Dinosaur bone
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Dinosaur Bone: Living Architecture Mineralized in Deep Time
Polished dinosaur bone is compelling because its pattern began as anatomy. Dense cortex, branching trabeculae, vascular canals, marrow spaces, fractures, and later mineral cements become a mosaic of cream, rust, ochre, black, gray, and blue-green when a fragment is cut across its internal structure. Yet the name requires precision: a polished piece may be genuine fossil bone without preserving enough evidence to identify a dinosaur, and many examples are more defensibly described as silicified vertebrate bone. This guide approaches the material first as a fossil, then as a mineralized object, a lapidary stone, and a geological record whose context matters.
Quick Facts
Dinosaur bone is a composite fossil material. Its behavior depends on the surviving bone phosphate, the minerals introduced during burial, the degree of replacement, later fractures, preparation, and any resin or backing added during lapidary work.
Identity, Terminology, and What the Name Can Prove
Dinosaur bone is not a mineral species. A polished piece may contain altered bone phosphate together with chalcedony, quartz, calcite, iron oxides, manganese oxides, clay, barite, opal, or other secondary minerals. Hardness, density, color, polish, and stability are therefore properties of a mixed fossil material.
In lapidary use, gembone usually means fossil bone sufficiently mineralized to cut and polish while retaining a visible network of internal structure. The word does not identify the animal, geological formation, or age. A fragment can be authentic fossil bone and still be impossible to assign confidently to a dinosaur from appearance alone.
The strongest dinosaur identification comes from context: a documented dinosaur-bearing formation, a known locality, diagnostic anatomy, association with identified remains, preparation records, or a chain of custody extending back to the field. Once a fragment has been detached, sliced, stabilized, and separated from its label, much of that evidence may be lost.
Fossil bone
A broad and accurate term for mineralized vertebrate skeletal tissue. It does not specify dinosaur, mammal, reptile, fish, age, or locality.
Silicified bone
Bone in which silica fills pores, replaces tissue, or both. Chalcedony-rich examples can approach quartz in hardness and polish.
Agatized bone
A traditional lapidary description for bone containing chalcedony or agate-like silica. It should not imply visible agate banding unless such banding is present.
Permineralized bone
Bone whose natural pore system has been filled by minerals carried in groundwater. Some original hard tissue may remain.
Opalized bone
Fossil bone in which opal is a major pore-filling or replacement phase. It may be more sensitive to heat and dehydration than chalcedony-rich material.
Commercial dinosaur bone
A common label that should be supported by formation and locality information. Without context, “mineralized vertebrate bone” may be more defensible.
Bone Architecture Behind the Mosaic
The visible pattern reflects a hierarchical biological material. Large structural regions, microscopic vascular systems, growth tissue, and marrow spaces can all influence a polished surface.
Cortical bone
The dense outer wall. In polished fragments it may appear as a compact rim with fine pores, subtle layering, or closely spaced vascular canals.
Trabecular bone
The branching internal lattice often called cancellous or spongy bone. Cross-sections create the familiar open network of walls and mineral-filled spaces.
Vascular canals
Channels that once carried blood vessels. Mineral infill can make them appear as dots, rods, short lines, or elongated tubes depending on orientation.
Marrow spaces
Larger internal cavities may fill with chalcedony, calcite, iron-rich cement, sediment, or several generations of minerals.
Osteons and growth tissue
True microscopic bone features may survive, but they are generally far smaller than the bold polygons visible in ordinary cabochons.
Fractures and compression
Breakage before or after burial can offset the original network, admit new minerals, and create secondary veins that cross the anatomy.
| Cut orientation | Likely appearance | What it may reveal |
|---|---|---|
| Across trabeculae | Polygonal or honeycomb-like openings separated by dark or pale walls. | Thickness, spacing, mineral infill, and later fracture cement. |
| Along trabeculae | Elongated ribbons, branching channels, or flame-like lines. | Direction of internal support structures and deformation. |
| Across vascular canals | Small circular or elliptical points within denser tissue. | Canal abundance and orientation in cortical bone. |
| Along vascular canals | Fine rods or parallel streaks. | Longitudinal structure and possible bone-shaft orientation. |
| Through cortex and interior | A dense border surrounding a more open center. | Original outside-to-inside relationship within the bone. |
How Bone Becomes Stone
Fossilization is not one instantaneous transformation. Burial, decay, groundwater movement, mineral precipitation, replacement, compaction, fracture, uplift, and weathering may alter the specimen at different times.
Burial isolates the remains
Sediment covers the bone and reduces exposure to scavenging, surface weather, and physical destruction.
Organic tissue decays
Collagen and other soft components break down while the mineralized skeletal framework and pore architecture may persist.
Groundwater enters the pore system
Water carrying dissolved silica, carbonate, iron, manganese, and other ions moves through canals, marrow spaces, fractures, and surrounding sediment.
Minerals precipitate inside open spaces
Permineralization strengthens the fossil by filling pores without necessarily removing all original bone mineral.
Replacement may alter the tissue itself
Original mineral phases can dissolve and be replaced molecule by molecule or region by region while the larger structure remains recognizable.
Later events add new structure
Compaction, faulting, oxidation, carbonate veining, silica deposition, and weathering may produce additional colors and boundaries.
Permineralization
Minerals fill existing pores and canals. The bone framework may remain partly original even when the fossil becomes dense and stone-like.
Replacement
Original material dissolves while another mineral occupies its place. Fine anatomical detail can survive if replacement proceeds gradually.
