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the echinoid fauna from japan and adjacent regions part i

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212 S. NISIYA'VIA<br />

76, pI. 1, figs. 1-3, 6-12, pI. 2, figs. 9-15, 19-21,pl. 45, figs. 27-28, text-figs. 53,55b (widely<br />

distributed all over <strong>the</strong> Indo-Pacific <strong>regions</strong>, <strong>from</strong> East Africa to Japan, in depths about<br />

0--45 metres).<br />

Temnotrema POMEL, 1883, p. 87 (non A. AGASSIZ, 1863).-LAMI3ERT <strong>and</strong> JEANNET, 1935, p. 6.<br />

Haplotype.-Temnopleurus hardwiekii (GRAY) A. AGASSIZ, 1872-74, pp. 166, 460, pI. 8a, figs.<br />

1-3 (Japan) (in which A. AG.'\SSIZ included Te11l1lotrema seulptum, a quite distinct<br />

species).<br />

Test of moderate or small size, low, hemispherical or subconical, or flattened<br />

above; generally slightly sunken at <strong>the</strong> peristomial edge. Pore-zones narrow, only<br />

in <strong>the</strong> largest specimens slightly widening adorally; pore-pairs arranged more or less<br />

distinctly in slightly oblique arcs of three. Trigeminate ambulacral plates of <strong>the</strong><br />

<strong>echinoid</strong> structure throughout; each plate with a primary tubercle of about <strong>the</strong> same<br />

size as <strong>the</strong> interambulacral primaries. Secondary tubercles in larger specimens well<br />

developed in <strong>the</strong> ambital region, almost as large as <strong>the</strong> primaries, forming horizontal<br />

<strong>and</strong> longitudinal series. Horizontal sutures aborally with deep <strong>and</strong> usually large pits,<br />

in ambulacra only one pit, ranging <strong>from</strong> <strong>the</strong> median suture to <strong>the</strong> base of <strong>the</strong> primary<br />

tubercle; in interambulacra two pits, one <strong>from</strong> median suture, <strong>the</strong> o<strong>the</strong>r <strong>from</strong> outer,<br />

adradial edge, <strong>the</strong> two being separated by <strong>the</strong> primary tubercle; pits sometimes<br />

widened towards <strong>the</strong> primary tubercle; on <strong>the</strong> oral side <strong>the</strong> pits become smaller or<br />

quite obsolete. Primary tubercles distinctly crenulate; <strong>the</strong> boss is sometimes distinctly<br />

serrate especially below <strong>the</strong> ambitus. There may be more or less distinct depressions<br />

on <strong>the</strong> plates, radiating <strong>from</strong> <strong>the</strong> primary tubercle. Apical system dicyclic, with<br />

subcentral or pronouncedly eccentric position of <strong>the</strong> anal opening. Peristomial membrane<br />

<strong>and</strong> buccal plates naked; in <strong>the</strong> adoral edge some small plates, outside <strong>the</strong><br />

buccal plates. Gill-slits very shallow; gills small, bush-shaped. Primary spines simple,<br />

finely striated; marginal spines flattened towards <strong>the</strong> end, which is more or less<br />

concave on <strong>the</strong> adoral side; peristomial spines usually curved, somewhat widened<br />

<strong>and</strong> flattened at <strong>the</strong> point. Secondary spines simple, pointed. Globiferous pedicellariae<br />

of one kind only, with or without lateral teeth. Spicules simple, bihamate, or sometimes<br />

biacerate (<strong>from</strong> MORTENSEN, 1943).<br />

The main point of distinction between this genus, to which Tem. alex<strong>and</strong>ri (BELL,<br />

1884) (Salmacis alex<strong>and</strong>ri BELL, 1884-b, p. 118.-Sal. virgulata val'. DODERLElN, 1903,<br />

p. 713, pI. 42, figs. 5-7a) is referred, <strong>and</strong> <strong>the</strong> allied genus Salmacis is that in Temnopleurus<br />

<strong>the</strong>re are large <strong>and</strong> deep sutural pits, while in <strong>the</strong> o<strong>the</strong>r <strong>the</strong>re are only<br />

angular pores.<br />

Temnopleurus is a well known genus among <strong>the</strong> family of <strong>the</strong> Temnopleurids,<br />

being characterized by <strong>the</strong> long <strong>and</strong> sharp angular pits, <strong>and</strong> by <strong>the</strong> well crenulated<br />

primary tubecles, of which one to three or rarely more are found on a coronal plate<br />

at <strong>the</strong> ambitus. Among <strong>the</strong> species which once placed in <strong>the</strong> genus Temnopleurlls<br />

by LAMBERT <strong>and</strong> THIERY (1911, p. 218), Tem. neuvillei LAMBERT, 1912 (LAMBERT,<br />

1912-a, p. 25, pI. 1, figs. 12-14-Eocene) <strong>and</strong> Tem. tuberclllosliS HAIME, 1853 (D'ARCHIAC<br />

<strong>and</strong> HAIME, 1953-54 (53), p. 206, pI. 13, fig. 11.-DuNCAN <strong>and</strong> SLADEN, 1882-a, p. 85,<br />

pI. 13, figs. 16-17) must be removed <strong>from</strong> this genus, <strong>and</strong> <strong>the</strong> former species is to be<br />

referred to Medocechinus JEANNET, 1936 (jEANNET, 1936-a, p. 2), <strong>and</strong> <strong>the</strong> latter to<br />

Trllmechinus LAMBERT <strong>and</strong> THIERY, 1911 (1911, p. 218). Among <strong>the</strong> fossil, <strong>the</strong> species<br />

described by HERKLOTS <strong>from</strong> <strong>the</strong> Miocene of Java, Tem. areolatus HERKLOTS (1854,

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