Coral sand O2 uptake and pelagic–benthic coupling in a subtropical fringing reef, Aqaba, Red Sea

Aquatic Biology

Andreas Haas¹  Markus Huettel¹  Ulrich Struck¹  Mohammed Y. Rasheed¹  Christian Wild¹  Florian W. Mayer¹  Malik S. Naumann¹ 

关键词: Coral reefs;    Calcareous sands;    O2 flux;    Spatial and temporal changes;    Seasonality;    Pelagic–benthic coupling;    Red Sea;    Advection chambers;   

DOI  :  10.3354/ab00181

学科分类：生物科学（综合）

来源: Inter-Research

【 摘 要 】

ABSTRACT: Calcareous sands are major sites for recycling of organic matter in coral reef ecosystems. O₂ uptake and pelagic–benthic coupling were studied in coral sands using benthic chambers and sediment traps during several seasonal expeditions between May 2004 and May 2008 along a fringing reef on the Jordanian Red Sea coast. A total of 12 independent dark chamber experiments were conducted at 2.5 to 16.5 m water depth on the highly permeable calcareous reef sands covering the seafloor at the reef and back-reef lagoon. Sedimentary O₂ uptake ranged from 20 to 39 mmol m^–2 d^–1 and was positively correlated with water depth in the lagoon, but not in the reef, where O₂ uptake was significantly lower. Comparison of sedimentary O₂ uptake rates recorded at the same locations revealed little temporal and seasonal variation, and no significant responses to changes in environmental factors in the water column, such as temperature and concentrations of organic or inorganic nutrients. These results suggest that efficient recycling in the pelagic food web of the nutrient-deprived coral reef limits the supply of degradable organic matter to the reef sediments. Increase of sedimentary O₂ uptake with water depth in the lagoon sands may therefore be a function of lateral transport of labile organic particles produced by reef organisms (e.g. benthic algae and corals) rather than sedimentation of water column production.

【 授权许可】

Unknown