Walcott-Rust quarry
Encyclopedia
The Walcott-Rust quarry is an excellent example of an obrution (rapid burial or "smothered") Lagerstätten. Unique preservation of trilobite
Trilobite
Trilobites are a well-known fossil group of extinct marine arthropods that form the class Trilobita. The first appearance of trilobites in the fossil record defines the base of the Atdabanian stage of the Early Cambrian period , and they flourished throughout the lower Paleozoic era before...

 appendages resulted from early consolidation (cementation) of the surrounding rock, followed by spar filling of the interior cavity within the appendages. The presence of so many well preserved trilobites in one location alone qualifies the beds as an exceptional trilobite site, but the beds are further distinguished as the source of the first trilobites for which appendages were definitively described.

Historical Overview

By 1860 William Palmer Rust (1826–1897) and his father Hiram were actively excavating fossils from quarries on the family farm originally opened for building stone. 1870 saw Charles Doolittle Walcott
Charles Doolittle Walcott
Charles Doolittle Walcott was an American invertebrate paleontologist. He became known for his discovery in 1909 of well-preserved fossils in the Burgess Shale of British Columbia, Canada.-Early life:...

 working a new trilobite locality in Upper Ordovician limestones on a creek near the Rust farm, where Walcott had recently moved. Walcott and Rust began to quarry the site with Walcott marrying Rust's daughter Laura Ann on January 9, 1872.

In 1873 Walcott and Rust sold their collections to Louis Agassiz
Louis Agassiz
Jean Louis Rodolphe Agassiz was a Swiss paleontologist, glaciologist, geologist and a prominent innovator in the study of the Earth's natural history. He grew up in Switzerland and became a professor of natural history at University of Neuchâtel...

 at the Museum of Comparative Zoology
Museum of Comparative Zoology
The Museum of Comparative Zoology, full name "The Louis Agassiz Museum of Comparative Zoology", often abbreviated simply to "MCZ", is a zoology museum located on the grounds of Harvard University in Cambridge, Massachusetts. It is one of three museums which collectively comprise the Harvard Museum...

, Harvard University
Harvard University
Harvard University is a private Ivy League university located in Cambridge, Massachusetts, United States, established in 1636 by the Massachusetts legislature. Harvard is the oldest institution of higher learning in the United States and the first corporation chartered in the country...

. At this meeting between Walcott and Agassiz, Walcott mentioned that he had seen evidence of appendages and soft tissue, which Agassiz recommended he pursue. Discovery of soft body preservation at the Walcott-Rust quarry pre-dates Walcott's discovery of the more famous Burgess Shale
Burgess Shale
The Burgess Shale Formation, located in the Canadian Rockies of British Columbia, is one of the world's most celebrated fossil fields, and the best of its kind. It is famous for the exceptional preservation of the soft parts of its fossils...

 lagerstätte
Lagerstätte
A Lagerstätte is a sedimentary deposit that exhibits extraordinary fossil richness or completeness.Palaeontologists distinguish two kinds....

 by 40 years.

Walcott left the area and active working of the quarry in 1876 (his wife Lura Ann died of tuberculosis on January 23, 1876) although he returned for brief periods throughout his career. In 1876/7 Walcott published several papers on trilobite appendages, the first documentation of these features. In 1879 Walcott took up his appointment with the USGS and sold the fossils he and Rust had collected between 1873 and 1879 to Alexander Agassiz
Alexander Emanuel Agassiz
Alexander Emmanuel Rodolphe Agassiz , son of Louis Agassiz and stepson of Elizabeth Cabot Agassiz, was an American scientist and engineer.-Biography:...

 at the Museum of Comparative Zoology.

Rust and his friends continued to extract and sell specimens from the quarry until Rust's death in 1897. It is estimated that over the years 8600 square feet (799 m²) were excavated. The old fossil quarry site was reopened in 1990 by Thomas E. Whiteley (also involved in the rediscovery of Beecher's Trilobite Bed) and extensively re-examined.

Sedimentology & environment of deposition

The Walcott-Rust quarry is excavated into beds of the lower part of the Rust Formation and consist of a distinctive one meter package of generally tabular, fine grained lime mudstone with a few bioturbated beds, part of a series of shallowing upward cycles that commence with dark shales that grade into fine-grained limestones. Many of these thin layers yield evidence for rapid deposition as distal carbonate turbidite
Turbidite
Turbidite geological formations have their origins in turbidity current deposits, which are deposits from a form of underwater avalanche that are responsible for distributing vast amounts of clastic sediment into the deep ocean.-The ideal turbidite sequence:...

s or storm layers.

Fossils occur at the bases, tops and within a number of the storm units. Fossils represented in the Walcott-Rust quarry beds reflect a shelf community that developed during times of rather low net sedimentation and minimal bioturbation
Bioturbation
In oceanography, limnology, pedology, geology , and archaeology, bioturbation is the displacement and mixing of sediment particles and solutes by fauna or flora . The mediators of bioturbation are typically annelid worms , bivalves In oceanography, limnology, pedology, geology (especially...

 of the bottom. These communities were episodically smothered by sediment layers re-suspended by storms in shallower water.

Fossil fauna

Exquisitely-preserved fossils, including at least 18 species of trilobites, have been documented. The four most common trilobites Ceraurus, Flexicalymene, Isotelus gigas, and Meadowtownella are found (complete or partially complete) throughout the deposit often associated with echinoderms. 22 of the 50 recognized beds were found to yield at least one complete articulated trilobite and/or echinoderm (primarily crinoids).
More specifically, the fauna includes brachiopods, bryozoans, 11 described species of crinoids, one paracrinoid, one rhombiferan, two "carpoids", two asteroids, one ophiuroid, and one edrioasteroid.

Taphonomy & exceptional preservation

One layer (the "Ceraurus layer") yields specimens that are uniquely preserved with calcified appendages, forming the basis of Walcott's earliest and still classic papers which first documented biramous limbs of trilobites. Trilobites appendages are preserved in specimens of Ceraurus, Flexicalymene, and Meadowtownella uniquely preserved as sparry calcite infilings. Exceptionally fine detail of the appendages was preserved and has undergone very little compaction (a contrast to other sites). This type of preservation is only apparent when a specimen is sliced and the cut surface is polished or a thin section made. Also, only those specimens which are partially enrolled show a significant amount of this type of preservation. For these reasons it is unlikely that this preservation would be obvious to anyone collecting trilobites.

A sequence of events was necessary for this appendage preservation to take place. The trilobites that show the best soft tissue preservation were buried when partially enrolled inside the layer. The burial was in lime sediment and that may have buffered the micro-environment against any acidic products of bacterial metabolism. The surrounding rock must have consolidated very rapidly to allow the three-dimensional preservation. Organic matter made the closed micro-environment anaerobic; decay proceeded by sulfate reducing bacteria producing bicarbonate and sulfide byproducts (Allison, 1990). A slightly alkaline environment, saturated with carbonate, with bicarbonate build-up may have led to highly localized calcium carbonate precipitation. Pyrite formation, more common in such circumstances, may have been inhibited because of the small amount of iron in the carbonate sediment.

See also

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