15.11.2013 Views

UTRECHT MICROPALEONTOLOGICAL BUllETINS

UTRECHT MICROPALEONTOLOGICAL BUllETINS

UTRECHT MICROPALEONTOLOGICAL BUllETINS

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Type-stratum: The limestone bed in member Kk2 from which sample 12 was<br />

taken, see chart II.<br />

Remarks: This assemblage zone was based on one single sample (12, section<br />

1, chart II). Cordylodus rotundatus was not actually found in this zone, but<br />

it might form part of it, according to its deduced regional range (fig. 15).<br />

Drepanoistodus numarcuatus was not found anymore above this zone.<br />

II.2.4.8. The Triangulodus subtilis/Gothodus microdentatus Assemblage<br />

Zone<br />

Diagnosis: A conodont assemblage zone defined by the total range of<br />

Gothodus microdentatus and by the occurrence of Triangulodus subtilis<br />

before the first appearances of Scolopodus rex and Oelandodus elongatus<br />

(chart II and fig. 15).<br />

Description: In the rock-sequence of Kopingsklint Gothodus microdentatus,<br />

Triangulodus subtilis, Drepanoistodus conulatus and Periodon flabellum start<br />

their range together in this zone. They were found together with Cordylodus<br />

angulatus, Paroistodus amoenus, P.parallelus, Scolopodus peselephantis,<br />

Drepanodus arcuatus, Paracordylodus gracilis, Protopanderodus longibasis,<br />

Prioniodus deltatus, Drepanoistodus inconstans and Dforceps.<br />

Type-locality: Kopingsklint, section l.<br />

Type-strata: The two upper limestone beds of member Kk 2.<br />

Remarks: This assemblage zone was recognized in only one sample (13 in<br />

section 1, see chart II). Paroistodus amoenus and Gothodus microdentatus<br />

seem to terminate their range at the top of this zone. Cordylodus rotundatus<br />

was not actually found in this zone, but it might occur in it according to its<br />

regional range (fig. 15).<br />

11.2.4.9. The Prioniodus elegans/Oelandodus elongatus Assemblage Zone<br />

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

Prioniodus elegans and Oelandodus elongatus before the first appearance of<br />

Stolodus stoia (chart III and fig. 15).<br />

Description: In the rock-sequence of section 6 Prioniodus elegans, Oelandodus<br />

elongatus and Scolopodus rex start their range with a considerable<br />

number of species, known from the previous zones at Kopingsklint and near<br />

Horns Udde: Scolopodus peselephantis, Drepanodus arcuatus, Protopanderodus<br />

longibasis, Prioniodus deltatus, Drepanoistodus forceps, D.conulatus,<br />

Paroistodus parallelus and Periodon flabellum.<br />

Type-locality: The coastal cliff between Aleklinta and Djupvik, section 6.<br />

Type-stratum: The basal glauconitic bed of member Ka- d 1, sample 2, chart<br />

III.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!