Significance of nanophytoplankton photosynthesis and primary production ina coastal upwelling system (Ria de Vigo, NW Spain)

Citation
Gh. Tilstone et al., Significance of nanophytoplankton photosynthesis and primary production ina coastal upwelling system (Ria de Vigo, NW Spain), MAR ECOL-PR, 183, 1999, pp. 13-27
Citations number
80
Categorie Soggetti
Aquatic Sciences
Journal title
MARINE ECOLOGY-PROGRESS SERIES
ISSN journal
01718630 → ACNP
Volume
183
Year of publication
1999
Pages
13 - 27
Database
ISI
SICI code
0171-8630(1999)183:<13:SONPAP>2.0.ZU;2-I
Abstract
The Rias Baixas are reported to have the highest primary production along t he NW coast of Spain due to the influence of upwelling, which occurs from A pril to October. Samples were taken over 2 wk periods at a single station i n the Ria de Vigo during spring, summer and autumn 1993 to study the variat ion in the phytoplankton photosynthetic parameters (light limited slope, al pha(B) and light saturated chlorophyll specific rate, P-m(B)) and daily pri mary production in relation to phytoplankton size class, species and hydrog raphic parameters. The range in primary production for the Ria was 65 to 36 89 mg C m(-2) d(-1) for total phytoplankton, 65 to 2533 mg C m(-2) d(-1) fo r net phytoplankton and 0 to 1650 mg C m(-2) d(-1) for nanophytoplankton. T he data suggest that most of the variation in primary production in the Ria during the upwelling season was due to nanophytoplankton. Upwelling/downwe lling cycles in the Ria therefore give rise to a larger variation in energy transfer through the microbial loop than through the classic, short, food chain. This is caused mainly by increases in nanophytoplankton aB coupled w ith high NO3 due to upwelling events. The data also suggest that there are 3 principal factors that give high primary production in the Ria. Periodic relaxation and stratification events linked to water column heating during upwelling/downwelling cycles coincided with periods of high productivity. S ize class also influences the primary production; net phytoplankton had sig nificantly higher primary production during the upwelling season than the n anophytoplankton and was responsible for 66% of the mean primary production . Species differences affected the primary production in the Ria; highest v alues coincided with blooms of Chaetoceros spp, and the lowest with dinofla gellate blooms of Gymnodinium catenatum.