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The occurrence of Scrobicularia plana in the Red Crag, Lower Pleistocene

✍ Scribed by R.G. Dixon

Book ID
114035785
Publisher
The Geological Society (London)
Year
1976
Tongue
English
Weight
230 KB
Volume
87
Category
Article
ISSN
0016-7878

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Pleistocene decalcification of Late Plio
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Uppermost sands of the Red Crag at Walton‐on‐the‐Naze (Essex) and elsewhere in East Anglia have been decalcified to iron‐stained quartz sands. In contrast, lower sands are only minimally altered and contain aragonitic and calcitic shells. Aragonitic shells are slightly dissolved (chalkified), but ca