E. Urquhart et Ft. Banner, BIOSTRATIGRAPHY OF THE SUPRA-OPHIOLITE SEDIMENTS OF THE TROODOS MASSIF, CYPRUS - THE CRETACEOUS PERAPHEDHI, KANNAVIOU, MONI AND KATHIKAS FORMATIONS, Geological Magazine, 131(4), 1994, pp. 499-518
The Troodos Massif of Cyprus exposes a classic and much-studied ophiol
ite sequence representing oceanic crust of Late Cretaceous age. K-Ar d
ating of the sheeted dykes and of the overlying pillow lavas gives a r
ange of 83 +/- 3 Ma (earliest Campanian) and 75 +/- 5 Ma (late Campani
an) respectively. for the formation of the upper levels of the ophioli
te. An authochthonous sequence of Late Cretaceous to Recent age sedime
nts is exposed resting on the ophiolite, the oldest part of which refl
ects sedimentation in an apparently deep marine, oceanic setting. Litt
le biostratigraphical information is available to constrain the chrono
stratigraphy of these sediments in relation to the complex geological
history of the island, including the uplift and unroofing of the ophio
lite, despite their richness in microfauna and flora. This paper provi
des an integrated biostratigraphical study based on radiolaria, plankt
onic foraminifera and calcareous nannofossils of the oldest part of th
e supra-ophiolite succession, of the Cretaceous Perapedhi, Kannaviou,
Moni and Kathikas formations. For the first time, well-defined micropa
laeontological evidence establishes the relative ages of these formati
ons. The umbers of the Perapedhi formation are no younger than Campani
an in age while the volcaniclastic sediments of the Kannaviou formatio
n were also deposited during Campanian times. The matrix of the Moni f
ormation contains a microfauna consistent with the hypothesis that it
is derived from the Kannaviou. In contrast, the Kathikas formation is
composed of sediment derived mainly from the allochthonous Mamonia com
plex, but autochthonous pelagic interbed horizons demonstrate that it
was deposited probably within a very short time interval during the la
te Maastrichtian. Key index species are figured, including the first p
ublished micrographs of Cretaceous planktonic foraminifera from Cyprus
.