Journal of Plankton Research, Vol 21, 1911-1921, Copyright © 1999 by Oxford University Press
D Giroldo and A Vieira
Carbon assimilation (14C) and dissolved organic
carbon (DO14C) release by a tropical strain of
Cryptomonas obovata was studied. Cells were exposed to
a range of irradiances (0-2000
ORIGINAL ARTICLES
Assimilation and release of 14C in a tropical strain of Cryptomonas obovata (Cryptophyceae) exposed to several irradiances
Federal University of São Carlos, Department of Botany, CEP 13565-905, CP 676, São Carlos SP, Brazil
mol
m-2 s-1) using axenic batch
cultures in the laboratory (Ek = 180
mol
m-2s-1). At up to 2000
mol m-2s-1, carbon
assimilation was not inhibited and an acclimation to low irradiances was
observed. DO14C release was dependent on carbon
fixation and no increase was detected under high irradiances. To determine
particulate organic carbon (PO14C) loss and
CO14C release cells acclimated to 350
mol
m-2 s-1 were incubated during
4 h at 35, 350, 850 and 1900
mol m-2
s-1. DO14C release was
responsible for 30% of the PO14C loss at 1900
mol m-2s-1. High-
and low-molecular-weight (HMW, LMW) compounds were released by
C.obovata under all irradiance conditions. However,
increased release with exposure time was observed only for the HMW
compounds.
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