crinoid

Within 10 to 16 months the crinoid will be able to reproduce.

Sometimes used in a general sense for any crinoid.

A crinoid would have several anchors that were also made of disks.

The 2005 recording showed a crinoid moving at much faster speeds.

They filtered food particles from the water and are the rarest part of the crinoid.

The beaded crinoid can sometimes be seen "walking" across the seabed on its arms.

This crinoid was a colonial animal with ten long arms each that it used to capture prey.

Pernerocrinus is an extinct genus of crinoid from the Devonian.

The beaded crinoid has a cup shaped body, usually hidden from sight, from which about twenty arms project.

The beaded crinoid extends its arms and pinnules in slow flowing water.

They looked like feathery arms, and they are the reason that crinoid are often called sea lilies.

Sometimes you can find a crinoid that has been split in half, these specimens are very beautiful and are very good for jewelry.

The orange sea lily is a stalkless crinoid.

Like arms of primitive crinoid.

Iocrinus is an extinct genus of crinoid (sea lilies and feather stars).

Encrinus is an extinct genus of crinoid, and "one of the most famous".

Disks are the most commonly preserved part of the crinoid, and can be found in the hundreds in hash fossils.

It was located at the top of the crinoid's stem, and some crinoid balls were adorned with spikes.

The beaded crinoid is found in the Caribbean Sea and the Gulf of Mexico.

In 2005, a stalked crinoid was recorded pulling itself along the sea floor off the Grand Bahama Island.

In deeper waters, tunicate and stalked crinoid have been spotted by scuba expeditions.

Echmatocrinus is a problematic Cambrian animal which resembles a crinoid or an octocoral.

Alphacrinus is an extinct genus of crinoid which existed during the early Ibexian period.

The inside of a fossil crinoid is usually calcite crystals, because their skeletons were made of calcite.

In this fossil-rich bed have been found the fossils of sixty species of crinoid, distributed among more than forty genera.

Her digging has unearthed crinoid fossils from lily-shaped marine animals, as well as trilobites, the remains of ancient crustaceans.

Even when polished, Tennessee marble retains a fossiliferous texture, with bryozoan and crinoid fossils being among the most commonly found.

However, bryozoan and crinoid meadows can persist over time and produce compositionally distinct bodies of sediment with depositional relief.

Saint-Marc-des-Carrières limestone is a pearly grey, and becomes a pale beige with age, while Queenston limestone has pink calcite streaks from crinoid fossils and takes a chamois tint as it ages.