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'Phyto-convection': the role of oceanic convection in primary production

'Phyto-convection': the role of oceanic convection in primary production

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_17627138

'Phyto-convection': the role of oceanic convection in primary production

About this item

Full title

'Phyto-convection': the role of oceanic convection in primary production

Publisher

Oldendorf: Inter-Research

Journal title

Marine ecology. Progress series (Halstenbek), 1999-11, Vol.189, p.77-92

Language

English

Formats

Publication information

Publisher

Oldendorf: Inter-Research

More information

Scope and Contents

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...

Alternative Titles

Full title

'Phyto-convection': the role of oceanic convection in primary production

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_17627138

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_17627138

Other Identifiers

ISSN

0171-8630

E-ISSN

1616-1599

DOI

10.3354/meps189077

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