Autor: |
E. L. Cavan, M. Trimmer, F. Shelley, R. Sanders |
Jazyk: |
angličtina |
Rok vydání: |
2017 |
Předmět: |
|
Zdroj: |
Nature Communications, Vol 8, Iss 1, Pp 1-9 (2017) |
Druh dokumentu: |
article |
ISSN: |
2041-1723 |
DOI: |
10.1038/ncomms14847 |
Popis: |
The downward transfer of organic carbon from the surface to the deep ocean is increased in oxygen minimum zones relative to oxic waters. Here, the authors show reduced interactions of zooplankton with sinking particles owing to low oxygen are likely the primary reason for the observed high transfer of carbon. |
Databáze: |
Directory of Open Access Journals |
Externí odkaz: |
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