Arkell.1956.Jurassic..

RUSSIA AND THE EUROPEAN ARCTIC
fragment of Q. holtedahli Salfeld & Frebold, 1924, pi. i, figs. 3, 4, type from
Novaya Zemlya). Q. lamberti was collected in King Charles Islands.
LOWER CALLOVIAN AND UNDATED
Possibly part of the 40 m. of unfossiliferous shales and sandstones resting
on the Trias at Festungsprofil is represented by shales in Ice Fiord and at
South Cape which have yielded Kepplerites (Seymourites) tychonis Ravn,
K. (S.) svalbardensis Bodyl. and Cadoceras cf. crassum Mads. (Frebold,
1929, pi. ii, 1930, pi. vii, fig. 1; Sokolov & Bodylevsky, 1931, pi. v, figs.
1, 2), correlating approximately with the Koenigi Zone. On King Charles
Islands earlier Lower Callovian is represented by Arctocephalites arcticus
(Newton) (Frebold, 1951, p. 79).
? BATHONIAN
In King Charles Islands the earliest fossiliferous Jurassic, following
a thick sandy series, consists of some shaly sandstones containing a pelecypod
assemblage which includes such typical Great Oolite forms as
Meleagrinella echinata (Smith), M. braamburiensis (Phil.), Pteroperna
emarginata Morris & Lycett and Lima cf. semicircular is Goldf. On the
strength of this faunule Pompeckj (1899a) assigned the beds to the
Bathonian.
No other Bathonian occurs in the Spitsbergen area nor in Franz Joseph
Land. It must be emphasized that the placing of the Arctocephalites
beds in the Bathonian by Spath did not result from 'revision of the
ammonites' (Frebold, 1951, p. 79), but was simply a matter of nomenclature,
Spath having unfortunately decided to classify the basal Callovian
Macrocephalus Zone in the Bathonian. No Bathonian ammonites are
known from the Arctic.
TOARCIAN
In several areas (not Festungsprofil) the base of the Jurassic is formed
by a phosphatic conglomerate, containing Upper and Middle Toarcian
ammonites: Pseudolioceras compactile (Simpson), 'Coeloceras' polare Frebold,
Dactylioceras annuliferum (Simpson), Grammoceras cf. saemanni
(Dumortier), with belemnites and pelecypods (Frebold, 1929, pi. i; 1930,
pi. vi; Bodylevsky, 1929). This thin bed has a wide distribution and
always rests on Trias. It is a condensed and possibly a remanie bed
(Weir, 1933, p. 693).
ANDOE ISLAND, LOFOTEN ISLANDS
On the isle of Andoe in the Lofotens, off the north coast of Norway,
about 10 sq. km. of the coastal flat is underlain by Jurassic and Cretaceous
sediments. The beds are faulted down into the granitic basement in a
way similar to the outliers in the Hebrides. They are almost completely
concealed by Quaternary deposits and are known only from borings for
coal. The total thickness is at least 510 m.
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