The silica uptake of Halichondria panicea Pallas, 1766 was measured in
laboratory experiments from February until August 1995. Uptake rates
were determined by measuring the decrease of dissolved silica in the s
urrounding seawater. All specimens were collected in Kiel Bight and ma
intained in aquaria up to several weeks prior to the experiments. Up t
o 5.27 mu mol Si g(-1) AFDW h(-1) were incorporated by the sponges, wi
th a strong, size-independent individual variation. A positive correla
tion between the content of dissolved silica in the seawater and the s
ilica uptake was found. Temperature had no decisive effect on uptake r
ates. The nutritional condition of the sponges turned out to be of gre
at importance. After 1 wk of starvation, Halicondria panicea uptake ra
tes were only 15% of the previous amount, which indicates that silica
transport is an energy-consuming process. During the most intense phas
e of reproduction activity in spring, female specimens showed a signif
icant drop in their silica uptake. Obviously they did not produce spic
ules during this time. An attempt to estimate the influence of H. pani
cea on its habitat as a consumer of dissolved silica led to the conclu
sion that in summer the sponges might affect the phytoplankton species
composition by competing with diatoms for dissolved silica.