Tyndall Stone is used extensively throughout North America as a building and framing stone, known for its distinctive mottled pattern and high diversity and abundance of well-preserved fossils, including solitary and colonial corals, brachiopods, cephalopods, gastropods, stromatoporoids, and receptaculitids. Stratigraphically, Tyndall Stone is found in the Selkirk Member of the Red River Formation (Late Ordovician). Tyndall Stone is mined exclusively from Gillis Quarries in the town of Garson, Manitoba. The quarry is also the location of this study. At first glance the homogeneous lithology suggests a static, unchanging paleoenvironment. Upon detailed examination of a 5 m study section, however, fossil data reveal obvious environmental fluctuations that are not detectable frorn lithology alone. An overall upward shallowing sequence is suggested by an increase in stromatoporoid and receptaculitid abundance over time. An increase in sedimentation rate accompanied the upward shallowing sequence, as evidenced by the overall decrease in encrusting relationships and percentage of highly abraded horn corals. A sudden deepening event is recorded between 1.5 and 2.0 m above the base of the study section (interval 4). Within this interval, a sudden decrease in stromatoporoids and receptaculitids is observed, along with a sharp increase in encrusting relationships and percentage of highly abraded horn corals. The mottled pattern of the Tyndall Stone is attributed to the feeding activity of shrimp-like organisms burrowing their way through the firm to hard sediment in search of food. This trace fossil is recognized as the ichnogenus Thalassinoides. Cluster and correlation analyses reveal close ecological relationships between various fossil groups. Most prominent among these relationships include 1) the gastropods and cephalopods, and 2) the stromatoporoids and the encrusting coral, Protrochiscolithus. Statistical analyses also reveal similarities and dissimilarities between intervals in the study section. Most notable is the extreme dissimilarity between interval 4 and every other interval. The fossil assemblage found within the Tyndall Stone suggests a shallow marine environment, with warm to temperate water temperatures, normal salinity and an abundance of nutrients in the water column. A northerly flowing paleocurrent is inferred from the orientations of cephalopods and cardinal septa directions of horn corals. It can easily be shown that the Tyndall Stone fossils display an abundance of paleoenvironmental and paleoecological information, despite a homogeneous lithology which suggests otherwise. Interpretation of paleoenvironment, then, cannot be based solely on lithology, as fossil data can be much more sensitive to environmental change