Annals of the South African Museum, Volume 69The Museum, 1976 - Natural history |
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Page 103
... lagoon show that the lagoon is a feature which existed at least by the Late Pleistocene . The lagoon is a north - westerly trending body 15 km long and a maximum of 4 km wide whose present channels are maintained by strong currents ...
... lagoon show that the lagoon is a feature which existed at least by the Late Pleistocene . The lagoon is a north - westerly trending body 15 km long and a maximum of 4 km wide whose present channels are maintained by strong currents ...
Page 108
... lagoon . Two explanations can be suggested . The first assumes that the peninsula separating the lagoon from the ocean owes its present extent to dune accumulation during the last glacial lowering of sea level . ( Evidence will be cited ...
... lagoon . Two explanations can be suggested . The first assumes that the peninsula separating the lagoon from the ocean owes its present extent to dune accumulation during the last glacial lowering of sea level . ( Evidence will be cited ...
Page 109
... lagoon where there are reputed to be reserves of 3 million metric tons . East of Kraalbaai they form a layer 1-3 m thick 5,5 m beneath the lagoon surface . Oysters generally settle on a hard substrate and it is possible that initial ...
... lagoon where there are reputed to be reserves of 3 million metric tons . East of Kraalbaai they form a layer 1-3 m thick 5,5 m beneath the lagoon surface . Oysters generally settle on a hard substrate and it is possible that initial ...
Contents
KENNEDY W J see KLINGER H C | 44 |
KENSLEY | 57 |
SIESSER W G see KLINGER H C | 72 |
Copyright | |
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abbreviations algae Anchisauridae Anchisaurus anteriorly Aristosaurus assemblage author's name Barghusen Barnard bed 3aS Berg River bicuspidata bone Broom Callianassa Cape Town capensis capitals cervical Churchhaven coast coronoid process dentary deposits dicynodonts distal Efraasia external adductor False Bay fauna fibres figures foramen fossa fossils Galton Gastropoda genus geol Gyposaurus Hendey holotype Huene Inguza insertion Kensley lagoon Langebaan Langebaanweg last interglacial Late Pleistocene lateral surface length limestone lower jaw Lufengosaurus mandibulae margin Massospondylus material medial molluscs muscle musculature open-coast ovig paratypes Pelletal Phosphorite Member pereiopod Phosphorite pleopod posterior posteriorly propodus prosauropod pterygoid quadrate Quarry Quartzose Sand Member ramus referred Saldanha scientific name sea level sediments separates setae shell shoreline skull South African Museum species specimens spines St Paul suggests SUID-AFRIKAANSE MUSEUM Synonymy Table Tankard temperature tendon Thecodontosaurus therapsids Typhlosaurus Typhlosaurus aurantiacus uropods Varswater Formation Velddrif Venjukovia ventral Verlorevlei vertebrae Х Х