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GEUS Bulletin no 5.pmd

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BATHONIAN CALLOVIAN<br />

species as the depositional settings of these localities<br />

are comparable overall. However, a Callovian range is<br />

reported from the present Arctic regions of the Sverdrup<br />

Basin and Svalbard (Smelror 1993).<br />

Some exceptionally early occurrences of Ambo<strong>no</strong>sphaera<br />

calloviana and Gonyaulacysta helicoidea in<br />

the A. ishmae Chro<strong>no</strong>zone and of Pareodinia stegasta<br />

and Paraevansia brachythelis in the C. apertum Chro<strong>no</strong>zone<br />

are recorded in the present succession.<br />

104<br />

BOREAL AMMONITE<br />

ZONATION<br />

Erym<strong>no</strong>ceras coronatum<br />

Kosmoceras jason<br />

Sigaloceras calloviense<br />

Proplanulites koenigi<br />

Succession at<br />

Ravn Pynt<br />

Succession south<br />

of Ravn Pynt<br />

LITHO-<br />

STRATIGRAPHY<br />

Cadoceras <strong>no</strong>rdenskjoeldi Spath<br />

Plateau<br />

Member<br />

Cadoceras apertum<br />

Cadoceras calyx<br />

Cadoceras variabile<br />

Arcticoceras cra<strong>no</strong>cephaloide<br />

Arcticoceras ishmae<br />

Arctocephalites greenlandicus<br />

Arctocephalites arcticus<br />

FAUNA HORIZONS<br />

31<br />

26<br />

22<br />

20<br />

19<br />

16<br />

15<br />

Pelion Formation<br />

Hiatus<br />

<strong>GEUS</strong> <strong>Bulletin</strong> <strong>no</strong> <strong>5.pmd</strong> 104<br />

29-10-2004, 11:14<br />

?<br />

Fig. 3. Schematic stratigraphical<br />

classification of the Middle Jurassic<br />

succession on Store Koldewey.<br />

The di<strong>no</strong>flagellate cysts in the Middle Jurassic succession<br />

are divided into an Upper Bathonian and a<br />

Lower Callovian di<strong>no</strong>flagellate cyst assemblage. The<br />

boundary is placed at 19.2 m, above which level a<br />

significant number of new species appear (Figs 2, 4).<br />

Most species in the Upper Bathonian assemblage also<br />

occur in the Lower Callovian assemblage and the composition<br />

of the Bathonian assemblage varies significantly<br />

between the few samples studied. The younger,

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