A limnological reconnaissance of Lake Lanao: With 6 figures and 3 tables in the text and on 2 folders
A limnological reconnaissance of Lake Lanao: With 6 figures and 3 tables in the text and on 2 folders
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拉瑙湖湖泊学勘察：正文中有 6 张图和 3 张表格，包含 2 个文件夹
DOI：
10.1080/03680770.1968.11895955
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发表时间：
1969
影响因子：
1.9
通讯作者：
D. G. Frey
中科院分区：
文献类型：
--
作者：
D. G. Frey
菲律宾棉兰老岛北部的拉瑙湖在湖泊学上引起了极大的兴趣，原因无非是它含有各种动物的特有物种，包括在湖中进化的鲤鱼物种群（最近的评论由 MYERS，1960 年，但另见 BROOKS 1950 年和 HERRE 1933 年）。与BAILEY Wu的观点相反。我们（引自 MYERS 1960）认为该湖只有大约 10,000 年的历史，根据玛丽亚克里斯蒂娜瀑布下方峡谷的长度，越来越多的证据表明该湖的年龄比这要长，甚至可能来自第三纪晚期。除了 HERRE 对鱼类的分类学研究之外，关于该湖及其湖泊学的出版物相对较少（参见 MYERS 中的参考书目） 1960）。 1932 年 Wallacea 探险队的零碎且尚未完整发表的观测结果包括最大深度探测为 107 m，5 月 7 日在 90 m 处溶解氧超过 1 ppm（与菲律宾几乎所有其他深湖相比，其中氧气在相对接近地表的情况下完全消失），以及 WoLTERECK 将该湖纳入他的热带深湖组中， 冬季完全循环（WoLTERECK 1933，1941）。最后的陈述完全是假设性的，因为到目前为止还没有对该湖进行季节性观测。除此之外，还有近海和近海浮游生物以及浅水底栖生物中存在的部分生物体清单（大多数情况下为属，某些情况下为物种）（WoLTERECK 1941）。这些观察结果非常零碎，更多的是暗示湖泊学过程而不是定义它们。
Lake Lanao on northem Mindanao in the Philippines is of great interest limnologically if for no other reason than that it contains endemic species of various kinds of animals, including a species flock of cyprinids that have evolved in the lake (most recent review by MYERS, 1960, but see also BROOKS 1950, and HERRE 1933). Contrary to the opinion of BAILEY Wu. us (quoted in MYERS 1960) that the lake is only about 10,000 years old, based on the short length of the canyon below Maria Cristina Falls, evidence is accumulating that the lake is mmh older than this, possibly even deriving from the late Tertiary.Relatively little has been published conceming the lake and its limnology, aside from taxonomic studies of the fishes by HERRE (see bibliography in MYERS 1960). The fragmentary and still incompletely published observations of the Wallacea Expedition in 1932 include a maximum depth sounding of 107 m, more than l ppm dissolved oxygen at 90 m on 7 May (in contrast to nearly all other deep lakes of the Philippines in whic: h the oxygen completely disappears relatively dose to the surface), and the inclusion of the lake by WoLTERECK in his group of deep tropical lakes with a complete circulation in winter (WoLTERECK 1933, 1941). This last statement is entirely presumptive, as up to now there have been no seasonal observations on the lake. Besides this there are partial lists of organisms (to genera in most cases, species in some) that occur in the inshore and offshore plankton, and to a lesser extent in the shallow-water benthos (WoLTERECK 1941). These observations, being very fragmentary, do more to suggest limnological processes than define them.