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1997年1月哥斯达黎加部分珊瑚礁中光和营养物质的空间分布。

Spatial distribution of light and nutrients in some coral reefs of Costa Rica during January 1997.

作者信息

Muller-Parker G, Cortés J

机构信息

Department of Biology and Shannon Point Marine Center, Western Washington University, Bellingham, Washington 98225-9160, USA.

出版信息

Rev Biol Trop. 2001 Dec;49 Suppl 2:251-63.

Abstract

The proximity of coral reefs to areas of present and future coastal development in Costa Rica highlights the need for assessing environmental conditions important to maintaining healthy corals. In January 1997 a survey of light penetration, inorganic nutrient concentrations, temperature, and salinity was conducted in the patch reefs of Bahía Culebra (Pacific Ocean) and on the Caribbean coast in the fringing reef at Parque Nacional Cahuita and near Limón. Temperature was 28 degrees C at all sites, and salinity ranged from 33 to 36 psu. Light attenuation coefficients ranged from 0.12 to 0.29 m(-1) in reef areas. Seawater nutrient concentrations were within the range of concentrations reported for tropical reef waters; combined NO3- and NO2- and PO4(3-) were each below 1 microM. NH4+ ranged from 0.2 to 7 microM, representing a significant source of nitrogen. The ratio of total dissolved inorganic nitrogen to phosphate averaged 27 for all reef waters. The high nitrate (3.6 microM) and light attenuation (0.95 m(-1)) values from the surface waters of the La Estrella plume (Caribbean coast) show that this river represents a significant source of nitrogen and light attenuation for the neighboring reefs at Cahuita. This survey provides a useful baseline for future studies, which should monitor these important coastal coral reef areas during both wet and dry seasons.

摘要

哥斯达黎加珊瑚礁与当前及未来沿海开发区的临近,凸显了评估对维持健康珊瑚至关重要的环境条件的必要性。1997年1月,在巴伊亚库莱布拉(太平洋)的斑块礁以及卡胡伊塔国家公园和利蒙附近加勒比海岸的边缘礁,对光穿透、无机养分浓度、温度和盐度进行了调查。所有地点的温度均为28摄氏度,盐度范围为33至36 psu。礁区的光衰减系数范围为0.12至0.29 m(-1)。海水养分浓度在热带礁水域报告的浓度范围内;NO3-与NO2-以及PO4(3-)的总和均低于1 microM。NH4+范围为0.2至7 microM,是一个重要的氮源。所有礁区海水的总溶解无机氮与磷酸盐的平均比值为27。来自拉埃斯特雷亚羽流(加勒比海岸)表层水的高硝酸盐(3.6 microM)和光衰减(0.95 m(-1))值表明,这条河流是卡胡伊塔附近礁区重要的氮源和光衰减源。这项调查为未来的研究提供了有用的基线,未来研究应在雨季和旱季对这些重要的沿海珊瑚礁区域进行监测。

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