Helicoplacoids are Early Cambrian echinoderms with tri-radiate ambulacra th
at are covered by helically-arranged columns of calcite plates. They are ab
undant only in, shales of the Middle Member of the Lower Cambrian Poleta Fo
rmation (Atdabanian) at Westgard Pass in the White-Inyo Mountains of Califo
rnia. To identify and understand the unique taphonomic conditions that led
to their preservation, 146 helicoplacoid specimens were examined along with
the rocks in which they are preserved. Considering their loosely articulat
ed skeletal construction, together with their common occurrence at the base
of cm-scale graded beds, helicoplacoids most Likely were preserved during
obrution events. A majority (69%) of helicoplacoid specimens are partially
disarticulated, probably indicating that most helicoplacoids underwent some
combination. of preburial and post-burial decay. Because most (73%) helico
placoid specimens are preserved on the same bedding-plane as at Least one o
ther individual, and many (39%) are preserved on bedding planes containing
at least 10 individuals, it appears that helicoplacoids were gregarious and
frequently were preserved in, mass mortality obrution deposits. Low levels
of bioturbation, possible microbial stabilization of the sediment, a shall
ow redox boundary, and a normally calm depositional environment capable of
preserving obrution deposits are all factors that aided in the preservation
of helicoplacoids. Additionally, the presence of helicoplacoids in several
facies of the Middle Member of the Poleta Formation indicates that they li
ved in a wider range of paleoenvironments than those represented by the sha
les, where they are found most commonly The exceptional preservation of hel
icoplacoids, therefore, is most likely narrowly restricted stratigraphicall
y and geographically because the proper balance of energy regimes, together
with the factors mentioned above, was achieved only rarely during the Earl
y Cambrian, not because helicoplacoids were restricted to Living in one pal
eoenvironment.