A Late Ordovician seafloor, preserved through repeated burial.
The Mt. Orab butter shale is a thin fossil-bearing
interval within the Sunset Member. Its articulated fossils record several events,
not one frozen moment for the entire bed.
Repeated clay-silt couplets within the butter-shale interval
The approximately 0.46 m measurement describes the studied Mt. Orab interval,
not the thickness of the entire Arnheim Formation or a measurement of every Flat Run exposure.
Rapid burial, repeated
The interval contains at least seven recognizable clay-silt couplets interpreted
as stacked storm-generated event beds. More than one depositional event contributed
to the assemblage.
Silt: locally transported remains
The basal silt portions include transported skeletal debris and disarticulated
trilobite remains. These are interpreted as parautochthonous: moved locally rather
than necessarily buried exactly where they lived.
Clay: more articulated remains
The clay-rich portions preserve articulated enrolled, prone and partially enrolled
trilobites, alongside carcasses and molts. They are interpreted as largely autochthonous:
organisms rapidly buried at or near where they lived. Enrolment alone does not establish
how an individual died.
Fauna / Field record
Arnheim fauna checklist
Documented fauna, comparison records and what I’ve personally found.
Personally found is a separate claim.
A checked box means I’ve personally found it. An unchecked box means I haven’t recorded a personal find here, not absence from the formation. These are read-only field-record markers, not visitor checkboxes or stock indicators.
This is a working selection, not an exhaustive census. Formation-wide records are not automatically Mt. Orab or Flat Run records. Occurrence evidence is stated separately on each entry; my personal identification is not being attributed to a paper that only identifies the genus.
Flexicalymene retrorsa
Personally found
Trilobite · Calymenidae · Mt. Orab bed documented
I’ve personally found Flexicalymene retrorsa, which is also documented from the Mt. Orab bed. I record the identification and provenance of each specimen separately.
Trilobite · Asaphidae · Formation-wide record; personal Mt. Orab find
I’ve personally found I. maximus at my home quarry. The UGA reference includes the Arnheim in its occurrence range. The Mt. Orab taphonomy paper records Isotelus at genus level; I’m not using that paper to establish the species of my find.
Echinoderm · crinoid · My Arnheim find — my identification
I’ve found stems I identify as Cincinnaticrinus. I’m recording them at genus level, without assigning a species. The Mt. Orab paper supports crinoid occurrence generally, not my identification of these stems.
Echinoderm · crinoid · My Arnheim find — my identification
I identify the calyx I found as Pycnocrinus dyeri. An Arnheim specimen in the Geneseo collection is catalogued as Glyptocrinus dyeri, an alternative combination encountered in collection records. The UGA reference treats Pycnocrinus and Glyptocrinus as distinct genera; the names are not generally interchangeable. I count this as one find, not two.
PBDB collection 192315 records this genus, citing Key and colleagues (2010). That collection record does not mean I’ve personally found or identified it.
Trilobite · Cheiruridae · Formation-wide Arnheim record
The UGA occurrence compilation includes the Arnheim, citing Ludvigsen (1977) and Babcock (1996). This does not establish a Flat Run or butter-shale occurrence.
Echinoderm · edrioasteroid · Formation-wide Arnheim record
An attached echinoderm included in the Arnheim occurrence compilation. This is not a crinoid, and my crinoid finds do not establish that I’ve found this animal.
Mollusc · nautiloid cephalopod · Formation-wide Arnheim record, genus only
The compilation includes an Arnheim record at genus level. Its named species have different listed ranges; they are not assigned here. This is not a confirmed Mt. Orab butter-shale record.
The UGA compilation lists an Arnheim occurrence from Dalvé (1948), but explicitly questions the validity of this species. I include it as a qualified historical record, not as an identification of my crinoid material.
Trilobite · Asaphidae · Arnheim occurrence unverified in checked sources
I include it for comparison and leave it unchecked. The UGA reference lists the species but supplies no occurrence range for it. That gap is not proof of absence; a specific Arnheim or Mt. Orab record is still needed.
Trilobite · Lichidae · Arnheim occurrence I can confirm — fragments
I can confirm Allolichas fragments from the Arnheim, but I’m not marking them as a personal find. I use the species spelling given by Dry Dredgers; that overview does not establish the formation or identify these fragments to species.
Taxa documented in the Mt. Orab study, at the identification level
supported by my working reference.
Flexicalymene retrorsa
Trilobite · Calymenidae
The characteristic named trilobite of the Mt. Orab Lagerstätte. Enrolled, prone and partially enrolled individuals occur alongside carcasses, molts and disarticulated remains.
Isotelus sp.
Trilobite · Asaphidae
Documented at genus level. Assigning I. maximus or I. gigas requires diagnostic specimen morphology; locality alone does not establish the species.
Crinoidea indet.
Crinoids
Crinoids are documented in the Mt. Orab fauna. Isolated stems and columnals do not by themselves establish a species identification.
Modiolopsis
Bivalve
Documented at genus level in the Mt. Orab faunal assemblage.
Bryozoa
Bryozoans
Documented colonial animals in the Mt. Orab community; species names require additional evidence.
Chondrites
Trace fossil
A burrow trace recorded in the event beds, not the name of an identified body fossil.
Lingulids are also reported. Brachiopods
are outside this guide’s main focus, not absent from the assemblage.
Formation-wide and regional evidence
Not confirmed from the Mt. Orab bed
This section describes the limits of the cited literature; personal finds
and occurrences I can confirm are recorded separately in the checklist above.
An Arnheim or Cincinnatian record alone is not a butter-shale record.
Pycnocrinus dyeri
Documented from the Arnheim Formation in the research draft, but not securely established from the Mt. Orab butter-shale horizon.
Platyceratid gastropods
An Arnheim crinoid association is reported in the research draft. That does not establish a Flat Run butter-shale occurrence or a species identification.
Orthoconic nautiloids
Known in the wider Cincinnatian / Richmondian record. Locality-specific evidence remains weak. Use “orthoconic nautiloid cephalopod, indeterminate genus” for undiagnosed material rather than automatically calling it Orthoceras.
Other possibilities under study
Cyclonema, Cyclora, Trepospira, Treptoceras, Glyptocrinus, Xenocrinus, Cupulocrinus, Ectenocrinus and rare trilobites such as Ceraurus remain comparative possibilities, not a confirmed Flat Run fauna list.
Cephalopod presence must not be inferred solely from healed injuries or bite marks;
a fauna list needs body-fossil evidence.
Name only what the evidence supports
Use the narrowest identification supported by the specimen. Formation-wide records do not establish a Mt. Orab or Flat Run occurrence. A locality study does not authenticate an individual lot.
Use Isotelus sp. when species is uncertain, Crinoidea indet. for unidentified
crinoid material, and a species name only when diagnostic characters support it.
F. retrorsa is documented in the bed; that is not an instruction to rename every
existing Flexicalymene specimen.
Source and scope
Hunda, B. R., Hughes, N. C., & Flessa, K. W. (2006). Trilobite taphonomy and temporal resolution in the Mt. Orab Shale Bed (Upper Ordovician, Ohio, U.S.A.). PALAIOS, 21, 26–45.
The bed summary follows the supplied Mt. Orab working fauna research draft.
The expanded checklist also cites formation-level reference pages and collection records,
with occurrences I can confirm and my personal finds identified separately.
These additional records are not all established by the Mt. Orab paper.
Formation-wide evidence alone does not establish a home-quarry occurrence.