Cargando…
The coupling of Phanerozoic continental weathering and marine phosphorus cycle
Organic matter production and decomposition primarily modulate the atmospheric O(2) and CO(2) levels. The long term marine primary productivity is controlled by the terrestrial input of phosphorus (P), while the marine P cycle would also affect organic matter production. In the past 540 million year...
Autores principales: | Wang, Ruimin, Lang, Xianguo, Ding, Weiming, Liu, Yarong, Huang, Tianzheng, Tang, Wenbo, Shen, Bing |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2020
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7118102/ https://www.ncbi.nlm.nih.gov/pubmed/32242080 http://dx.doi.org/10.1038/s41598-020-62816-z |
Ejemplares similares
-
The effects of marine eukaryote evolution on phosphorus, carbon and oxygen cycling across the Proterozoic–Phanerozoic transition
por: Lenton, Timothy M., et al.
Publicado: (2018) -
Continental flood basalts drive Phanerozoic extinctions
por: Green, Theodore, et al.
Publicado: (2022) -
Dataset of Phanerozoic continental climate and Köppen–Geiger climate classes
por: Pohl, Alexandre, et al.
Publicado: (2022) -
Continental flood basalts do not drive later Phanerozoic extinctions
por: Henehan, Michael J., et al.
Publicado: (2023) -
Diversity partitioning in Phanerozoic benthic marine communities
por: Hofmann, Richard, et al.
Publicado: (2019)