ANALYSIS OF PHYTOPLANKTON OF THE AUSTRALIAN SECTOR OF THE SOUTHERN-OCEAN - COMPARISONS OF MICROSCOPY AND SIZE FREQUENCY DATA WITH INTERPRETATIONS OF PIGMENT HPLC DATA USING THE CHEMTAX MATRIX FACTORIZATION PROGRAM
Sw. Wright et al., ANALYSIS OF PHYTOPLANKTON OF THE AUSTRALIAN SECTOR OF THE SOUTHERN-OCEAN - COMPARISONS OF MICROSCOPY AND SIZE FREQUENCY DATA WITH INTERPRETATIONS OF PIGMENT HPLC DATA USING THE CHEMTAX MATRIX FACTORIZATION PROGRAM, Marine ecology. Progress series, 144(1-3), 1996, pp. 285-298
A new matrix factorization program 'CHEMTAX' was used to interpret hig
h-performance liquid chromatography (HPLC) pigment data from a transec
t between Prydz Bay, Antarctica, and Australia during March 1987. The
program calculated the abundance of diatoms, dinoflagellates, haptophy
tes resembling Emiliania huxleyi, haptophytes resembling Phaeocystis a
ntarctica, cyanobacteria, prasinophytes, chlorophytes and cryptophytes
along the transect. The results were compared with those of microscop
y and particle size analysis. The transect was dominated by small cell
s: particle size analysis showed that particles <2 mu m represented 27
to 44% of the total by number while particles 2 to 20 mu m represente
d 55 to 68%. Particles >20 mu m never represented more than 3% by numb
er but constituted 57 to 93% of the total volume. Microscopic analysis
showed that small flagellates were the most abundant cells along the
transect, with a 5-fold increase in abundance at 47 degrees S. Numbers
of diatoms (most <20 mu m in size) increased markedly south of the Po
lar Front, correlating with the concentration of silica. Dinoflagellat
e numbers were relatively constant along the transect, although somewh
at higher north of 50 degrees S. Those <20 mu m in size were most nume
rous and accounted for most of the latitudinal variation. interpretati
on of HPLC pigment data using the CHEMTAX program was consistent with
microscopical analysis. The computed abundances of diatoms and dinofla
gellates correlated more strongly with the numbers of small (<20 mu m)
diatoms and dinoflagellates, respectively, than with large ones. Comp
uted cyanobacterial abundances correlated well with microscopical obse
rvations except for small errors where cyanobacteria were absent, prob
ably due to misallocation of zeaxanthin from chlorophytes and prasinop
hytes. The program was able to distinguish 2 populations of haptophyte
s along the transect, representing Phaeocystis antarctica and coccolit
hophorids, even though their pigment compositions were qualitatively (
though not quantitatively) identical. It also indicated the separate d
istributions of chlorophytes and prasinoxanthin-containing prasinophyt
es, and showed the presence of cryptophytes where none were observed b
y microscopy.