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38 Massive free-lying brachiopod

Brachiopoda, Terebratulida: Erihadrosia epsilon

One of the variety of life habits that brachiopods have evolved is known as ‘free-lying’. While juveniles of free-lying brachiopods are probably always attached to a hard substrate (ie a shell or pebble) by their pedicle, as these species get larger they allow their pedicle to wither and they lie on the sea floor on soft sediments. The foramen is tiny in adults.

This figure shows three images, which include two views of the brachiopod Erihadrosia epsilon and a cartoon of the brachiopod on the sea floor. The specimen ID number for the fossil in this figure is OU6957. The left image shows a top-down or dorsal view of the fossil brachiopod. The shell is oval-shaped with visible growth lines and is light brown. The shell is around six centimetres wide and ten centimetres long. The top right image is a side profile or lateral view of the same fossil. This view highlights the thickness and curvature of the fossil. The cartoon in the lower right is an illustration depicting how Erihadrosia epsilon would have sat on the sea floor, with the two shells slightly open into the water as the hinge is anchored into the sediment.

An example of the brachiopod Erihadrosia epsilon in different views, including a reconstruction of how it would have sat on the sea floor (specimen OU 6957). Image credit: JH Robinson with illustration adapted from Richardson (1981).

Brachiopods must open their shells (at the ‘anterior’ end) in order to feed by filtering tiny food particles out of the sea water.  Free-lying brachiopods thicken the posterior end of the shell so it is much heavier and sinks a little into the soft sediment, raising up the anterior end.

Many different genera and species of brachiopod have adopted this free-lying habit over their 500 million year history. In New Zealand the most impressive species is Erihadrosia epsilon (originally called Stethothyris epsilon); single specimens can be up to 10 cm long.

Erihadrosia lived in shallow shelf environments around New Zealand during the Middle Miocene.

—Written by Jeffrey H Robinson

Specimen number: OU 6957 Age: Approximately 14 million years old (middle Miocene, Lillburnian stage)
Locality:  Cucullaea Shellbed, Clifden, Southland Rock Formation: Clifden Limestone
Collected by: JD Campbell and others
Citation: Hiller N, MacKinnon DI. 2000. A reappraisal of the systematics of the Stethothyris group of brachiopods from the Cenozoic of New Zealand and Australia. New Zealand Journal of Geology and Geophysics 43:59–81. doi.org/10.1080/00288306.2000.9514870
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