstruction of iron oxidation-reduction process based on an Archean Ocean analogue. Yang X; Guo Q; Boyko V; Avetisyan K; Findlay AJ; Huang F; Wang Z; Chen Z Sci Total Environ; 2022 Apr; 817():152609. PubMed ID: 34963590 [TBL] [Abstract][Full Text] [Related]
16. Carbonate petrography, kerogen distribution, and carbon and oxygen isotope variations in an early Proterozoic transition from limestone to iron-formation deposition, Transvaal Supergroup, South Africa. Beukes NJ; Klein C; Kaufman AJ; Hayes JM Econ Geol; 1990; 85(4):663-90. PubMed ID: 11538478 [TBL] [Abstract][Full Text] [Related]
17. Microbial production of isotopically light iron(II) in a modern chemically precipitated sediment and implications for isotopic variations in ancient rocks. Tangalos GE; Beard BL; Johnson CM; Alpers CN; Shelobolina ES; Xu H; Konishi H; Roden EE Geobiology; 2010 Jun; 8(3):197-208. PubMed ID: 20374296 [TBL] [Abstract][Full Text] [Related]