Department of Environmental Sciences, University of Virginia, Charlottesville, Virginia, United States of America.
PLoS One. 2013;8(3):e58581. doi: 10.1371/journal.pone.0058581. Epub 2013 Mar 11.
Quantitative studies of coral reefs are challenged by the three-dimensional hard structure of reefs and the high spatial variability and temporal dynamics of their metabolism. We used the non-invasive eddy correlation technique to examine respiration and photosynthesis rates, through O2 fluxes, from reef crests and reef slopes in the Florida Keys, USA. We assessed how the photosynthesis and respiration of different reef habitats is controlled by light and hydrodynamics. Numerous fluxes (over a 0.25 h period) were as high as 4500 mmol O2 m(-2) d(-1), which can only be explained by efficient light utilization by the phototrophic community and the complex canopy structure of the reef, having a many-fold larger surface area than its horizontal projection. Over diel cycles, the reef crest was net autotrophic, whereas on the reef slope oxygen production and respiration were balanced. The autotrophic nature of the shallow reef crests implies that the export of organics is an important source of primary production for the larger area. Net oxygen production on the reef crest was proportional to the light intensity, up to 1750 µmol photons m(-2) s(-1) and decreased thereafter as respiration was stimulated by high current velocities coincident with peak light levels. Nighttime respiration rates were also stimulated by the current velocity, through enhanced ventilation of the porous framework of the reef. Respiration rates were the highest directly after sunset, and then decreased during the night suggesting that highly labile photosynthates produced during the day fueled early-night respiration. The reef framework was also important to the acquisition of nutrients as the ambient nitrogen stock in the water had sufficient capacity to support these high production rates across the entire reef width. These direct measurements of complex reefs systems yielded high metabolic rates and dynamics that can only be determined through in situ, high temporal resolution measurements.
珊瑚礁的定量研究受到珊瑚礁三维硬结构以及其代谢的高空间变异性和时间动态性的挑战。我们使用非侵入性的涡度相关技术,通过 O2 通量,来检测美国佛罗里达群岛的珊瑚礁顶和礁坡的呼吸和光合作用速率。我们评估了不同珊瑚礁生境的光合作用和呼吸作用是如何受到光和水动力的控制的。许多通量(在 0.25 h 期间)高达 4500 mmol O2 m(-2) d(-1),这只能通过光养生物群落的高效光利用和珊瑚礁复杂的冠层结构来解释,其表面积比水平投影大许多倍。在日周期内,珊瑚礁顶是净自养的,而在礁坡上,氧气的产生和呼吸作用是平衡的。浅礁顶的自养性质意味着有机物的输出是更大面积初级生产力的重要来源。珊瑚礁顶的净氧气产生与光强度成正比,最高可达 1750 µmol 光子 m(-2) s(-1),此后随着与光强峰值同时出现的高速水流刺激呼吸作用而降低。夜间呼吸作用速率也因水流而受到刺激,这是通过珊瑚礁多孔框架的增强通风实现的。呼吸作用速率在日落后直接达到最高值,然后在夜间下降,这表明白天产生的高度不稳定的光合作用产物为深夜的呼吸作用提供了燃料。珊瑚礁框架对获取营养物质也很重要,因为水中的环境氮储量有足够的能力支持整个珊瑚礁宽度的这些高生产力。这些对复杂珊瑚礁系统的直接测量产生了高代谢率和动态,这只能通过原位、高时间分辨率测量来确定。