Near- bottom depletion of zooplankton over coral reefs: I: Diurnal dynamics and size distribution

Ruthy Yahel*, Gitai Yahel, Amatzia Genin

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

85 Scopus citations

Abstract

Changes in the near-bottom abundance of zooplankton on scales of centimeters to meters and hours to seasons are of great importance to corals and other benthic zooplanktivores. Our objective was to characterize such spatio-temporal changes over several coral reefs in the Gulf of Aqaba, Red Sea. Using arrays of underwater pumps, we found a substantial depletion of zooplankton near the bottom. Vertical gradients in zooplankton abundance were steeper during the night than day, mostly due to a greater nocturnal increase in zooplankton biomass higher in the water column. On average, the layer < 1 m above bottom (mab) was depleted by 2.6 ± 2.2 mg m-3 (4 6± 35%) and 1.4 ± 1.4 mg m-3 (37 ± 43%) during night and day, respectively. A long time series of bi-weekly samples at 0.5 mab, lasting 1.5 years, indicated a doubling of the biomass during the night with no apparent seasonality. The diel change was due to an increase in the abundance of only large (> 200 μm) zooplankters around dusk and their disappearance in the morning. Diurnal predation by zooplanktivorous fish, sediment resuspension by benthivorous fish and zooplankton behavior appear to control the dynamics of suspended particles over the reef, creating sharp vertical gradients and a remarkable diel cycle in the ratio between nutritious plankton and inorganic particles.

Original languageEnglish
Pages (from-to)75-85
Number of pages11
JournalCoral Reefs
Volume24
Issue number1
DOIs
StatePublished - Mar 2005

Keywords

  • Boundary layer
  • Predation
  • Seston quality
  • Vertical distribution
  • Vertical migration

Fingerprint

Dive into the research topics of 'Near- bottom depletion of zooplankton over coral reefs: I: Diurnal dynamics and size distribution'. Together they form a unique fingerprint.

Cite this