GARDEN ISLAND - THE EARLIEST (AND FIRST-ILLUSTRATED) BRYOZOAN REEF IN NORTH AMERICA (BASAL CHAZYAN, EARLY MIDDLE ORDOVICIAN; LAKE CHAMPLAIN, NEW YORK - VERMONT)
Only 10 bryozoan species were identified from 714 zoaria seen is 75 peel-sections made from the Garden Island bryozoan reef and its immediate surroundings.
Batostoma chazyensis (incl. campensis), encrusting to massive to locally stubby-branching trepostome, overwhelmingly dominates the reef core, and thin-branching trepostome Champlainopora (Atactotoechus) chazyensis the reef flank. Each comprises 50-90% of its ecozone's rock volume, and 60% and 90% (respecitively) of its zone's zoaria. The former was the principal frame-builder in the core, now layered cruststone and bindstone with micritic matrix containing crinoid and brachiopod debris; the latter grew prolifically on the flank, their broken fallen branch fragments now forming the skeletal sediment preserved as rudstone with partly sparry and partly micritic matrix.
A third species, ceramoporoid Ceramoporella (Cheiloporella) adamarhombica, is uncommon in the core, where its thin crusts locally constitute 10-15% of rock volume and zoarial count.
Two species, bifoliate Chazydictya chazyensis and fenestrate Phylloporina reticulata, are rare throughout, comprising only 2-3% of the zoaria and no more than traces volumetrically. Five more are even rarer, 0.1-0.5% of the zoarial counts: small irregular trepostomes Nicholsonella pulchra and Jordanopora heroensis, tiny arthrostylid Helopora mucronata, and bifoliates Eopachydictya gregaria and Stictopora (Rhinidictya) fenestrata.