Arkell.1956.Jurassic..

POLAND
monographed by Neumayr (1871), has a 'mixed' aspect. Teisseyre
(1887), who first described the genus Proplanulites from the Balin Oolite,
handled over 10,000 arnmonites from it, but saw only two specimens of
Lytoceras and none of Phylloceras. The following is a list of the ammonites
figured in Neumayr's classic monograph, embodying numerous subsequent
changes of nomenclature.
Hecticoceras laubei (Neum.), pi. ix, fig. 4
Hecticoceras krakoviensis (Neum.), fig. 5
Hecticoceras balinense Bonarelli, fig. 6
Hecticoceras taeniolatum Bonarelli, fig. 7
Hecticoceras metomphalum Bonarelli, fig. 8
Torricellites uhligi (Parona & Bonarelli), fig. 9
Procerites sp., pi. x, fig. 1, pi. xi, fig. 1
? Orionoides sp., pi. x, figs. 2, 3
Proplanulites majesticus Buckman, pi. xi, fig. 2
Proplanulites sp., fig. 3
Proplanulites cf. spirorbis (Neum.), fig. 4
Subgrossouvria euryptycha (Neum.), pi. xii, fig. 1
Grossouvria anomala Loczy, fig. 2
Siemiradzkia de mariae (Parona & Bonarelli), fig. 4
Wagnericeras sp., fig. 6
Indosphinctes sp., pi. xiii, fig. 1
Indosphinctes pseudopatina (Parona & Bonarelli), fig. 2
Choffatia funata (Oppel), pi. xiv, fig. 1
Choffatia evoluta (Neum.), fig. 2
Grossouvria subtilis (Neum.), fig. 3
Choffatia furcula (Neum.), pi. xv, fig. 1
Choffatia balinensis (Neum.), fig. 2
Parapatoceras calloviense (Morris), p. 46
In the Cracow area conglomerates in the Callovian contain pebbles
derived from Palaeozoic rocks and in at least one locality a 0-4 m. marl
belonging to the Lamberti Zone rests directly on Upper Carboniferous
porphyry (Dzulynski, 1952, p. 168). In the hills SW. of the Lysa
Gora, however, the Callovian reaches a thickness of about 33 m. It
consists of sandy marls with subordinate bands of limestone, partly
silicified, and chert, and yields Macrocephalites, Reineckeia and Erymnoceras
(Swidzinski, 1931, p. 851).
Very different is the facies to the north-east, where at Lukow, 65
miles ESE. of Warsaw, a brickfield is worked in an erratic mass of
unstratified clay 4 m. thick, containing nodules with splendidly preserved
ammonites mainly of the Upper Callovian (Makowski, 1952). A few
nodules found in a separate part of the workings yield only Cadoceras
tschefkini (d'Orb.), gen. nov. (aff. Longaeviceras) sp. nov. (Makowski,
pi. vi, figs. 1-3), and schumarovi (Nik.) (pi. v, 10); the age of these is
probably Athleta Zone or Middle Callovian. All the other ammonites
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