Fossil Hill Member

The Fossil Hill Member was first recognized for its paleontological resources at the end of the 19th century. John Campbell Merriam and Eustace Furlong from the University of California Berkeley led the Saurian Expedition of 1905 to Fossil Hill in the Humboldt Mountains with the intention to search for Ichthyosaur fossils. The expedition was joined by the venerable heiress Annie Alexander who financed the expedition and provided most of the written documentation through journal entries and photographs. The expedition excavated the remains of 25 Triassic Ichthyosaurs, many of which were collected and shipped back to Berkeley. These skeletons, along with those collected from subsequent expeditions by UC Berkeley in the early 20th century, were the most complete Ichthyosaur specimens from North America at the time, and Merriam's study of these fossils provided some of the earliest knowledge on early ichthyosaur evolution. In the latter half of the 20th century, the section of Fossil Hill Member outcropping in the Augusta Mountains was identified for its ammonoid record to be used in biostratigraphic definition and correlation of Triassic rocks. Field observations of vertebrate fossils in the Augusta Mountains drew the attention of paleontologist Martin Sander who has led numerous teams to collect marine reptile fossils including specimens representing 7 new species. Paleontological fieldwork and research in the Augusta Mountains is ongoing. == Geology ==

Stratigraphy The Favret Formation and the Prida Formation, constitute two of the recognized geological formations within the Star Peak Group, of Northwestern Nevada. The Fossil Hill member links these two formations. Tectonic fragmentation of the region has broken apart most stratigraphic units of the Star Peak Group. Because of this outcrop discontinuity, the Fossil Hill Member is part of different formations in different parts of the outcrop area. In the Prida Formation, this member outcrops west of the Humboldt Range, and in the Favret Formation, it outcrops in the Augusta Mountains and southern extent of the Tobin Range. Although differing in precise age, the strata assigned to this member form a laterally uniform unit of offshore calcareous rocks. The various occurrences of the Fossil Hill member are also united by a distinct pelagic Anisian paleofauna preserved in the rocks. The Fossil Hill varies in thickness throughout its outcrops. In the China Mountain and Tobin Range sections, erosion and dolomitization from overlying units have rendered the Fossil Hill usually thin or locally absent. The unit within the Prida Formation varies from 60 to 120 meters thick while the section in the Augusta Mountains exceeds 250 meters. Silty shale is the prevailing lithology throughout the Fossil Hill Member outcropping in the Augusta Mountains with alternating facies of fissile shaley limestone and massive black limestones common throughout the entire section. Specific bioclastic beds dominated by Daonella fossils occur at multiple intervals within the shaley limestones. Compressed ammonoid fossils are also common. Three dimensionally preserved ammonoids occur less commonly but are still present in multiple areas. These three dimensional ammonoids are less prone to weathering and are useful for biostratigraphy. == Paleobiota ==

The Fossil Hill Member preserves a marine fossil assemblage from the continental margin off the west coast of Pangaea. • Germanonautilus furlongi • Grypoceras whitneyi • Paranautilus smithi ==See also==