Near-surface Heating of Young Rift Sediment Causes Mass Production and Discharge of Reactive Dissolved Organic Matter

Ocean margin sediments have been considered as important sources of dissolved organic carbon (DOC) to the deep ocean, yet the contribution from advective settings has just started to be acknowledged. Here we present evidence showing that near-surface heating of sediment in the Guaymas Basin, a young...

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Detalles Bibliográficos
Autores principales: Lin, Yu-Shih, Koch, Boris P., Feseker, Tomas, Ziervogel, Kai, Goldhammer, Tobias, Schmidt, Frauke, Witt, Matthias, Kellermann, Matthias Y., Zabel, Matthias, Teske, Andreas, Hinrichs, Kai-Uwe
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5361187/
https://www.ncbi.nlm.nih.gov/pubmed/28327661
http://dx.doi.org/10.1038/srep44864

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5361187/
https://www.ncbi.nlm.nih.gov/pubmed/28327661
http://dx.doi.org/10.1038/srep44864

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