Cargando…
Homogeneous sulfur isotope signature in East Antarctica and implication for sulfur source shifts through the last glacial-interglacial cycle
Sulfate aerosol (SO(4)(2−)) preserved in Antarctic ice cores is discussed in the light of interactions between marine biological activity and climate since it is mainly sourced from biogenic emissions from the surface ocean and scatters solar radiation during traveling in the atmosphere. However, th...
Autores principales: | Ishino, Sakiko, Hattori, Shohei, Savarino, Joel, Legrand, Michel, Albalat, Emmanuelle, Albarede, Francis, Preunkert, Susanne, Jourdain, Bruno, Yoshida, Naohiro |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6711983/ https://www.ncbi.nlm.nih.gov/pubmed/31455786 http://dx.doi.org/10.1038/s41598-019-48801-1 |
Ejemplares similares
-
A simple and reliable method reducing sulfate to sulfide for multiple sulfur isotope analysis
por: Geng, Lei, et al.
Publicado: (2018) -
Early sea ice decline off East Antarctica at the last glacial–interglacial climate transition
por: Sadatzki, Henrik, et al.
Publicado: (2023) -
Constraining the atmospheric OCS budget from sulfur isotopes
por: Hattori, Shohei, et al.
Publicado: (2020) -
Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial
por: Stein, Ruediger, et al.
Publicado: (2017) -
Neodymium isotope evidence for glacial-interglacial variability of deepwater transit time in the Pacific Ocean
por: Hu, Rong, et al.
Publicado: (2018)