Argyrotheca

Some Argyrotheca species have red stripes radiating from the pedicle opening (or foramen). These species are among a few living brachiopods with color marking on the shell. All other colored brachiopods are from shallow water too. This kind of color patterns may be a form of camouflage. The shell is biconvex with two high and wide ribs radiating close to the midline (a shell-shape called strangulate) and four radiating ribs of declining height and width further lateral (a shell-shape called oppositely multiplicate), smooth or more commonly multiplicate. The inner surface of the shell has many rather coarse pits (or punctae). The larger valve (pedicle valve or ventral valve) has a fairly short stump beak (or subtruncate). The pedicle opening (or foramen) is large (about a third of the maximum with of the shell), almost entirely situated in the backfolding part (or delthyrium) of the pedicle valve (submesothyridid to almost hypothyridid), leaving ample space for the small deltidial plates. The pedicle collar is well developed, and is supported by median ridge (or septum).The lophophore is large. Differences with related genera Argyrotheca resembles Megathiris, but Argyrotheca has one partition in the middle of the inside of the pedicle valve (the medial dorsal septum) and a lophophore indented in the middle but without lobation of the branches (or schizolophous), while Megathiris has three septa and a lophophore with lobed branches (or ptycholophous). Joania, which was recently split from Argyrotheca, can be distinguished by the radial ribs on the inside of the peduncle valve that end in tubercles somewhat removed from the margin, and a row of tubercles on the edge of the septum. == Taxonomy ==

A. rubrocostata does not have a brood pouch and has separate sexes. This cast doubts on the monophyly of Argyrotheca. Reassigned species • A. arguta = Joania arguta • A. cordata = Joania cordata == Ecology ==

Reproduction Unique among extant brachiopods, Argyrotheca and Joania are hermaphrodite. Another most unusual specialization, in both these genera, is that the eggs (or ovae) are retained in the enlarged nephridia that act as a brood pouch. Fertilization takes place with its own sperm or after sperms have entered with the inhalant water current. Here early larval development takes place. The fertilized ova develop into ciliated larvae with a feebly free-swimming life of at most a few days before settling and metamorphosis into a tiny brachiopod fixed to the substrate.). This implies that reproduction needs to be both quick and efficient. Being hermaphrodite allows for quick and efficient self-fertilisation, and the brood pouch would reduce predation of the larvae. Attachment Near Bermuda Argyrotheca is mostly found on the underside of leaf-shaped corals, like Agaricia, Mycetophyllia or Montastraea or in between branches of corals, such as Porites, Mussa and Madracis, up to about 75 m. Further down, sponges like Agelas and Plakorthis, and concretions dominante as substrate. Another study of fossil A. cuneata showed a large difference between two nearby (2 km) and almost contemporary (Middle Miocene, Serravallian) locations in Poland. At Węglin, 23% of the shells had holes, but only 2% at Weglinek. Here two types of holes were distinguished: conical, assigned to naticid molluscs, and cylindrical holes, that are assumed to be made by muricate sea snails. Agyrotheca shakes forcefully when disturbed by animals swimming by and when disposing of particles. File:Argyrotheca cuneata brachial recent.jpg|Argyrotheca cuneata, brachial valve, 2 mm across, found at 33 m deep, near Rome, Italy File:Argyrotheca cureata posterior recent.jpg |anterior view File:Argyrotheca cuneata lateral recent.jpg|lateral view == Distribution ==

Argyrotheca is known from the Upper Cretaceous in Europe and North America, from the Eocene in Europe, North and Latin America and the West Indies, from the Oligocene in Europe and Mexico, from the Miocene in Europe, the Russian Federation, North America, the West Indies and New Zealand, and from the Pliocene in England and Italy. It can currently be found in the Atlantic (60-1280m), Pacific (160m), Mediterranean (6-400m), A. cistellula, A. cordata and A. cuneata are the only species present in the Mediterranean. == Species ==

A. ageriana A. ageriana, has been described from the lower Pleistocene of Italy (Castro Marina, Lecce, Apulia). It lived in a temperate to warm-temperate sea, 75–100 m deep. A. cistellula A. cistellula is a minute brachiopod, dirty white to yellow or grey in color, and has a maximum size of 2 x 3 mm. The brachial valve is rounded rectangular, a bit wider than long, or square in outline. This valve is slightly bilobed. The hinge line is straight and spans the entire width of the shell. Externally the surfaces are smooth or show faint concentric growth lines. The inner surfaces of the shell have small pits (or is endopunctate). The peduncle valve is moderately convex and has a short drop-shape, with a straight beak (or umbo), and a straight margin opposite to the hinge. The opening for the peduncle (or foramen) is large, - of the total width and the triangular plates that bridge the distance between the dorsal and ventral surfaces of the shell (or deltidial plates) do not touch. This species attaches itself to hard substrates, in water between 20–100 m. The current known distribution of A. cistellula is Norway, the United Kingdom and Ireland (north-east Scotland, English Channel, west coast of the British Isles), and Italy (Sardinia and Sicily). A. cuneata Living specimens of A. cuneata have been reported from a submarine cave in Cyprus (Cape Greco, 6 m deep, with two other brachiopod species: Novocrania turbinata and Megathyris detruncata), and the Cape Verde Islands (Tarrafal, northwestern coast of Sao Tiago Island, 15 m deep). The species is also reported from the outer shelf (100–200 m deep), off the coast of Brazil (Rio de Janeiro, São Paulo, and Parana states), on carbonate rich sediment, where they are attached to shell fragments like those of bivalves. == References ==