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UTRECHT MICROPALEONTOLOGICAL BUllETINS

UTRECHT MICROPALEONTOLOGICAL BUllETINS

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Remarks: Throughout the Oland sections, the oistodiform element remained<br />

very constant in· shape, whereas both the ozarkodinaform element (= the<br />

Prioniodina inflata-like elements, Pl. 4, figs. 18~20) and the multiramiform<br />

elements (= the elements of the Periodon transition series of Lindstrom<br />

1964; see for instance Pl. 4, figs. 15-17) underwent considerable changes in<br />

shape.<br />

The older forms of the ozarkodinaform elements had a short and undenticulated<br />

base (Pl. 4, fig. 18). They also lacked the oulodus-like bending,<br />

described by Lindstrom (1964). The anterior process was hardly developed<br />

and undenticulated. The illustrations of plate 4, figs. 18 to 20, show the<br />

gradual change to the ozarkodinaform elements described as Prioniodina<br />

inflata LINDSTROM, 1955.<br />

The early forms of the multiramiform elements were hardly denticulated<br />

if at all (Pl. 4, fig. 15). The basal sheath was higher and the cusp wider and<br />

flatter, compared to the later forms (Pl. 4, figs. 16 and 17). The change to<br />

the more conspicuously denticulated forms was very gradual.<br />

Biometrical and statistical data probably will enable the distinction of<br />

several species within this lineage. For the time being, they are all placed in<br />

one multi-element species.<br />

Regional occurrence: At Kopingsklint the species occurs from the top of<br />

member K k2 up to and including the top portion of the Bruddesta Formation.<br />

In section 6 from member Ka- d 1 up to and including the lowermost<br />

portion of the Horns Udde Formation. Near Horns Udde from the top of<br />

member K k2<br />

up to a level at about 2.80 m. over the base of the Bruddesta<br />

Formation.<br />

Biostratigraphic range: Periodon flabellum was found from the Triangulodus<br />

SlAbtilis/Gothodus microdentatus Assemblage Zone up to and including the<br />

lower portion of the Triangulodus brevibasis Assemblage Zone (fig. 15).<br />

Genus Pravognathus STAUFFER, 1936<br />

Type species: Heterognathus idoneus STAUFFER, 1935.<br />

Definition: "Base thin, long, slender, straight or slightly arched and twisted<br />

just anterior to the middle; lintler side of base with narrow groove extending<br />

entire length,. slightly widening and deepening beneath the arch or beneath<br />

the more prominent denticles; the upper edge of base bears 2, 3 or 5, possibly<br />

more, large, long, pointed, orally flattened, aborally rounded denticles on<br />

the arched or twisted portion; these may incline in various directions. Anterior<br />

limb or portion of base bears 4 or 5, possibly more, denticles of decreasing<br />

size; posterior limb bears 10 to 12, possibly more, small laterally flattened,

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