1997
DOI: 10.1111/j.0022-3646.1997.00542.x
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NONDESTRUCTIVE TRACING OF MIGRATORY RHYTHMS OF INTERTIDAL BENTHIC MICROALGAE USING IN VIVO CHLOROPHYLL A FLUORESCENCE1,2

Abstract: In vivo chlorophyll (Chl) a fluorescence was measured in undisturbed intertidal sediments with the purpose of tracing the vertical migratory rhythms of benthic microalgae. A pulse amplitude jluorometer, an instrument which does not require physical contact with the sample, was

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Cited by 193 publications
(146 citation statements)
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“…The initial phase is an upward migration pulse beginning at least 2-3 h before the daytime emersion period and ending around the time when light exposure is expected to begin (t i ). Previous results that showed a peak of surface biomass occurring sometime after the beginning of tidal exposure (t Bmax > t i ) (Seroˆdio et al, 1997(Seroˆdio et al, , 2005 appear to be a particular case of the general pattern described here, since both studies refer to days when light exposure started with sunrise. Considering the lack of physical (light, temperature) or chemical gradients at the sediment-air interface (after prolonged darkness, the upper and lower layers both become uniformly anoxic), the accumulation of cells at the surface could be explained by an endogenous negative geotactic behaviour (Harper, 1977;Mitbavkar & Anil, 2004).…”
Section: Biofilm Formationsupporting
confidence: 66%
See 1 more Smart Citation
“…The initial phase is an upward migration pulse beginning at least 2-3 h before the daytime emersion period and ending around the time when light exposure is expected to begin (t i ). Previous results that showed a peak of surface biomass occurring sometime after the beginning of tidal exposure (t Bmax > t i ) (Seroˆdio et al, 1997(Seroˆdio et al, , 2005 appear to be a particular case of the general pattern described here, since both studies refer to days when light exposure started with sunrise. Considering the lack of physical (light, temperature) or chemical gradients at the sediment-air interface (after prolonged darkness, the upper and lower layers both become uniformly anoxic), the accumulation of cells at the surface could be explained by an endogenous negative geotactic behaviour (Harper, 1977;Mitbavkar & Anil, 2004).…”
Section: Biofilm Formationsupporting
confidence: 66%
“…Several studies have reported the endogenous nature of the vertical migratory behaviour of benthic microalgae, showing that the vertical movements continue for several days, synchronized with solar and tidal cycles, in the absence of external stimuli (Palmer & Round, 1967;Palmer, 1974;Seroˆdio et al, 1997). However, the motility of benthic microalgae also responds to exogenous cues, such as temperature (Cohn et al, 2003), the presence of sub-surface nutrients (Kingston, 2002), physical disturbance of the sediment (Hopkins, 1966) or wave action (Kingston, 1999b), and sediment desiccation (Coelho et al, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…However, this suggests a close coupling between water content and cyanobacterial movements. Similarly, migration of benthic diatoms in tidal sediment is strongly influenced by the tide level [13,26], but the causes of the rhythm are not yet clearly understood [13]. The upward migration in the presence of water could simply be a relaxation of a tightly bound population that initiates a random walk; thus part of it reaches the surface in the absence of stimulus.…”
Section: Control Of the Migrationmentioning
confidence: 99%
“…The temporal up-scaling issue is transversal to any MPB remote sensing approach and it is based on the drastic change of MPB biomass and specific composition during an emersion period [1,49,50]. In contrast, reflectance images are acquired instantaneously and the derived ETR maps would thus assess primary production at a single acquisition time which would inevitably induce a strong bias for tidal scale as well as daily budget estimation.…”
Section: Remote Sensing Applicationsmentioning
confidence: 99%