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21<span style="color:#FFFFFF;font-size:5px;">brian was seriously considered as containing life. This frond-shaped fossil was found in England&#39;s Charnwood Forest first by a 15-year-old girl in 1956 (Tina Negus, who was not believed) and then the next year by a group of three schoolboys including 15-year-old Roger Mason. Due to the detailed geological mapping of the British Geological Survey, there was no doubt these fossils sat in Precambrian rocks. Palaeontologist Martin Glaessner finally, in 1959, made the connection between this and the earlier finds and with a combination of improved dating of existing specimens and an injection of vigour into the search many more instances were recognised. All specimens discovered until 1967 were in coarse-grained sandstone that prevented preservation of fine details, making interpretation difficult. S.B. Misra&#39;s discovery of fossiliferous ash-beds at the Mistaken Point assemblage in Newfoundland changed all this as the delicate detail pres
22 erved by the fine ash allowed the description of features that were previously undiscernible. It was also the first discovery of Ediacarans in deep water sediments. Poor communication, combined with the difficulty in correlating globally distinct formations, led to a plethora of different names for the biota. In 1960 the French name &quot;Ediacarien&quot; &ndash; after the Ediacara Hills &ndash; was added to the competing terms &quot;Sinian&quot; and &quot;Vendian&quot; for terminal-Precambrian rocks, and these names were also applied to the life-forms. &quot;Ediacaran&quot; and &quot;Ediacarian&quot; were subsequently applied to the epoch or period of geological time and its corresponding rocks. In March 2004, the International Union of Geological Sciences ended the inconsistency by formally naming the terminal period of the Neoproterozoic after the Australian locality. The term &quot;Ediacaran biota&quot; and similar (&quot;Ediacara&quot;/&quot;Ediacaran&quot;/&quot;Ediacarian&quo
23 t;/&quot;Vendian&quot;, &quot;fauna&quot;/&quot;biota&quot;) has, at various times, been used in a geographic, stratigraphic, taphonomic, or biological sen</span><br />
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