. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology. CIFELLI : BATHONIAN FOUAMINIFERA OF ENGLAND 260 111 general, the major units of the Great Oolite Series (often, but not always designated as formations) are as follows, in ascending order: Fuller's Earth Clay, Great Oolite Limestones, STAGE DORSET COAST BATH AREA < FORAM OBTAINED LUWER CORNBRASH LOWER CORNBRASH LOWER CORNBRASH LOWER CORNBRASH GREAT OOUTE Ls UPPER FULLER'S EARTH CLAY WATTONENSIS BEOS WYCHWOOD BEDS BRADFORD CLAY KEMBLE BEOS BUSWORTH CLAY UPPER FULLERS EARTH CLAY. (=MAINLY HAMPEN MARLY BEDS ? ARKELL,1
. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology. CIFELLI : BATHONIAN FOUAMINIFERA OF ENGLAND 260 111 general, the major units of the Great Oolite Series (often, but not always designated as formations) are as follows, in ascending order: Fuller's Earth Clay, Great Oolite Limestones, STAGE DORSET COAST BATH AREA < FORAM OBTAINED LUWER CORNBRASH LOWER CORNBRASH LOWER CORNBRASH LOWER CORNBRASH GREAT OOUTE Ls UPPER FULLER'S EARTH CLAY WATTONENSIS BEOS WYCHWOOD BEDS BRADFORD CLAY KEMBLE BEOS BUSWORTH CLAY UPPER FULLERS EARTH CLAY. (=MAINLY HAMPEN MARLY BEDS ? ARKELL,195I, p 14) HOOKNORTON Ls Figure 1. Inferred relationships of English Bathonian strata. Forest Marble and Cornbrash. All of these strata are Bathonian except the Upper Cornbrash, which is Callovian. In addition, the. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Harvard University. Museum of Comparative Zoology. Cambridge, Mass. : The Museum
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