LATE
ALBIAN (UPPER GAULT) |
Stratigraphy at Folkestone |
based
on a section between Copt Point and East Wear Bay |
Sub-Stage |
Ammonite Zone | Ammonite Subzone | Bed |
Lithology |
Metres | |
LATE ALBIAN (UPPER GAULT) | Stoliczkaia
dispar |
Mortoniceras (Durnovarites) perinflatum |
XIII |
FAWNISH GREY MARLY CLAY | 8.84 | |
Mortoniceras (Mortoniceras) rostratum | MOTTLED LIGHT GREY AND FAWN GREY MARLY CLAY |
0.91 | ||||
BLUISH PALE GREY MARLY CLAY HIGHLY GLAUCONITIC AT BASE BUT GLAUCONITE GRAINS DIMINISH UPWARDS IN SIZE AND NUMBER |
3.96 | |||||
Callihoplites auritus |
XII |
HIGHLY CLAUCONITIC LIGHT GREY WITH SCATTERED PHOSPHATIC NODULES AND A SEAM OF THEM AT BASE |
0.99 | |||
XI |
PALE GREY MARLY CLAY WITH PHOSPHATIC NODULE BED AT BASE | 10.67 | ||||
Hysteroceras varicosum | 1.55 | |||||
X |
TOUGH LIGHT GREY MARLY CLAY WITH PHOSPHATIC NODULES AT TOP AND IN A SEA AT 0.73 M BELOW TOP | |||||
IX |
LIGHT GREY MARLY CLAY INDURATED AT TOP WHICH IS MARKED BY PHOSPHATIC NODULES. MARLSTONE LENTICLES OCCUR BETWEEN 0.76M AND 1.7M ABOVE BASE. |
2.85 | ||||
VIII |
(iii) PHOSPHATIC NODULES AND PART-PHOSPHATISED FOSSILS IN SHELLY GREY CLAY | 0.075 to 0.1 | ||||
(ii) MID-GREY CLAY WITH NUMEROUS Inoceramus (Birostrina) sulcata | 0.225 to 0.28 | |||||
(i) BLACK PHOSPHATIC NODULES IN SHELLY CLAY |
0.05 | |||||
Middle Albian (Lower Gault) (part) |
Euhopliteslautus (part) |
Anahoplites daviesi (part) | VII |
Reference: Owen H.G. 1976 The Stratigraphy of the Gault and Upper Greensand of the Weald Proc. Geol. Ass. 86 475-98 |