Bryozoans

Bryozoans

Bryozoans are colonial animals of uncertain evolutionary descent. They may be related to freshwater rotifers. Bryozoans are found in the lower intertidal to subtidal zones, attached to a firm substrate, and also in brackish water. Individual animals are too small to see with the naked eye.

Bryozoan growth forms range from encrusting, forming coatings on hard surfaces, to bushy. An entire colony may bear a superficial resemblance to a hydroid colony, although bryozoans are internally more advanced than cnidarians. Bryozoan colonies grow to 3", and are occasionally larger.

Bryozoan anatomy
Note separate mouth and anus, unlike hydroid
Spiral Tufted Byozoans
Spiral Tufted Byozoans Amanthia spp

Klondike Rocks
The low, shelf-like structure of the rocks, which seldom rise
more than two feet above the bottom. Cunners

These low outcroppings appear in small to large patches over a two-mile area called the Klondike, and elsewhere, at depths ranging from 60 to 90 feet. The overhangs, crags, and holes afforded by the piles of rocks and boulders provide excellent homes for fish and lobsters. Visibility can be great here at times, but it is usually 10-20 ft, with a silty bottom in most places. The larger areas extend for many hundreds of feet, and an incautious diver can easily get lost. The stone itself is a type of sandstone known as Greensand, which occurs along the northern part of the New Jersey coast, and parts of Long Island, most famously as the Shrewsbury Rocks.