Adaptations of Gracilaria pacifica (Rhodophyta) to nitrogen procurement at different intertidal locations
Autor: | Paul Harrison, D. H. Turpin, T. E. Thomas |
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Rok vydání: | 1987 |
Předmět: |
education.field_of_study
Ecology Population chemistry.chemical_element Intertidal zone Aquatic Science Biology Nitrate reductase biology.organism_classification Nitrogen chemistry.chemical_compound chemistry Nitrate Algae Botany Ammonium Desiccation education Ecology Evolution Behavior and Systematics |
Zdroj: | Marine Biology. 93:569-580 |
ISSN: | 1432-1793 0025-3162 |
DOI: | 10.1007/bf00392795 |
Popis: | Nitrogen uptake, assimilation and accumulation were studied in three populations of Gracilaria pacifica Abbott in Bamfield Inlet, British Columbia, Canada, over three summers, 1979–1981. Two of these populations were in the intertidal one high and one low, and the third was a subtidal cultured population. Nitrate uptake rates, internal nitrate content and nitrate reductase activities were highest in the low intertidal population. Time-courses of uptake and uptake kinetics were studied. Both nitrate and ammonium were taken up simultaneously. Thalli from the high-intertidal population showed enhanced nitrate and ammonium uptake following mild desiccation, and greater tolerance to desiccation in terms of maintaining nitrogen uptake after severe desiccation. Transplants were made to determine the effect of intertidal height and geographic location on responses to desiccation, nitrogen uptake, assimilation and accumulation. Nitrate and ammonium uptake rates were dependent on intertidal height and geographic location. Transplanting up the intertidal increased nitrate uptake and nitrate reductase activity, but decreased the nitrate content of the thalli. There were few significant differences in ammonium uptake rates, and ammonium, amino acid, and soluble-protein content of the various populations. All high-intertidal populations, transplanted or natural, showed enhanced nitrate uptake rates following desiccation. Enhanced ammonium uptake rates following desiccation were restricted to the high-intertidal thalli in only one geographic location. Tolerance to higher levels of desiccation also appeared to be intertidal height-dependent, but required more than five weeks to fully develop or disappear. |
Databáze: | OpenAIRE |
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