Unidad de Limnología y Recursos Acuáticos (ULRA), Departamento de Biología, Facultad de Ciencias y Tecnología, Universidad Mayor de San Simón (UMSS), Cochabamba, Bolivia.
Photochem Photobiol Sci. 2013 Sep;12(9):1649-57. doi: 10.1039/c3pp25285j.
Tropical high-altitude Andean lakes are physically harsh ecosystems. Located above the treeline (≥4000 m a.s.l.), they share common features with temperate alpine lakes, which impose extreme conditions on their aquatic organisms: e.g., strong winds, broad diel variations in water temperature, and intense solar ultraviolet radiation (UVR). However, because of their latitude, they differ in two major ecological characteristics: they lack ice cover during the winter and they do not present summer water column stratification. We sampled 26 tropical high-altitude Andean lakes from three regions of the Bolivian Eastern Andes Cordillera during the wet period (austral summer). We performed an ordination to better describe the typology of Andean lakes in relation to the environmental variables, and we assessed the relationships among them, focussing on the UV-A transparency (360 nm) throughout the water column. We found a positive correlation between UV-A transparency calculated as Z(1%) (the depth which reaches 1% of the surface UV-A), the lake maximum depth and Secchi transparency (r = 0.61). Z(1%) of UV-A was smaller in shallow lakes than in deep lakes, indicating that shallow lakes are less transparent to UV-A than deep lakes. We hypothesize that, compared to shallow lakes, deep lakes (maximum depth > 10 m) may have lower dissolved organic carbon (DOC) concentrations (that absorb UV radiation) due to lower temperature and reduced macrophyte cover. Based on our data, tropical high-altitude Andean lakes are less transparent to UV-A (K(d) range = 1.4-11.0 m(-1); Z(1%) depth range = 0.4-3.2 m) than typical temperate alpine lakes (1-6 m(-1), 3-45 m, respectively). Moreover, they differ in vertical profiles of UV-A, chlorophyll-a, and temperature, suggesting that they may have a distinct ecological functioning. Such peculiarities justify treating tropical high-altitude Andean lakes as a separate category of alpine lakes. Tropical high-altitude Andean lakes have been poorly studied. Thus they deserve more in-depth studies in the face of global changes regarding the use of their UV transparency as a sentinel proxy of climate changes, particularly global warming.
热带高海拔安第斯山湖是自然条件恶劣的生态系统。这些湖泊位于林线以上(≥4000 米海拔),与温带高山湖泊具有共同特征,这对其水生生物构成了极端条件:例如,强风、水温的宽幅日变化和强烈的太阳紫外线辐射(UVR)。然而,由于它们所处的纬度不同,它们在两个主要生态特征上有所不同:它们在冬季没有冰盖,也不存在夏季水柱分层现象。我们在玻利维亚东部安第斯山脉 Cordillera 的三个地区的雨季(南半球夏季)采集了 26 个热带高海拔安第斯山湖的样本。我们进行了排序分析,以更好地描述安第斯山湖与环境变量之间的类型学关系,并评估了它们之间的关系,重点关注整个水柱中的 UV-A 透明度(360nm)。我们发现 UV-A 透明度与 UV-A 计算的 Z(1%)(达到表面 UV-A 的 1%的深度)、湖泊最大深度和塞奇透明度之间呈正相关(r=0.61)。浅水湖的 UV-A 透明度 Z(1%)小于深湖,这表明浅水湖对 UV-A 的透明度低于深湖。我们假设,与浅湖相比,深湖(最大深度>10 米)的溶解有机碳(DOC)浓度可能较低(吸收 UV 辐射),因为温度较低且大型植物覆盖较少。根据我们的数据,热带高海拔安第斯山湖对 UV-A 的透明度较低(K(d)范围=1.4-11.0 m(-1);Z(1%)深度范围=0.4-3.2 m),与典型的温带高山湖泊(分别为 1-6 m(-1)和 3-45 m)相比。此外,它们在 UV-A、叶绿素-a 和温度的垂直分布上存在差异,表明它们可能具有独特的生态功能。这些特殊性使得热带高海拔安第斯山湖成为高山湖泊的一个独立类别。热带高海拔安第斯山湖的研究较少。因此,在面对全球气候变化,特别是全球变暖,将其 UV 透明度用作气候变化的哨兵代理时,它们需要更深入的研究。