Abstract
Long standing water-gauge data recorded at the lower course of the Magda-lena river (Colombia), show every 6 to 7 year extreme high and low water levels. These rhythmical changes could be proved highly significant with Student's t-test. Furthermore, these oscillations of waterlevels could be corre-lated with long-term changes of rainfalls in the upper hydrographic basin of the Magdalena. The extreme high waters cause cyclical floodings of the Ciénaga Grande de Santa Marta, a brackish water lagoon communicated with the Magdalena, and thus the cyclical extinction of the oyster Crassostrea rhizophorae, which is of considerable economic importance.
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CITATION STYLE
Kaufmann, R., & Hevert, F. (2016). El régimen fluviométrico del Río Magdalena y su importancia para la Ciénaga Grande de Santa Marta. Boletin de Investigaciones Marinas y Costeras, 7, 121–137. https://doi.org/10.25268/BIMC.INVEMAR.1973.7.0.550
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