O. Hints, Ordovician eunicid polychaetes of Estonia and surrounding areas: review oftheir distribution and diversification, REV PALAE P, 113(1-3), 2000, pp. 41-55
Scolecodonts, the jaws of polychaete worms, are common and diverse palynomo
rphs in the Ordovician rocks of Estonia and surrounding areas. Some 120 app
aratus-based species representing about 40 genera have been recorded thus f
ar. Relatively long stratigraphical ranges of the majority of species refle
ct a low rate of evolution of jawed polychaetes. However, some individual s
pecies, as well as structural changes in the assemblages, appear to be usef
ul for stratigraphical purposes. Environmental events like those in the mid
dle Caradoc and late Ashgill had some impact on polychaete faunas, but less
than on several other groups. In order to study the spatial distribution o
f eunicids, faunas of particular intervals of the Ordovician were investiga
ted. Quantitative analysis revealed that polychaete assemblages with a very
consistent qualitative and quantitative composition were widespread over l
ong distances within the belts of similar facies conditions in the Baltosca
ndian Palaeobasin. On the other hand, it appears that species of Ordovician
jawed polychaetes were strongly influenced by particular facies, and accor
dingly well differentiated along the palaeobasin gradient. The decrease in
diversity and abundance towards the deeper-water part of the palaeobasin in
dicates that the majority of Ordovician eunicids preferred relatively shall
ow-water conditions. The increase in differentiation of environments is acc
ompanied by an increase in differentiation of polychaete assemblages. (C) 2
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