INORGANIC CARBON UPTAKE FOR PHOTOSYNTHESIS BY THE SYMBIOTIC CORAL DINOFLAGELLATE ASSOCIATION .1. PHOTOSYNTHETIC PERFORMANCES OF SYMBIONTS AND DEPENDENCE ON SEA-WATER BICARBONATE/
C. Goiran et al., INORGANIC CARBON UPTAKE FOR PHOTOSYNTHESIS BY THE SYMBIOTIC CORAL DINOFLAGELLATE ASSOCIATION .1. PHOTOSYNTHETIC PERFORMANCES OF SYMBIONTS AND DEPENDENCE ON SEA-WATER BICARBONATE/, Journal of experimental marine biology and ecology, 199(2), 1996, pp. 207-225
The aim of this and the accompanying paper is to investigate the mecha
nisms of dissolved inorganic carbon (DIC) uptake by the scleractinian
coral Galaxea fascicularis, and its delivery to the endosymbiotic phot
osynthetic dinoflagellates (zooxanthellae). For this purpose, a compar
ison was made between the photosynthetic performance of zooxanthellae
in intact symbiosis within microcolonies of Galaxea fascicularis, fres
hly isolated zooxanthellae (FIZ) and cultured zooxanthellae (CZ) under
different conditions. Discrimination between CO2 or HCO3- uptake was
achieved by several means including changes in DIC concentration, pH v
ariations, pharmacology or modifications of ion concentration in seawa
ter. In this paper, the photosynthesis/irradiance curves of G. fascicu
laris microcolonies, FIZ and CZ are presented. It is shown that zooxan
thellae inside their host have lower photosynthetic performance than i
solated zooxanthellae. Light saturation (I-k) occurred at higher irrad
iance in the intact association than in isolated symbionts. Light util
ization efficiency (alpha) was minimum in the intact association and i
ncreased in FIZ and CZ. G. fascicularis microcolonies, FIZ and CZ were
tested for their ability to utilize HCO3- as a source of DIC for phot
osynthesis. Two main approaches were used, the first consisting of cha
nging the bicarbonate concentration by adding HCO3- to bicarbonate-fre
e artificial seawater at constant pH, and the second of modifying the
pH of the seawater in a closed or open system. At saturating light int
ensity, the DIC concentration saturating for photosynthesis is no more
than that of normal sea water. At pH 8.2, a half-maximal rate of phot
osynthetic O-2 evolution is achieved at 408, 71 and 178 mu M HCO3- for
coral, FIZ and CZ respectively. The photosynthetic O-2 production wit
h constant inorganic carbon but varying pH reached an optimum at pH 8
to 9 suggesting that HCO3- is the main species taken up initially. FIZ
and CZ possess the ability to utilize both CO2 and HCO3- as substrate
s for transport. The rate of non-enzymatic dehydration of HCO3- exceed
s the rate of photosynthesis in coral and FIZ. but not in CZ. The resu
lts presented in this paper suggest that C. fascicularis microcolonies
are able to take up bicarbonate to supply symbiont photosynthesis, al
though zooxanthellae in hospite seems DIC-limited. FIZ seem to absorb
CO2 and HCO3- indiscriminately while CZ use HCO3-.