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UTRECHT MICROPALEONTOLOGICAL BUllETINS

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section 6. Paracordylodus gracilis was only found in the uppermost sample,<br />

but according to its decuded regional range, it might be found throughout<br />

this zone.<br />

11.2.4.12. The Pro topanderodus rectus/O~pikodus evae Assemblage Zone<br />

Diagnosis: A conodont assemblage zone characterized by the concurrence of<br />

the ranges of Protopanderodus rectus and Oepikodus evae prior to the first<br />

occurrence of Oistodus lanceolatus (charts II, III and IV, fig. 15).<br />

Description: In the small rock-section of locality 2 near Horns Udde (see<br />

figs. 5 and 15) Protopanderodus rectus and Oepikodus evae were found<br />

together with Scolopodus peselephantis, Drepanodus arcuatus, Pro topanderodus<br />

longibasis and Prioniodus deltatus, the latter four species being<br />

known from lower zones in this section. In the same sample Drepanoistodus<br />

forceps, Paroistodus parallelus, Paracordylodus gracilis, Periodon flabellum,<br />

Oelandodus elongatus, Scolopodus rex and Stolodus stola appear for the first<br />

time in the rock-section near Horns Udde (chart IV). The latter seven species<br />

were already known from older assemblages elsewhere in the area and they<br />

were found throughout this zone (charts II, III and IV, fig. 15).<br />

Type-locality: Locality 2 near Horns Udde (see fig. 5).<br />

Type-stratum: A limestone bed from the upper part of member Kk2 from<br />

which sample III was obtained (see chart IV the inset).<br />

Remarks: This zone was primarily based on the fauna of sample III from the<br />

small rock-section near Horns Udde (see chart IV the inset). It was subsequently<br />

recognized in section 6 and 1. Paracordylodus gracilis is absent in<br />

sample 7 of section 6 and in sample 14 of section 1, both were taken from<br />

the basal glauconitic layer of member Kk 3' Drepanoistodus conulatus does<br />

occur in sample 14 of section 1, contrary to the assemblage typical for this<br />

zone near Horns Udde. Paracordylodus gracilis seems to end its range within<br />

this zone (see fig. 15).<br />

II,2.4.13. The Oistodus lanceolatus/Prioniodus deltatus Assemblage Zone<br />

Diagnosis: A conodont assemblage zone characterized by the overlap of the<br />

ranges of Oistodus lanceolatus and Prioniodus deltatus (charts III and IV,<br />

fig. 15).<br />

Description: In one sample (no. 9) of section 6 Oistodus lanceolatus and<br />

O.papiliosus start their ranges, whereas Prioniodus deltatus and Oelandodus<br />

elongatus occur for the last time. A similar overlap was found near Horns<br />

Udde in the sample suite IV to 7b (chart IV). The only difference is that<br />

Oelandodus elongatus stops before the top of the zone here. In addition,

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