Annals of the South African Museum: Annale Van Die Suid-Afrikaanse Museum |
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Page 215
The greater diversity of this brachiopod assemblage suggests somewhat deeper water than the Weltevrede Formation assemblage , probably subtidal . The sedimentary facies of the Wagen Drift Formation are interpreted as having formed in a ...
The greater diversity of this brachiopod assemblage suggests somewhat deeper water than the Weltevrede Formation assemblage , probably subtidal . The sedimentary facies of the Wagen Drift Formation are interpreted as having formed in a ...
Page 220
The lowest sandstones were probably deposited by wash - over processes into the. Fig . 4. Top of an upward - coursening sequence in the Weltevrede Formation , Howison's Poort . Fig . 5. Thin upward - fining sequence near the.
The lowest sandstones were probably deposited by wash - over processes into the. Fig . 4. Top of an upward - coursening sequence in the Weltevrede Formation , Howison's Poort . Fig . 5. Thin upward - fining sequence near the.
Page 222
These probably formed in stagnant back - barrier lagoonal or marsh environments ( Fig . 6 ) . A similar detailed facies analysis is not available for the lower part of the Witteberg Group in the Western Cape but Theron ( 1970 ) stated ...
These probably formed in stagnant back - barrier lagoonal or marsh environments ( Fig . 6 ) . A similar detailed facies analysis is not available for the lower part of the Witteberg Group in the Western Cape but Theron ( 1970 ) stated ...
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Common terms and phrases
abbreviated according articulate brachiopods association author's name authors Barwis bedding benthic assemblages bivalves Blinkberg Bokkeveld Group Boucot capital collected communities consists containing cycles delta deposited described Devonian Devonian rocks differences DISTRIBUTARY diversity dominated Eastern environment environmental fauna feeders figures gastropod given homalonotid Howison's Poort illustrations inarticulate indicate infaunal interpreted intertidal italics known letters Lingula localities lower major marine marine invertebrates mark Member Middle mould Museum Natural History nearshore Note occur original placed plant fossils Plectonotus possible punctuation quartz arenites range recorded references represent reworking salinity sandstones scientific sediment SEDIMENTARY FACIES separates sequence shales shallow siltstone similar Smith South African species specimens Stratigraphic subtidal suggest Tables Tankard thick thin Touws River trace fossils trilobite Tropidoleptus sp unit upper valve Wagen Drift Formation Weltevrede Formation Western Cape Witpoort Formation Witteberg Group yielded Zoophycos