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Temporal variation of particulate organic carbon flux at the mouth of Tokyo Bay
A sediment trap experiment was conducted at a depth of 750 m at the mouth of Tokyo Bay to clarify the quantity and transport process of particles from the bay to the open ocean. The high total mass flux (8.7 ± 4.5 g m(–2) d(–1)) suggests that the particles not only originate in the surface layer rig...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Springer Nature Singapore
2022
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9387886/ https://www.ncbi.nlm.nih.gov/pubmed/36000070 http://dx.doi.org/10.1007/s10872-022-00660-7 |