Brachiopods

BGS fossils and geological time

The Early Palaeozoic brachiopod Dolerorthis.
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The Early Palaeozoic brachiopod Dolerorthis. ©Natural History Museum.

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Brachiopods have a very long history of life on Earth (at least 550 million years). They first appear as fossils in rocks of earliest Cambrian age, and their descendants survive, albeit relatively rarely, in today’s oceans and seas. They were particularly abundant during Palaeozoic times (248 to 545 million years ago), and are often the most common fossils in rocks of that age.

Brachiopods vary considerably in size. The aptly named Carboniferous genus Gigantoproductus may grow up to 30 centimetres across. In contrast, the Jurassic rhynchonellid genus Nannirhynchia is minute, generally only two or three millimetres across, or the size of a large pin head.

The animal

Leptanena depressa, J Sowerby, 1824.
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Leptanena depressa, J Sowerby, 1824. BGS ©UKRI. All rights reserved.

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Brachiopods are marine animals belonging to their own phylum of the animal kingdom, Brachiopoda. Although relatively rare, modern brachiopods occupy a variety of sea-bed habitats ranging from the tropics to the cold waters of the Arctic and, especially, the Antarctic.

Brachiopods are virtually defenceless and their shell, enclosing the animal’s organs, is the only protection against predators. Most are permanently attached by a fleshy stalk (the pedicle) to a hard, sea-floor surface, and are incapable of actively pursuing food. A few species can attach themselves directly to soft sediment and others remain unattached. Opening and closing of the shell allows food-bearing currents of water to pass through it.

The shell comprises two valves that are composed of calcite or chitinophosphate (calcium phosphate plus organic matter). The pedicle (or ventral) valve is typically externally convex. The other valve (the brachial or dorsal valve) may be similar but, in some brachiopods, it is extremely concave or more rarely conical.

The main features of a brachiopod shell and hinge. Many brachiopods have their valves hinged together, typically by a pair of ventral teeth and dorsal sockets. The snugly fitting join between the two closed valves is called the commissure. The inner surface of the valves may bear various projections and depressions that reflect the location and form of organs or muscles that open and close the valves. The external surface may show various types of ornamentation including concentric growth lines, lamellae and wrinkles (rugae), ribs, folds, sulci and spines.
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The main features of a brachiopod shell and hinge. Many brachiopods have their valves hinged together, typically by a pair of ventral teeth and dorsal sockets. The snugly fitting join between the two closed valves is called the commissure. The inner surface of the valves may bear various projections and depressions that reflect the location and form of organs or muscles that open and close the valves. The external surface may show various types of ornamentation including concentric growth lines, lamellae and wrinkles (rugae), ribs, folds, sulci and spines. BGS ©UKRI. All rights reserved.

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An artist’s impression of a Silurian seascape showing, on the right-hand side, clusters of Pentamerus (1) with other brachiopods, including Atrypa (2), as well as corals (3) and bryozoa (4). Atrypa also occurs amongst the brachiopod fauna shown in the deeper water on the left-hand side where crinoids (5) and gastropods (6) also live. BGS ©UKRI. All rights reserved. Based on a painting by Richard Bell.

Feeding: a living brachiopod

The filter-feeding mechanism of a living brachiopod.
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The filter-feeding mechanism of a living brachiopod. BGS ©UKRI. All rights reserved.

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A large part of the space between the two valves is occupied by a fleshy, hollow organ (the lophophore), which has long twisted or coiled arms and filaments. Cilia attached to the filaments beat rapidly, drawing in food-bearing water currents.

Water currents carrying food particles (represented by the solid black arrows in the diagram) enter between the brachiopod valves through the lateral inhalant aperture. Food is caught by the filaments on the lophophore arms, and filtered water (represented by the white arrows) leaves via the median exhalant aperture.

A silicified brachiopod showing the structure (brachidia) that supports the coiled arms of the lophophore. Knowledge of the internal features of the valves is required as an aid to identification.
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A silicified brachiopod showing the structure (brachidia) that supports the coiled arms of the lophophore. Knowledge of the internal features of the valves is required as an aid to identification. ©Natural History Museum.

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The geologists’ tool

Spirifer (Carboniferous).
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Spirifer (Carboniferous). BGS ©UKRI. All rights reserved.

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Brachiopods are characteristic of shallow marine environments, and in some Palaeozoic rocks they are the main rock-forming component. Brachiopods are also particularly suitable for palaeoecological analyses. Influenced by such factors as water depth, salinity, oxygen levels and static lifestyle, the distribution patterns of fossil brachiopods provide a useful tool in deducing the position of ancient shorelines and the past distribution of land and sea. Through the rapid evolution of some brachiopod lineages, they can be useful for understanding the relative ages of rock successions, and for correlation. 

Cambrian rocks characteristically contain a diverse and abundant brachiopod fauna that  preludes a dramatic diversification, making brachiopods, together with trilobites, the primary stratigraphical guide fossils in the shallow-water facies of the Ordovician They are also important in the Silurian and Devonian, and more locally in. the Carboniferous, but many major groups became extinct at the end of the Palaeozoic.

The main divisions of Earth history in which brachiopods have lived, showing the relative diversity of the phylum through time. Maximum diversity is seen in the Devonian.
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The main divisions of Earth history in which brachiopods have lived, showing the relative diversity of the phylum through time. Maximum diversity is seen in the Devonian. BGS ©UKRI. All rights reserved.

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Fun facts

3D fossil models

Atrypa reticularis var. (SM A 11629 – Holotype). Ludlow Epoch (Silurian Period) (423.6 – 427.4 Ma B.P.) See 3D fossils online.
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Atrypa reticularis var. woodwardi. (SM A 11629 – Holotype). Ludlow Epoch (Silurian Period) (423.6 – 427.4 Ma B.P.) See 3D fossils online. BGS ©UKRI. All rights Reserved.

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Many of the fossils in the BGS palaeontology collections are available to view and download as 3D models. To view this fossil, or others like it, in 3D visit GB3D Type Fossils.

Reference

Cox, B M, and Penn, I E. 2000. Brachiopods: fossil focus. Nottingham, British Geological Survey.

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