Sporopollenin layers in the cell wall of coccal green algae are responsible
for the resistance of cell walls to destructive processes during fossiliza
tion as well as during chemical preparation of samples for pollen-analysis.
Pollen slides of samples from limnic sediments thus also contain some alga
l cell walls. Although some pollen-analysts tried to stress this fact, the
finds of algae in pollen slides have not been paid systematic attention yet
, despite their potential use for a more accurate palaeoecological reconstr
uction.
The article summarizes the results of palaeoecological studies showing how
the algae can be used in palaeoecological reconstruction of past environmen
ts. The possibility of utilizing the indicative value of algal finds is dem
onstrated on examples of algal communities from fossil, subrecent and recen
t sediments from different longitudes, latitudes, and altitudes. The identi
fication and indicative values of species and varieties of Pediastrum are i
ncluded in a special review (KOMAREK & JANKOVSKA, Biblioth. Phycol., in pre
ss). The contemporary knowledge of ecological requirements of the given tax
a, completed by information from their fossil finds, makes possible the rec
onstruction of trophic and temperature conditions and of the purity of the
water environment of the past water biotopes.