Limnology of an equatorial high mountain lake - Lago San Pablo, Ecuador: The significance of deep diurnal mixing for lake productivity
Limnology of an equatorial high mountain lake - Lago San Pablo, Ecuador: The significance of deep diurnal mixing for lake productivity
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DOI:
10.1016/s0075-9511(02)80015-9
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发表时间:
2002-05-01
期刊:
影响因子:
1.7
通讯作者:
Casallas, J
中科院分区:
文献类型:
--
作者:
Gunkel, G;Casallas, J
Equatorial high mountain takes are a special type of lake occurring mainly in the South American Andes as well as in Central Africa and Asia. They occur at altitudes of a few thousand meters above sea level and are cold-water lakes ( 0.01 mg/l, and soluble inorganic nitrogen > 0.2 mg/l. Nitrogen and phosphorus are available in the epilimnion all year round (N-sol, inorg(.) = 0.3 to 1.7 mg/l N, SRP = 0.04 to 0.63 mg/l P). The N/P ratio is sometimes > 14, sometimes < 10, indicating a variability of the limiting nutrient factor. Considering the nutrient level, the phytoplankton biomass is quite low (about 4,000 cells per ml on average; maximum cell number: 13,000 in 1998 and 10,000 in 1999). The mean epilimnic chlorophyll content (Chl a) was 10 mug/l in 1998 and 11 mug/l in 1999, and the maximum Chl a content was 16 and 22 mug/l in 1998 and 1999, respectively.Phytoplankton production can be limited by nutrients, mainly nitrogen, but convective currents can also cause a significant loss of biomass. The lake's euphotic zone is smaller than its epilimnic zoned indicating that light radiation is limiting in the deeper water body, this is caused by a weak thermocline due to destratification by nocturnal cooling, the atelomixis.