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An approach for particle sinking velocity measurements in the 3–400 μm size range and considerations on the effect of temperature on sinking rates

The flux of organic particles below the mixed layer is one major pathway of carbon from the surface into the deep ocean. The magnitude of this export flux depends on two major processes—remineralization rates and sinking velocities. Here, we present an efficient method to measure sinking velocities...

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Detalles Bibliográficos
Autores principales: Bach, Lennart Thomas, Riebesell, Ulf, Sett, Scarlett, Febiri, Sarah, Rzepka, Paul, Schulz, Kai Georg
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer-Verlag 2012
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3873053/
https://www.ncbi.nlm.nih.gov/pubmed/24391276
http://dx.doi.org/10.1007/s00227-012-1945-2

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