The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum

Marine sediment records suggest that episodes of major atmospheric CO(2) drawdown during the last glacial period were linked to iron (Fe) fertilization of subantarctic surface waters. The principal source of this Fe is thought to be dust transported from southern mid-latitude deserts. However, uncer...

Descripción completa

Detalles Bibliográficos
Autores principales: Frisia, Silvia, Weyrich, Laura S., Hellstrom, John, Borsato, Andrea, Golledge, Nicholas R., Anesio, Alexandre M., Bajo, Petra, Drysdale, Russell N., Augustinus, Paul C., Rivard, Camille, Cooper, Alan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5472753/
https://www.ncbi.nlm.nih.gov/pubmed/28598412
http://dx.doi.org/10.1038/ncomms15425

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5472753/
https://www.ncbi.nlm.nih.gov/pubmed/28598412
http://dx.doi.org/10.1038/ncomms15425

Ejemplares similares