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Preferential depletion of zinc within Costa Rica upwelling dome creates conditions for zinc co-limitation of primary production
The Costa Rica Dome (CRD) is a wind-driven feature characterized by high primary production and an unusual cyanobacterial bloom in surface waters. It is not clear whether this bloom arises from top-down or bottom-up processes. Several studies have argued that trace metal geochemistry within the CRD...
Uloženo v:
| Vydáno v: | J Plankton Res |
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| Hlavní autoři: | , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Oxford University Press
2016
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4889994/ https://ncbi.nlm.nih.gov/pubmed/27275028 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1093/plankt/fbw018 |
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