Megafauna Bone Fragment 002 Mammalia indet.
Owned by ILoveMyCatFreckles (@Freckles).
Notes
The specimen shows characteristic trabecular (spongy) bone texture visible on the weathered surface, typical of fossilized vertebrate remains. The dark mineralization suggests a fluvial or marine depositional environment. Possible swamplands or marsh environment.
Details
Identification & Classification
- Fossil Type
- Bone
- Fossil Category
- Vertebrate
- Taxonomic Group
- Chordate
- Phylogenetic Group
- Vertebrata
Geological Context
- Geological Era
- Cenozoic
- Geological Period
- Pleistocene
- Absolute Age (MYA)
- 9
Locality
- Locality Type
- Unknown
Anatomy & Physical Traits
- Anatomical Element
- Indeterminate
- Side
- N/A
- Articulation
- Isolated
- Completeness
- Fragmentary
Preservation & Preparation
- Preservation Quality
- Fair
- Matrix Type
- Sandstone
- Preparation Level
- Unprepped
- Restoration %
- 0
Provenance & Collection
- Acquisition Source
- Fossil store, Crystal World Exhibition Centre
- Date Acquired
- Jun 4, 2026
- Acquisition Price
- $5
- Documentation Provided
- None
- Legal Status
- Legal to Own
- Display Status
- In Storage
- Collection ID
- bca5ea2e-56e6-43a3-80c1-5e9c5f507500
- Quantity
- 1
- Added Details
- The specimen shows characteristic trabecular (spongy) bone texture visible on the weathered surface, typical of fossilized vertebrate remains. The dark mineralization suggests a fluvial or marine depositional environment. Possible swamplands or marsh environment.
Megafauna Bone Fragment 002
Mammalia indet.
Geological Context
Locality
Anatomy & Physical Traits
Preservation & Preparation
Provenance & Collection
Added Details
The specimen shows characteristic trabecular (spongy) bone texture visible on the weathered surface, typical of fossilized vertebrate remains. The dark mineralization suggests a fluvial or marine depositional environment. Possible swamplands or marsh environment.
Megafauna Bone Fragment 002
Mammalia indet.
Added Details
The specimen shows characteristic trabecular (spongy) bone texture visible on the weathered surface, typical of fossilized vertebrate remains. The dark mineralization suggests a fluvial or marine depositional environment. Possible swamplands or marsh environment.