Record Display for the EPA National Library Catalog

RECORD NUMBER: 1578 OF 1596

OLS Field Name OLS Field Data
Main Title What controls phytoplankton production in nutrient-rich areas of the open sea? /
Author Chisholm, Sallie W. ; Morel, F. M. M.
Other Authors
Author Title of a Work
Morel, Francois M. M.
CORP Author American Society of Limnology and Oceanography, Walla Walla, WA.;Environmental Research Lab., Narragansett, RI.
Publisher U.S. Environmental Protection Agency, Environmental Research Laboratory, Global Change Research Program,
Year Published 1991
Report Number EPA/600/R-93/120
Stock Number PB93-211985
Subjects Marine phytoplankton. ; Primary productivity (Biology)
Additional Subjects Phytoplankton ; Limnology ; Biological productivity ; Southern Ocean ; Pacific Ocean ; Arctic regions ; Nutrients ; Carbon dioxide cycle ; Global warming ; Atmosphere ; Biomass ; Deep water ; Inorganic nitrates ; Phosphates ; Organic compounds ; Surface waters ; Tables(Data) ; Greenhouse gases ; Biological pump
Holdings
Library Call Number Additional Info Location Last
Modified
Checkout
Status
NTIS  PB93-211985 Most EPA libraries have a fiche copy filed under the call number shown. Check with individual libraries about paper copy. NTIS 01/01/1988
Collation 489 pages ; 28 cm
Abstract
The oceans play a critical role in regulating the global carbon cycle. Deep-ocean waters are roughly 200% supersaturated with CO2 compared to surface waters, which are in contact with the atmosphere. The difference is due to the flux of photosynthetically derived organic material from surface to deep waters and its subsequent remineralization, i.e. the 'biological pump'. The pump is a complex phytoplankton-based ecosystem. It is driven by sunlight, and fueled by the supply of inorganic nutrients derived primarily from the deep ocean. In areas of the oceans where inorganic N and P are effectively exhausted by phytoplankton in surface waters during the growing season, the pump functions at maximal efficiency: The transport of carbon to depth is limited by the flux of N and P into the surface waters. In the Southern Ocean, near the equator, and in the subarctic Pacific, however, relatively high concentrations of nitrate and phosphate are found in the surface waters throughout the year, and phytoplankton biomass and net production are much lower than would be expected based on the availability of major nutrients. (Copyright (c) 1991, by the American Society of Limnology and Oceanography, Inc.)
Notes
"Entire peer reviewed volume was sponsored and supported by the EPA Global Change Program, Symposium-02/22-24/1991 San Marcos, CA. Limnology & Oceanography, 36(8), 1991." Microfiche.