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Clam shrimp (once Conchostraca) are a taxon of bivalved branchiopod crustaceans that resemble the unrelated bivalved molluscs.[1] They are extant, and known from the fossil record, from at least the Devonian period and perhaps before.[2] They were originally classified in a single order Conchostraca, which later proved to be paraphyletic, being separated into three different orders: Cyclestherida, Laevicaudata, and Spinicaudata.

Clam shrimp
Temporal range: Devonian–Recent
Estherien 250909.jpg
Palaeestheria minuta, Ladinian, Germany
Scientific classification
Sars, 1899
Linder, 1945
Linder, 1945


Both valves of the shell are held together by a strong closing muscle. The animals react to danger by contracting the muscle, so that the valves close tightly and the crustacean, as if dead, lies motionlessly at the bottom of the pool.

In most species the head is dorsoventrally compressed. The sessile compound eyes are close together and located on the forehead; in the genus Cyclestheria they are truly fused. In front of them is a simple naupliar eye. The first pair of antennae is reduced and unsegmented. The second pair of antennae, however, is long and biramous. Both branches are covered with numerous bristles. The crustaceans swim primarily by swooping the antennae. In the common genus Lynceus, which can open its spherical valves wide, the thoracic legs move in an oar-like manner along with the antennae.

The number of segments constituting the thorax varies from 10 to 32, and the number of legs varies accordingly. They are similar in structure to the legs of tadpole shrimp, and similarly, their size decreases from front to back. In females, the outer lobes of several middle legs are modified into long, upward-bending threadlike outgrowths, used to hold the eggs on the dorsal side of the body under the shell. However, the main functions of the thoracic legs are respiration and carrying food forward to the mouth. The gills are basically the outer lobes of all thoracic legs that are closest to the base of the leg. The legs are in constant movement, and the water between the valves of the carapace is quickly renewed. The body ends in a large chitinised telson, which is either laterally compressed and bears a pair of large hooks, or dorsoventrally compressed, with short hooks.

Reproduction and developmentEdit


Clam shrimp have different reproductive strategies. For example, within the family Limnadiidae are found dioecious (male-female), hermaphroditic (only hermaphrodites), and androdioecious (male-hermaphrodite) species.

Life cycleEdit

The eggs are surrounded by a tough shell and can withstand drying out, freezing and other hostile conditions. In some species these eggs can hatch after as long as 7 years.

When the egg arrives in a suitable pool, a larva hatches out at the nauplius stage. Clam shrimp nauplii are distinguished by very small front antennae. At the second stage (metanauplius), the larva develops the small shell. They develop very quickly. For instance, Cyzicus reaches sexual maturity in 19 days after hatching.


California clam shrimp, Cyzicus californicus

Extant clam shrimp belong to three orders, divided into five families;[3] some notable genera and prehistoric taxa are also listed:

Geological historyEdit

Modern clam shrimp have little significance to humans. However, extinct species of these crustaceans are often studied by geologists. In freshwater deposits, generally poor in fossils, the well-preserved clam shrimp shells are found quite often. They help identify the age of the corresponding strata.

During the past geological periods clam shrimp were apparently more numerous and diverse than they are now. 300 extinct species are known, and half as many living species. The oldest clam shrimp, such as Asmussia murchisoniana, were found in Devonian deposits. Many extinct species, especially Triassic ones, lived in the sea, where no clam shrimp remain today.


  1. ^ J. Webb (1979). "A reappraisal of the palaeoecology of conchostracans (Crustacea: Branchiopoda)". Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen. 158 (2): 259–275.
  2. ^ K. J. Woolfe (1990). "Trace fossils as paleoenvironmental indicators in the Taylor Group (Devonian) of Antarctica". Palaeogeography, Palaeoclimatology, Palaeoecology. 80 (3–4): 301–310. doi:10.1016/0031-0182(90)90139-X.
  3. ^ Joel W. Martin & George E. Davis (2001). An Updated Classification of the Recent Crustacea (PDF). Natural History Museum of Los Angeles County. p. 132.

External linksEdit