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Fossil brachiopods(in the Netherlands and adjacent parts of Belgium and Germany)Brachiopods are a separate phylum of the animal kingdom. Just like bivalves whose shells can be found in large numbers on the sandy beaches of the North Sea, they have a soft body that is protected by a shell that consists of two hinged shell parts. However brachiopods are very different animals from bivalves. The class of bivalves belongs to the phylum of molluscs (Mollusca), while the brachiopods form their own phylum, which in itself is subdivided into classes.
The division of brachiopods and bivalves into two separate phyla obviously has to do with certain differences. The most striking difference can be found in the shells of the animals. For example, the ventral and dorsal shell of a brachiopod look different, while the shell halves of bivalves are identical. If we take a look at the individual shell halves, we see that the left and right sides are the same in brachiopods. In bivalves, the left and right halves are different; so they are not symmetrical (image 2).
As is often the case, there are
exceptions that prove the rule. For example, there are also bivalves
whose two shell halves are not identical, while there are also
brachiopods that have an almost identical ventral and dorsal shell. A
good example of this exception in bivalves is the great scallop (Pecten
maximus), which is also known as St. James shell and as an emblem of
the oil company Shell. This bivalve has both a convex and a flat shell,
while the left and right halves of the individual shells look the same (image 2).
In addition to the striking difference between the shells of brachiopods and bivalves, there are other differences such as the anatomy of the soft parts and the development of the animals. But of course you can’t see these differences when you find fossil specimens.
Brachiopods are sessile marine animals. This means that they are stuck on the surface and therefore they cannot move from one place to another. Many species are attached to that substrate with a fleshy, muscular stem. With special catching organs brachiopods swirl water into the shell where they then filter out the planktonic food particles. The water then leaves the shell again. Brachiopods have special opening and closing muscles for opening and closing the shell. For the origins of brachiopods we have to go back very far in geological history. The first species appeared early in the Cambrian, more than five hundred million years ago. A number of species even had already a great development during the Cambrian period. They had the peak of their development during the early Devonian period, more than four hundred million years ago. They can occur in great numbers in rocks from that period. Not so far from the Dutch border, in the Eifel in Germany, we frequently encounter them in various places in the limestone from the Middle Devonian.
The dominant time of the brachiopods does not end until the Permian. So we could say that they are typical animals of the Paleozoic era. But even during the subsequent Mesozoic, the brachiopods continued to play an important, although less predominant role. During the first part of the Mesozoic, the Triassic, the number of species and genera decreases considerably, but during the Jurassic and Upper Cretaceous there is a certain revival. We again find many brachiopods in the limestone of the upper Cretaceous in the south of Belgian and Dutch Limburg.
Today, several hundred species of brachiopods exist. That is not so much if we consider that about 30,000 fossil species (see also image 1) are known. Almost all species that still exist, occur in the sea on the continental shelf, in the littoral zone adjacent to the mainland. But some species are found in the deep sea. For those who want to know more about brachiopods, the following (German) books may be interesting. Especially these books were used to write (the original Dutch version of) this item about brachiopods. • Eifel-Brachiopoden by Hans J. Jungheim is published by Goldschneck-Verlag in 2000 (126 pages). The book not only provides good information about brachiopods in general, but also contains an extensive lexicon of terms and an extensive identification with images of brachiopods from the Eifel in Germany. •
Die Eifel
(Erdgeschichte, Fossilien, Lebensbilder) is also
written by Hans J. Jungheim and published by Goldschneck-Verlag
in 1996 (229 pages). This book contains an entire chapter with black
and white photos and drawings of brachiopods. Here too, attention is
paid to the identification of brachiopods from the Eifel. Text and pictures:
Jan Weertz |
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