Geochemical consequences of oxygen diffusion from the oceanic crust into overlying sediments and its significance for biogeochemical cycles based on sediments of the northeast Pacific

<p>Exchange of dissolved substances at the sediment–water interface provides an important link between the short-term and long-term geochemical cycles in the ocean. A second, as yet poorly understood sediment–water exchange is supported by low-temperature circulation of seawater through the oc...

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Bibliographic Details
Main Authors: G. J. M. Versteegh, A. Koschinsky, T. Kuhn, I. Preuss, S. Kasten
Format: Article
Language:English
Published: Copernicus Publications 2021-09-01
Series:Biogeosciences
Online Access:https://bg.copernicus.org/articles/18/4965/2021/bg-18-4965-2021.pdf