Cm. Smith et Rs. Alberte, CHARACTERIZATION OF IN-VIVO ABSORPTION FEATURES OF CHLOROPHYTE, PHAEOPHYTE AND RHODOPHYTE ALGAL SPECIES, Marine Biology, 118(3), 1994, pp. 511-521
Despite the plentiful diversity of macroalgae in coastal environments,
few studies have examined the in vivo absorption features of common m
arine macrophytes. Here we report on results of a survey of 12 central
California common intertidal and subtidal taxa, representing Chloroph
yta, Phaeophyta and Rhodophyta carried out in the summer of 1988. Comp
uter-assisted analyses were used to obtain fourth-derivative spectra f
rom in vivo absorption spectra determined at room temperature to obtai
n spectral diagnostics for the different algai divisions and to provid
e a means to determine whether spectral features could be used to iden
tify stress responses among these plants. Among the Chlorophyta, chara
cteristic maxima for chlorophylls a and b were resolved in all species
examined, and a spectral component attributable to siphonaxanthin-lik
e carotenoid(s) was observed in two Ulva species and the coenocytic al
ga Derbesia marina. Representatives of the Phaeophyta were characteriz
ed by similar maxima for chlorophyll a and c, and for fucoxanthin. Amo
ng the Rhodophyta, maxima for chlorophyll a, as well as B- and R-type
phycoerythrin were resolved. Differences in in vivo absorption feature
s were detected for two tidal populations of Porphyra perforata and Ma
stocarpus papillatus. High-tidal thalli absorb less green light in reg
ions characterized by phycoerythrin, but have enhanced carotenoid abso
rption compared with low-tidal thalli. Resolution of spectra by fourth
-derivative analysis revealed significant differences in phycoerythrin
and carotenoid contents. The spectral changes observed appear to refl
ect environmental and possibly populational characteristics of these a
lgae. The spectral analyses described here provide robust, non-invasiv
e means to characterize subtle responses of macroalgae to environment
in ways not possible previously. Additional merits of these fourth-der
ivative analyses for use in environmental studies are discussed.