Journal of the Transactions of the Victoria Institute, Or Philosophical Society of Great Britain, Том 76Victoria Institute., 1944 |
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Стр. 61
... fossil . ( a ) Fossils of the Lamellibranchs Fordilla and Modioloides occur in Lower Cambrian deposits ; some authorities , however , deem these to be the shells of Branchiopod Crustaceans . ( b ) Fossils of Insects and Amphibia occur ...
... fossil . ( a ) Fossils of the Lamellibranchs Fordilla and Modioloides occur in Lower Cambrian deposits ; some authorities , however , deem these to be the shells of Branchiopod Crustaceans . ( b ) Fossils of Insects and Amphibia occur ...
Стр. 62
... fossils been found , despite the fact that these rocks occur in all parts of the world , are of great thickness , often underlie the Cambrian rocks , and are in many cases undisturbed or modified and well - suited to hold fossils . By ...
... fossils been found , despite the fact that these rocks occur in all parts of the world , are of great thickness , often underlie the Cambrian rocks , and are in many cases undisturbed or modified and well - suited to hold fossils . By ...
Стр. 70
... Fossils are abundant in Triassic and very abundant in Jurassic rocks . The vertebrate fossils are mostly of reptiles , of which new orders appear successively including bipedal and quadrupedal Dino- saurs and Pterodactyls . The known ...
... Fossils are abundant in Triassic and very abundant in Jurassic rocks . The vertebrate fossils are mostly of reptiles , of which new orders appear successively including bipedal and quadrupedal Dino- saurs and Pterodactyls . The known ...
Содержание
REPORT OF COUNCIL FOR THE YEAR 1943 | 18 |
XV | 32 |
CURRENT THEORIES OF SPECIAL CREATION BY D DEWAR ESQ | 53 |
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