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Entoprocta

life science Maturity 5-7 Next article →

Entoprocta, often called goblet worms, are a phylum of aquatic animals. Most species are sessile, meaning they remain attached to a surface. They are mostly marine, though some live in freshwater. There are about 150 recognized species in this group. They are organized into four main families: Barentsiidae, Pedicellinidae, Loxokalypodidae, and Loxosomatidae. These animals are important for understanding how complex body plans evolve.

Barentsia laxa 1498941
Barentsia laxa 1498941

A mature entoproct has a very specific shape. The body consists of a goblet-shaped calyx. This calyx sits on a long, muscular stalk. The rim of the calyx holds a crown of 8 to 30 solid tentacles. These tentacles are extensions of the body wall. The mouth and the anus both sit inside this crown. The name Entoprocta actually means "anus inside." This distinguishes them from bryozoans, which have an anus outside their tentacle crown.

Pedicellina cernua 001
Pedicellina cernua 001

Feeding in entoprocts is a highly organized process involving cilia. Cilia are tiny, hair-like structures that move in waves. Two main types of feeding occur. First, they use ciliary sieving. One band of cilia creates a water current. A second band of cilia acts as a sieve to trap food. Second, they use downstream collecting. In this method, the same cilia that create the current also trap the particles. The current flows into the crown at the base of the tentacles. It then exits above the center of the crown. Some species even use sticky threads to capture large particles.

Many entoprocts live in colonies rather than alone. The individual members of a colony are called zooids. These zooids are not fully independent animals. They grow from shared attachment plates or from stolons. Stolons are tube-like networks that run across a surface. In solitary species, the stalk may end in a muscular sucker or a flexible foot. Some solitary species can even move by creeping or somersaulting. These animals lack a coelom, which is an internal fluid-filled cavity. Their internal organs are embedded in connective tissue.

Reproduction in entoprocts is quite diverse. Most species are simultaneous hermaphrodites. This means one individual has both male and female reproductive organs. They have gonads located between the atrium and the stomach. Some species release eggs into the water to hatch as planktonic larvae. Other species brood their eggs in a special chamber. Some use placenta-like organs to nourish these developing eggs. When a larva settles on a surface, it undergoes metamorphosis. During this change, the internal gut can rotate by up to 180 degrees. This ensures the mouth and anus face upward.

Understanding the history of entoprocts is difficult because they are soft-bodied. Soft tissues rarely leave fossils. For a long time, scientists studied a fossil called Dinomischus from the Burgess Shale. It was found in Canada and lived during the Mid-Cambrian period. Many thought it was an early entoproct. However, researchers later concluded it was not a true member of the phylum. The earliest confirmed fossils come from the Late Jurassic in England. These fossils resemble the modern genus Barentsia.

Dinomischus
Dinomischus

There is also evidence of even older relatives. Fossils of a species called Cotyledon tylodes were found in China. These fossils are 520 million years old. This species was larger than modern entoprocts, reaching up to 56 mm in height. It was also armored with scale-like structures called sclerites. This suggests that early ancestors lived during the Cambrian explosion. Scientists continue to debate the exact family tree of these animals. Some studies link them to the Trochozoa, which includes molluscs and annelids. Other research suggests they are closely related to bryozoans or belong to a clade called Tetraneuralia.

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File:Barentsia laxa 1498941.png
Barentsia laxa 1498941.png
File:Pedicellina cernua 001.png
Pedicellina cernua 001.png
File:Dinomischus.png
Dinomischus.png
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