Cargando…
A sluggish mid‐Proterozoic biosphere and its effect on Earth's redox balance
The possibility of low but nontrivial atmospheric oxygen (O(2)) levels during the mid‐Proterozoic (between 1.8 and 0.8 billion years ago, Ga) has important ramifications for understanding Earth's O(2) cycle, the evolution of complex life and evolving climate stability. However, the regulatory m...
Autores principales: | Ozaki, Kazumi, Reinhard, Christopher T., Tajika, Eiichi |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
John Wiley and Sons Inc.
2018
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6585969/ https://www.ncbi.nlm.nih.gov/pubmed/30281196 http://dx.doi.org/10.1111/gbi.12317 |
Ejemplares similares
-
A case for an active eukaryotic marine biosphere during the Proterozoic era
por: Eckford-Soper, Lisa K., et al.
Publicado: (2022) -
Diagenetic nutrient supplies to the Proterozoic biosphere archived in divergent nitrogen isotopic ratios between kerogen and silicate minerals
por: Stüeken, Eva E., et al.
Publicado: (2022) -
Extreme sensitivity in Snowball Earth formation to mountains on PaleoProterozoic supercontinents
por: Walsh, Amber, et al.
Publicado: (2019) -
Triple oxygen isotope constraints on atmospheric O(2) and biological productivity during the mid-Proterozoic
por: Liu, Peng, et al.
Publicado: (2021) -
Mr Sluggish Schizophrenia
por: van Voren, Robert
Publicado: (2021)