Annals of the South African Museum, Volume 69The Museum, 1976 - Natural history |
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Page 37
... molluscs are present ( Fig . 2 ) . The importance of this is that it implies that temperatures were such that the normal spawning ... molluscs . These molluscs obviously lived in environments THERMALLY ANOMALOUS LATE PLEISTOCENE MOLLUSCS 37.
... molluscs are present ( Fig . 2 ) . The importance of this is that it implies that temperatures were such that the normal spawning ... molluscs . These molluscs obviously lived in environments THERMALLY ANOMALOUS LATE PLEISTOCENE MOLLUSCS 37.
Page 38
assemblages of molluscs . These molluscs obviously lived in environments reflected in the sediments , and have suffered little post - death transportation . 4. The sediments and their mollusc fossils indicate water depths in general ...
assemblages of molluscs . These molluscs obviously lived in environments reflected in the sediments , and have suffered little post - death transportation . 4. The sediments and their mollusc fossils indicate water depths in general ...
Page 41
... molluscs . Because of the low migratory ability of molluscs in the post - larval stage , their geographic distribution depends primarily on the dispersion of larvae . Distribution of the planktonic larvae depends upon ocean currents ...
... molluscs . Because of the low migratory ability of molluscs in the post - larval stage , their geographic distribution depends primarily on the dispersion of larvae . Distribution of the planktonic larvae depends upon ocean currents ...
Contents
KENNEDY W J see KLINGER H C | 44 |
KENSLEY | 57 |
SIESSER W G see KLINGER H C | 72 |
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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