Phytoplankton motility and the competition for nutrients in the thermocline

Ross, O. N.; Sharples, J. 2007 Phytoplankton motility and the competition for nutrients in the thermocline. Marine Ecology - Progress Series, 347. 21-38. 10.3354/meps06999

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Abstract/Summary

Diatoms and dinoflagellates are 2 important groups of phytoplankton that co-exist in the competition for light and nutrients. Following the diatom-dominated spring bloom, the shelf sea subsurface chlorophyll maximum (SCM) is often dominated by motile species of phytoplankton, in particular dinoflagellates and sometimes coccolithophores. Turbulence in shelf seas, driven by surface winds and by tidal currents, is likely to easily counteract the typically weak swimming capabilities of phytoplankton. The thermocline marks a low turbulence region, separating the nutrient-depleted surface (wind-mixed) layer and the nutrient-replete bottom (tidally-mixed) layer, and so would seem to be an ideal environment for employing a strategy of vertical migration. However, the positioning within the thermocline is crucial, as turbulence in the adjoining boundary layers removes cells that stray too close to the edges of the thermocline and mixes them into resource-limited layers of the water column. We combined a Lagrangian random walk model, a k-epsilon turbulence scheme and a simple photosynthesis model to track individual phytoplankton cells in a tidally-mixed, stratified water column (e.g. a summer, temperate shelf sea). By allowing motile and non-motile species to compete, we found that an ability to use motility to balance resource requirements can offset modest physiological disadvantages compared to the non-motile phytoplankton, leading to either co-existence or even dominance of the motile species. However, more severe physiological disadvantages (e.g. combinations of growth rate, nutrient uptake capabilities, and/or respiration) cannot be compensated for by motility alone, and further adaptations (such as mixotrophy) would be required. We also show that the SCM can be a place for significant new production (values of 1 g C m(-2) d(-1) and f-ratios of over 0.5 are possible), which stresses its potential importance as a source of food to the pelagic throughout summer

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.3354/meps06999
Programmes:	Oceans 2025 > Shelf and coastal processes
ISSN:	0171-8630
Additional Keywords:	OPM2007 NISCOCT07 AR0708 REF ISI HIJ JOURNAL UKUNIVCOAUTHOR AJWOCT07 THEME 3 WP 3.2 LLH3201 PHYTOPLANKTON SPECIES COMPETITION MOTILITY TIDAL MIXING SHELF SEA THERMOCLINE CARBON EXPORT NITROGEN FLUX F-RATIO TURBULENCE MODELLING LAGRANGIAN MODELLING CHLOROPHYLL MAXIMUM LAYERS RANDOM WALK MODELS VERTICAL DISTRIBUTION MARINE PHYTOPLANKTON TURBULENCE CLOSURE NORTH SEA LIGHT INTENSITY GROWTH RATES DYNAMICS OCEAN
NORA Subject Terms:	Marine Sciences
Date made live:	07 Oct 2008 13:50 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/2708

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