Effect of reef framework and bottom sediment on nutrient enrichment in a coral reef of the Gulf of Aqaba, Red Sea
M Rasheed
MI Badran
C Richter
M Huettel
Abstract
Inorganic nutrients and chlorophyll a concentrations were measured bi-weekly in a transect across a coral reef in the Gulf of Aqaba over a period of 1 yr. The nutrient and chlorophyll concentrations were compared to those in adjacentoffshore waters (400 m depth). In reef and offshore waters, nutrient (ammonium, nitrite, nitrate, phosphate and silicate) and chlorophyll a data showed seasonal changes, with high concentrations in winter and low concentrations in summer. However,throughout the summer, nutrient concentrations in the coral reef waters significantly exceeded those in the offshore waters, while this difference was less pronounced in winter. This difference was caused by nutrient release from regenerative spaces inthe reef framework and coral sand. In the reef framework water (i.e. cavity water), nutrient concentrations were 1.2- to 2.3-fold higher than those in the surrounding waters, corresponding to fluxes of 14.5 mmol m-2 d-1 for ammonium,7.7 mmol m-2 d-1 for nitrate, 0.9 mmol m-2 d-1 for nitrite, and 1.3 mmol m-2 d-1 for phosphate. In the less permeable reef sediments, nutrient concentrations exceeded those of thefree-stream waters by factors of 15 to 80. Here, the calculated diffusive fluxes were 0.06 mmol m-2 d-1 for ammonium, 0.03 mmol m-2 d-1 for nitrate, 0.01 mmol m-2 d-1 for nitrite, 0.01 mmolm-2 d-1 for phosphate, and 0.07 mmol m-2 d-1 for silicate. Our results highlight the importance of the reef framework and coral sand for the trapping and mineralization of particulate organic matter and theregeneration of nutrients in oligotrophic coral reef waters.
Rasheed M., Badran M., Richter C. and Huettel M. (2002) Effect of reef framework and bottom sediment on nutrient enrichment in a coral reef of the Gulf of Aqaba, Red Sea. Marine Ecology Progress Series 239: 277-285. 10.3354/meps239277
@article{Rasheed2002,
Title = {Effect of reef framework and bottom sediment on nutrient enrichment in a coral reef of the Gulf of Aqaba, Red Sea},
Author = {Rasheed, M and Badran, MI and Richter, C and Huettel, M},
Editor = {},
Journal = {Marine Ecology Progress Series},
Year = {2002},
Pages = {277-285},
Volume = {239},
Doi = {10.3354/meps239277},
Abstract = {Inorganic nutrients and chlorophyll a concentrations were measured bi-weekly in a transect across a coral reef in the Gulf of Aqaba over a period of 1 yr. The nutrient and chlorophyll concentrations were compared to those in adjacentoffshore waters (400 m depth). In reef and offshore waters, nutrient (ammonium, nitrite, nitrate, phosphate and silicate) and chlorophyll a data showed seasonal changes, with high concentrations in winter and low concentrations in summer. However,throughout the summer, nutrient concentrations in the coral reef waters significantly exceeded those in the offshore waters, while this difference was less pronounced in winter. This difference was caused by nutrient release from regenerative spaces inthe reef framework and coral sand. In the reef framework water (i.e. cavity water), nutrient concentrations were 1.2- to 2.3-fold higher than those in the surrounding waters, corresponding to fluxes of 14.5 mmol m-2 d-1 for ammonium,7.7 mmol m-2 d-1 for nitrate, 0.9 mmol m-2 d-1 for nitrite, and 1.3 mmol m-2 d-1 for phosphate. In the less permeable reef sediments, nutrient concentrations exceeded those of thefree-stream waters by factors of 15 to 80. Here, the calculated diffusive fluxes were 0.06 mmol m-2 d-1 for ammonium, 0.03 mmol m-2 d-1 for nitrate, 0.01 mmol m-2 d-1 for nitrite, 0.01 mmolm-2 d-1 for phosphate, and 0.07 mmol m-2 d-1 for silicate. Our results highlight the importance of the reef framework and coral sand for the trapping and mineralization of particulate organic matter and theregeneration of nutrients in oligotrophic coral reef waters.},
}
TY - JOUR
AU - Rasheed, M
AU - Badran, MI
AU - Richter, C
AU - Huettel, M
TI - Effect of reef framework and bottom sediment on nutrient enrichment in a coral reef of the Gulf of Aqaba, Red Sea
T2 - Marine Ecology Progress Series
PY - 2002
SP - 277-285
VL - 239
DO - 10.3354/meps239277
AB - Inorganic nutrients and chlorophyll a concentrations were measured bi-weekly in a transect across a coral reef in the Gulf of Aqaba over a period of 1 yr. The nutrient and chlorophyll concentrations were compared to those in adjacentoffshore waters (400 m depth). In reef and offshore waters, nutrient (ammonium, nitrite, nitrate, phosphate and silicate) and chlorophyll a data showed seasonal changes, with high concentrations in winter and low concentrations in summer. However,throughout the summer, nutrient concentrations in the coral reef waters significantly exceeded those in the offshore waters, while this difference was less pronounced in winter. This difference was caused by nutrient release from regenerative spaces inthe reef framework and coral sand. In the reef framework water (i.e. cavity water), nutrient concentrations were 1.2- to 2.3-fold higher than those in the surrounding waters, corresponding to fluxes of 14.5 mmol m-2 d-1 for ammonium,7.7 mmol m-2 d-1 for nitrate, 0.9 mmol m-2 d-1 for nitrite, and 1.3 mmol m-2 d-1 for phosphate. In the less permeable reef sediments, nutrient concentrations exceeded those of thefree-stream waters by factors of 15 to 80. Here, the calculated diffusive fluxes were 0.06 mmol m-2 d-1 for ammonium, 0.03 mmol m-2 d-1 for nitrate, 0.01 mmol m-2 d-1 for nitrite, 0.01 mmolm-2 d-1 for phosphate, and 0.07 mmol m-2 d-1 for silicate. Our results highlight the importance of the reef framework and coral sand for the trapping and mineralization of particulate organic matter and theregeneration of nutrients in oligotrophic coral reef waters.
ER -
