A. Schreiber et al., ICY HERITAGE - ECOLOGICAL EVOLUTION OF THE POSTGLACIAL BALTIC SEA REFLECTED IN THE ALLOZYMES OF A LIVING FOSSIL, THE PRIAPULID HALICRYPTUS-SPINULOSUS, Marine Biology, 125(4), 1996, pp. 671-685
Genetic variation of 16 allozyme loci in 397 Halicryptus spinulosus (P
riapulida) revealed overall polymorphism of P = 0.438 and Hardy-Weinbe
rg expectations for heterozygosity of H-e = 0.060 for Baltic Sea stock
s, H-e = 0.143 for the White Sea and H-e = 0.121 for Iceland. Maximal
unbiased standard distances of D = 0.0693 separated Baltic and White S
ea populations. Nordic and Baltic populations could be distinguished b
y allozymes, but Baltic subsamples proved cohesive. Gene flow amounted
to effective exchange values per generation of N-m = 2.94 over 650 km
of continuous habitat, N-m = 10.65 over 175 km, and N-m = 13.85 over
20 km. Gene flow started to decrease with geographic distance beyond a
dispersal threshold of 20 km, but hierarchical G(ST)-statistics indic
ated light isolation by distance beyond a minimum of 8 km. Gene flow i
s high for a benthic worm assumed to lack dispersal by pelagic larva,
a paradox which cannot be resolved now. Baltic populations are charact
erized by lower heterozygosity than Nordic stocks. In the Baltic Basin
, temporally continuous brackish-water conditions have only existed fo
r the past 7000 years. The two possible colonization routes of H. spin
ulosus to the geologically young Baltic Sea imply genetic drift, wheth
er by founder effect (sweepstake colonization from Iceland) or by refu
gial bottlenecking during the Ancylus phase of the Baltic Basin after
a direct connection to the White Sea had been sequestered. Continued g
enetic drift is emphasized by lower heterozygosity in the ecologically
unstable Belt Sea compared to the central Baltic. Allozymes falsify t
he reduced-mutability hypothesis to explain bradytelic evolution of Pr
iapulida. Regional genetic homogeneity, ample polymorphism, and prefer
ence for anoxic black mud qualify H. spinulosus populations as indicat
ors of microevolutionary responses to water circulation regimes or pol
lution in the Baltic Sea.