Brachiopod
Brachiopods, also known as lamp shells, are a group of marine invertebrates that belong to the phylum Brachiopoda. Brachiopods are known for their hard "shells" on the upper and lower surfaces, which are unlike the left and right arrangement seen in bivalve mollusks. These organisms have a rich fossil record, dating back to the Cambrian period, making them important for paleontological studies. Despite their once vast diversity and abundance, modern brachiopods are less common and are primarily found in cold and deep marine environments.
Anatomy and Physiology[edit | edit source]
Brachiopods are characterized by their two shells or valves: the ventral valve, which is often larger, and the dorsal valve. These valves are composed of calcium carbonate and are connected by a hinge at the rear, allowing them to open and close. Inside, brachiopods have a lophophore, a specialized feeding organ that also functions in gas exchange. The lophophore is a crown of ciliated tentacles that filters food particles from the water.
Classification[edit | edit source]
The Brachiopoda phylum is divided into two main classes: the Rhynchonellata, which have ribbed shells, and the Lingulata, which have smooth shells and a stalk for attachment to the seabed. These classes are further divided into orders and families based on characteristics such as shell shape, hinge structure, and lophophore arrangement.
Ecology[edit | edit source]
Brachiopods are sessile organisms, meaning they are fixed in one place and do not move around. They are benthic, living on the sea floor, and are found in a range of marine environments from shallow waters to depths of several thousand meters. Brachiopods are filter feeders, using their lophophores to capture food particles suspended in the water.
Evolution and Fossil Record[edit | edit source]
Brachiopods were most abundant during the Paleozoic era, particularly in the Ordovician, Silurian, and Devonian periods. They suffered significant declines during the Permian-Triassic extinction event, but some groups survived and continued to the present day. The fossil record of brachiopods is extensive and includes thousands of described species, making them important indicators of environmental conditions in past geological periods.
Conservation[edit | edit source]
Today, brachiopods are considered relatively rare compared to their historical abundance. Some species are threatened by habitat destruction, pollution, and the effects of climate change on ocean chemistry, particularly ocean acidification, which can affect their shell formation. Conservation efforts are focused on protecting marine habitats and understanding the impacts of environmental changes on brachiopod populations.
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Contributors: Prab R. Tumpati, MD