1990
DOI: 10.1016/0272-7714(90)90105-z
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Phytoplankton seed populations of the Cape Peninsula upwelling plume, with particular reference to resting spores of Chaetoceros (bacillariophyceae) and their role in seeding upwelling waters

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Cited by 84 publications
(64 citation statements)
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“…Although the ecologically relevant time scales of adaptation pertain to natural, mixed-species phytoplankton assemblages, successional changes in species composition of the assemblage during a bloom event (Chavez et al 1990;Pitcher 1990) may obscure the analysis of events controlling molecular and physiological processes sensitive to changing environments. In contrast, the experimental approach used here enabled precise observations of the physiological, biochemical, and molecular responses of N-stressed S. costatum cells to improved conditions of light and N03-availability simulating a brief upwelling pulse.…”
Section: Discussionmentioning
confidence: 99%
“…Although the ecologically relevant time scales of adaptation pertain to natural, mixed-species phytoplankton assemblages, successional changes in species composition of the assemblage during a bloom event (Chavez et al 1990;Pitcher 1990) may obscure the analysis of events controlling molecular and physiological processes sensitive to changing environments. In contrast, the experimental approach used here enabled precise observations of the physiological, biochemical, and molecular responses of N-stressed S. costatum cells to improved conditions of light and N03-availability simulating a brief upwelling pulse.…”
Section: Discussionmentioning
confidence: 99%
“…Thus, those vegetative cells and, moreover, their resting stage cells, advected from coastal waters to the surface of the pelagic region (at least in the euphotic layer), might contribute to the initiation of annual blooms, as seed cells, in the KumanoNada. On the other hand, Pitcher (1990) suggested that the upwelling system of southern Benguela plays an important role to help the resting spores, distributed in the subsurface layer, to be brought back to the surface and act as seeds for their blooms. Takahashi et al (1977) also pointed out the possibility that water mass movements, such as upwelling and vertical mixing, could return sunken phytoplankton cells to the euphotic layer in the deep inlet of British Columbia, Canada.…”
Section: Figmentioning
confidence: 99%
“…In northern fjords, there are few planktonic cells left in the surface waters after the typically long, dark winters, and benthic resting stages are the most likely supply of cells for the spring diatom bloom (Eilertsen et al 1995). Resting stages are also an important inoculation source for bloom formation in upwelling areas, because the propagules are brought to the surface with nutrient-rich deep water (Pitcher et al 1993). In most temperate areas, however, it has been difficult to determine if spores actually seed diatom blooms, because fugitive vegetative cells may always be present in low numbers (Garrison 1981).…”
Section: Acknowledgmentsmentioning
confidence: 99%
“…In the East China Sea, storms resuspend resting stages in early spring, and these cells can grow to bloom proportions in about 1 week (Ishikawa et al 2001). Phytoplankton in the southern Benguela upwelling region are seeded by inoculations of diatom resting stages through upwelling (Pitcher 1990).…”
Section: Resuspension Of Resting Stages For Bloom Inoculation-mentioning
confidence: 99%