New types of microbial fossils and new occurrences of fossils previously reported only from the Beck Spring Dolomite of the Pahrump Group are now recognized from each of the three formations of the Pahrump Group (Crystal Spring Formation, Beck Spring Dolomite, and Kingston Peak Formation) approximately 1.3 X 10° years old. Comprising perhaps eight or nine distinctive forms, these fossils are characteristically preserved as faint ghostlike structures whose low‐contrast outlines are clearly revealed only when illuminated by a xenon lamp and recorded on high‐contrast film. They represent a distinctive, previously overlooked or neglected type of preservation that has significantly extended the known distribution of microbial fossils in the Pahrump. They include the oldest occurrence known to us of filaments designatable asGirvanellaand apparently the first from rocks of pre‐Phanerozoic age. Similar fossils were also found, using the same techniques, in the Chuar Group of the Grand Canyon and in the Uluntui Suite of middle Riphean age in eastern Siberia. Although time correlation of pre‐Phanerozoic rocks based on similar microbial assemblages would be premature, similarity between such assemblages in all formations of the Pahrump Group and with that of the Uluntui Suite is consistent with the inferred unity and middle Riphean age of the Pahrump Group. In addition to theGirvanellawe find two smaller types of filaments, two kinds of simple spheroids, and three composite forms (two spheroids and one stalked cluster) that attain diameters up to 80 μm and are probably eucaryotic.