Seasonal dynamics and potential fate of size-fractionated phytoplankton ina temperate nearshore environment (Western Gulf of St Lawrence, Canada)

Citation
E. Tamigneaux et al., Seasonal dynamics and potential fate of size-fractionated phytoplankton ina temperate nearshore environment (Western Gulf of St Lawrence, Canada), EST COAST S, 48(2), 1999, pp. 253-269
Citations number
76
Categorie Soggetti
Aquatic Sciences
Journal title
ESTUARINE COASTAL AND SHELF SCIENCE
ISSN journal
02727714 → ACNP
Volume
48
Issue
2
Year of publication
1999
Pages
253 - 269
Database
ISI
SICI code
0272-7714(199902)48:2<253:SDAPFO>2.0.ZU;2-U
Abstract
Environmental conditions and seasonal dynamics of the <5 and >5 mu m phytop lankton were monitored in a temperate nearshore environment (Baie des Chale urs, western Gulf of St Lawrence, Canada). Following the spring bloom, ther e was a sharp decrease in the contribution of >5 mu m phytoplankton to the chlorophyl a biomass and primary production, so that the <5 mu m fraction a ccounted for up to 80-90% of both biomass and production throughout the sum mer. Strong summer stratification prevented wind-driven mixing and nutrient replenishment by transient upwelling events. The compensation depth for ph ytoplankton growth was close to the less than or equal to 25 m bottom, so t hat only cells growing near the bottom could have been limited by light. In spite of the high production of <5 mu m phytoplankton (>0.5 g C m(-2) d(-1 )), their biomass remained relatively constant, which is indicative of a ti ght balance between production and export, involving active microbial grazi ng. Production per unit biomass of >5 mu m phytoplankton [8-126 mg C (mg Ch lorophyll a d)(-1)] was generally higher than that of the small size fracti on [13-56 mg C (mg Chlorophyll a d)(-1)], suggesting active photosynthesis by the former. Seasonal changes in size-fractionated production and biomass indicate that > 5 mu m phytoplankton experienced intense export. This is c onsistent with the accumulation of large cells with low photosynthetic effi ciency near the bottom during the period of strong stratification, probably resulting from the sinking of intact phytoplankton. In addition, there is indirect evidence of mesozooplankton grazing on large phytoplankton during summer. The coexistence of microbial and herbivorous feeding modes during s ummer corresponds to a multivorous food web. (C) 1999 Academic Press.