'Phyto-convection': the role of oceanic convection in primary production
'Phyto-convection': the role of oceanic convection in primary production
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Publisher
Oldendorf: Inter-Research
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Language
English
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Oldendorf: Inter-Research
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Contents
Typical sinking rates of marine phytoplankton cover a range extending from a few meters up to several hundred meters.per day. If it were not for a process which maintains plankton near the sea surface, in the euphotic layer, it would sink to depths of thousands of meters in the deep ocean during the winter season. Consequently, plankton would not b...
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Full title
'Phyto-convection': the role of oceanic convection in primary production
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TN_cdi_proquest_miscellaneous_17627138
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_17627138
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ISSN
0171-8630
E-ISSN
1616-1599
DOI
10.3354/meps189077