1997
DOI: 10.1093/plankt/19.3.319
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Relationships between phytoplankton dynamics and the availability of light and nutrients in a shallow sub-tropical lake

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Cited by 97 publications
(46 citation statements)
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“…Given the affinity of cyanobacteria and other primary producers for NH 4 ? , it is surprising that nutrient limitation bioassays conducted on natural phytoplankton assemblages often use only NO 3 -as the N source (e.g., Aldridge et al 1995;Phlips et al 1997). It seems possible that using only NO 3 -could underestimate the potential degree of N limitation, particularly if cyanobacteria are a significant fraction of the phytoplankton community.…”
Section: Introductionmentioning
confidence: 99%
“…Given the affinity of cyanobacteria and other primary producers for NH 4 ? , it is surprising that nutrient limitation bioassays conducted on natural phytoplankton assemblages often use only NO 3 -as the N source (e.g., Aldridge et al 1995;Phlips et al 1997). It seems possible that using only NO 3 -could underestimate the potential degree of N limitation, particularly if cyanobacteria are a significant fraction of the phytoplankton community.…”
Section: Introductionmentioning
confidence: 99%
“…However, evidence supporting the importance of DIN in cyanobacterial bloom formation is equivocal: Lathrop (1988) found that additions of NH 4 ? and NO 3 -did not prevent blooms of Microcystis, Stockner and Shortreed (1988) added NH 4 ? and NO 3 -to an oligotrophic lake with low N:P and stimulated a bloom of Anabaena, whereas Varis et al (1989) found a negative relationship for several cyanobacteria species (including A. flos-aquae) and ammonia, and Philips et al (1997) found decreasing levels of DIN corresponding to cyanobacterial blooms. The similar temporal pattern of N-deficiency in both lakes also suggests that nitrogen deficiency was not a principal factor in the different composition of the autumn forming bloom species.…”
Section: Discussionmentioning
confidence: 97%
“…The pelagic region (1,400 km 2 ) of this lake is comprised of: (a) a deeper (up to 5 m), turbid central zone with sediments of unconsolidated mud, phosphorus-rich water, and a low phytoplankton biomass (Olila and Reddy, 1993;Phlips et al, 1997); (b) a shallower (2-3 m) mud-bottomed north zone, which receives large inputs of phosphorus from nearby tributaries and often has phytoplankton blooms (Havens et al, 1994); and (c) sand and peatbottomed south and west zones, located between the pelagic and littoral regions. At the interface of these pelagic and littoral zones, the underwater irradiance is favorable both for phytoplankton and periphyton growth (Phlips et al, 1993).…”
Section: Study Sitementioning
confidence: 99%