Bc. Cowell et Ps. Botts, FACTORS INFLUENCING THE DISTRIBUTION, ABUNDANCE AND GROWTH OF LYNGBYA-WOLLEI IN CENTRAL FLORIDA, Aquatic botany, 49(1), 1994, pp. 1-17
Fifteen sites in the Kings Bay/Crystal River estuarine system, Florida
, were sampled over 1 year to determine the spatial and temporal distr
ibution and abundance of the filamentous blue-green alga, Lyngbya woll
ei (Farlow ex Gomont) Speziale and Dyck. Monthly biomass (dry weight)
of benthic Lyngbya mats was constant at approximately 1 kg m(-2) durin
g most of the year, but it decreased from April to July when large mat
s were observed floating on the water surface. Multiple regression ana
lyses showed that Lyngbya biomass was correlated negatively with condu
ctivity and alkalinity; this is consistent with L. wollei being primar
ily a freshwater species. In regions of the bay with higher salinities
, the vascular macrophyte, Hydrilla verticillata (L.f.) Royle, prevail
ed. Nutrient influences appeared to be small even though the northeast
portion of Kings Bay/Crystal River has high concentrations of nitroge
n, phosphorus and calcium. Controlled laboratory studies were conducte
d to determine the effects of pH, salinity, and nutrients on growth of
L. wollei. Optimal growth occurred at a pH of 8.0 and a salinity of 0
ppt (g 1(-1)); salinities in excess of 5.25 ppt killed more than 99%
of the cells within 2 weeks. Growth of Lyngbya from five Kings Bay sta
tions in six nutrient sources (spring water; NO3-N, NH4-N, PO4-P, NO3-
N+PO4-P, and NH4-N+PO4-P) did not differ among stations, and nutrient
additions produced no increases over spring water. Addition of Ca2+ in
creased growth of L. wollei at low and intermediate concentrations of
nitrogen and/or phosphorus; this partially explains why spring water,
derived from the limestone aquifer, produces such good growth of lyngb
ya.