Abstract

Between September, 1976 and July, 1977 Phaeodactylum tricornutum Bohlin was replaced as the dominant species by Skeletonema costatum (Grev) Cleve as temperatures fell below 10°C in the fall in an outdoor pond supplied with a mixture of waste water and sea water. Phaeodactylum tricornutum returned in the spring as the major species when temperatures rose above 10°C. In an adjacent pond in which only nitrogen and phosphorus were added in excess, however, P. tricornutum dominated throughout the entire study period even through the temperature varied between 0 and 25°C. We suspected that the difference inspecies dominance in the two ponds occurred because Skeletonema costatum requires silicon, which was present in sufficient quantities only in the waste-water-enriched pond. whereas Phaeodatylum tricornutum does not have a specififc requirement for this nutrient. The cellular chemical composition of P. tricornutum varied in a U-shaped fashion with changing temperature: minimum values for the cellular carbon, nitrogen, and chlorophyll contents were displayed at 15–20°C and maximum values at 3 and 15°C. Both the cellular carbon: nitrogen and carbon: chlorophyll ratios by weight were invariant with changing temperatures at ≈6: 1 and 50: 1 respectively, indicating nutrient saturation. Only under conditionsof nutrient saturation, which can be established in various ways, can the influence of temperature on phytoplankton physiology be separated from nutrient-related factors.

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