IR Home
MEPS
Home
Editors
Forthcoming
Information
Subscribe
Journals
Home
MEPS
AME
CR
DAO
ESEP
ESR
Search
Subscribe
Book Series
EE Books
Top Books
ESEP Books
Order
EEIU Brochures
(pdf format)
Discussion Forums
Home
Research
IR Research
Institutions
International Ecology Institute
Eco-Ethics International Union
Foundation
Otto Kinne Foundation
 |  |
MEPS 277:51-60 (2004)
|
Abstract
|

Annual phytoplankton production in a coastal lagoon of the southern California Current System
Martín A. Montes-Hugo1,2,*, Saúl Alvarez-Borrego-2, Gilberto Gaxiola-Castro-2
1División de Oceanología, CICESE, Km 107 Carretera Tijuana-Ensenada, Ensenada, Baja California, CP 22860, México
2Present address: EOS Laboratory, College of Marine Science, University of South Florida, 140 7th Avenue S, St. Petersburg, Florida 33701, USA
*Email: mmontes@mail.usf.edu

ABSTRACT: Seasonal and annual integrated phytoplankton production (AIP) of a shallow lagoon of the NW coast of Baja California, Estero de Punta Banda, was estimated during inverse-estuarine conditions in 1998 and 1999, a non-El Niño year. Estero de Punta
Banda is a coastal lagoon with no city/industrial waste input; its primary production is comparable to that of impacted coastal bodies such as those in the Southern California area. To calculate AIP, we used representative averages of chlorophyll a
concentration for 2 regions within the lagoon (outer and inner), representative averages of the photosynthetic parameters, an atmospheric model to estimate photosynthetically available radiation (PAR), and multiple linear regression models for the
vertical attenuation coefficient of PAR (KPAR) as a function of wind speed and tidal range. The seasonal average daily integrated primary production was highest in summer (880 and 47 mgC m-2 d-1 for the outer and
inner regions, respectively), due to higher temperature and light levels, as is generally reported for other temperate estuaries. Values in winter were about half those in summer. Average AIP for the whole lagoon (125 gC m-2 yr-1)
was relatively low compared with estimates for larger, deeper and/or sewage-enriched coastal water bodies. This was mainly due to the shallow integration depth of AIP in our study area and to high turbidity caused by tidal currents and wind waves.
KEY WORDS: Coastal lagoon · Phytoplankton · Modeled primary production · Southern California Current System
Full text in pdf format

Published in MEPS Vol.
277
(2004) on August 16
Print ISSN: 0171-8630; Online ISSN: 1616-1599.
Copyright © Inter-Research, Oldendorf/Luhe, 2004
|