Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the “dolomite problem”

Paleozoic and Precambrian sedimentary successions frequently contain massive dolomicrite [CaMg(CO(3))(2)] units despite kinetic inhibitions to nucleation and precipitation of dolomite at Earth surface temperatures (<60 °C). This paradoxical observation is known as the “dolomite problem.” Accordin...

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Publicado en:Proc Natl Acad Sci U S A
Autores principales: Chang, Biao, Li, Chao, Liu, Deng, Foster, Ian, Tripati, Aradhna, Lloyd, Max K., Maradiaga, Ingrid, Luo, Genming, An, Zhihui, She, Zhenbing, Xie, Shucheng, Tong, Jinnan, Huang, Junhua, Algeo, Thomas J., Lyons, Timothy W., Immenhauser, Adrian
Formato: Artigo
Lenguaje:Inglês
Publicado: National Academy of Sciences 2020
Materias:
Physical Sciences
Acceso en línea:https://ncbi.nlm.nih.gov/pmc/articles/PMC7321997/
https://ncbi.nlm.nih.gov/pubmed/32513736
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1916673117
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