New Zealand Journal of Marine and Freshwater Research abstracts

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Light level variation in Lake Tutira after transient sediment inflow and its effect on the submersed macrophytes

I. M. JOHNSTONE

P. W. ROBINSON

New Zealand Electricity P. O. Box 445 Hamilton New Zealand

Abstract After exceptionally heavy rainfalls and associated land movements in July 1985, sediment inflow into Lake Tutira, Hawke's Bay, New Zealand, caused a five-fold reduction in the depth at which 5% of the surface photosynthetically active radiation remained. Light level reduction was associated with increased nephelometric turbidity caused by the suspended sediment. The decreased light levels, as monitored by measurement of the vertical attenuation coefficient of light in the lake, persisted for about three months and were accompanied by a marked reduction in the lower depth limit of aquatic macrophytes: from 6.7 to 1.8 m for Elodea canadensis, and from 4.6 to 1.8 m for Hydrilla verticillata. As water quality returned to its pre-storm condition, these species regrew very rapidly in the denuded areas from surviving rhizomes.

Keywords macrophytes; decline; turbidity; light; Lake Tutira; New Zealand; sediment inflow; precipitation; land movements; water quality

New Zealand Journal of Marine and Freshwater Research, 1987, Vol. 21: 47-53 0028-8330/87/2101-0047$2.50/0 © Crown copyright 1987 Received 6 March 1986; accepted 9 May 1986

PDF file of entire paper: medium quality (491K); (scanned from paper original: notes about this process)

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