Recrystallization
Existing mineral grains reorganize into larger or more stable crystals, sometimes preserving shape while reducing microscopic detail.
The polished object is therefore not merely a bone filled once with one mineral. It can be a sequence of biological structure, burial chemistry, repeated fluid movement, fracture, and repair recorded in the same fragment.
Minerals, Color, and Pattern Vocabulary
Color does not come from the animal’s original bone. It is produced mainly by minerals introduced or altered during fossilization and later weathering.
| Mineral or process | Typical visual effect | Practical significance |
|---|---|---|
| Chalcedony and microcrystalline quartz | White, cream, gray, translucent blue-gray, muted green, or nearly colorless pore fillings. | Raises hardness and commonly allows a high, durable polish. |
| Calcite | White, cream, honey, or clear infill with cleavage flashes. | Softer and acid-sensitive; may undercut during polishing. |
| Iron oxides and hydroxides | Red, rust, orange, brown, ochre, or yellow staining and cement. | Creates much of the familiar western gembone palette. |
| Manganese oxides | Black, charcoal, or dark dendritic boundaries. | Can increase contrast but may mark fractures or later weathering. |
| Opal | Milky translucency, pale gray, cream, or locally play-of-color. | May require more conservative heat and humidity care than quartz-rich material. |
| Sediment and clay | Earthy, matte, tan, gray, or greenish material retained in pores. | May remain porous, soft, or difficult to polish evenly. |
| Later fractures | Straight, branching, or offset veins crossing the biological network. | May add design interest or create structural weakness. |
| Resin stabilization | Darker saturation, reduced porosity, filled pits, and improved polish. | Useful preparation that should be disclosed and considered during cleaning or repair. |
Trabecular mosaic
Irregular windows separated by mineralized struts; the classic gembone appearance.
Cortical field
Dense, comparatively uniform material with fine canal points and subtle growth structure.
Channel pattern
Elongated dark or translucent lines produced by vascular canals viewed along their length.
Mineral windows
Clear or translucent pore fillings that contrast with opaque bone walls.
Brecciated bone
Broken anatomical fragments recemented by silica, carbonate, iron-rich material, or sediment.
Dendritic overprint
Branching manganese or iron patterns deposited along fractures and surfaces after fossilization.
Physical and Optical Properties
| Property | Typical expression | Interpretive significance |
|---|---|---|
| Material type | Composite fossil containing preserved or altered bone mineral plus secondary minerals. | No single formula or fixed property set describes every specimen. |
| Hardness | Approximately Mohs 3 in calcite-rich areas; commonly 6.5–7 in well-silicified areas. | Mixed mineralization can produce uneven cutting and polishing behavior. |
| Specific gravity | Variable with porosity and mineral content. | Density alone cannot establish fossil identity or taxon. |
| Luster | Waxy to vitreous after polishing; dull or earthy on porous rough surfaces. | A glossy finish may reflect silica or resin rather than one uniform natural phase. |
| Transparency | Usually opaque, with translucent mineral-filled pores and thin edges. | Backlighting can reveal fracture networks, pore fillings, dye, and backing. |
| Cleavage | No single aggregate cleavage; individual calcite fillings may cleave. | Breakage usually follows fractures, pores, mineral boundaries, or weakened trabeculae. |
| Fracture | Uneven to conchoidal in silica-rich areas; granular or stepped in mixed material. | Fresh edges can expose multiple mineral generations. |
| Refractive behavior | Aggregate response governed by chalcedony, calcite, opal, resin, and opaque tissue. | A single refractive-index reading rarely characterizes the entire object. |
| Ultraviolet response | Variable; calcite, resin, glue, and trace activators may fluoresce differently. | Useful for mapping construction and repairs, but not diagnostic by itself. |
| Porosity | Low in dense silicified bone; moderate to high in incompletely filled or weathered material. | Controls staining, stabilization, cleaning response, and polish quality. |
Under Magnification
A hand lens or microscope helps separate anatomical structure from fracture, sediment, treatment, and imitation. Begin with pattern continuity rather than searching for one isolated feature.
Trabecular walls
Natural walls vary in thickness, curve organically, branch, reconnect, and continue beneath the polished surface.
Mineral-filled pores
Chalcedony may appear waxy, finely crystalline, zoned, or translucent; calcite may show cleavage flashes or coarser crystals.
Vascular channels
Small circles, ellipses, or elongated rods occur within denser tissue and may retain consistent directional relationships.
Fracture generations
Some cracks cut across both tissue and earlier pore fillings, proving that they formed after the primary mineralization.
Resin and adhesive
Glossy menisci, trapped bubbles, filled pits, differences in fluorescence, or a distinct backing line may reveal preparation.
Surface printing or composite structure
A pattern confined to the face, repeated motifs, mold marks, bubbles, or abrupt lamination may indicate imitation or assembly.
Non-destructive examination sequence
Examine the entire object before concentrating on microscopic detail. Fossil identity, mineralization, preparation, and condition must be considered together.
- Follow the pattern to the edgeNatural architecture should continue into sidewalls unless the object is backed or heavily reconstructed.
- Compare face and reverseThe reverse may preserve rough cortex, matrix, saw marks, resin, or a join concealed from the front.
- Rotate under raking lightSeparate glassy polish, pearly calcite, matte sediment, pits, coatings, and undercut areas.
- Backlight thin sectorsLook for translucent pore fillings, fracture penetration, color concentration, and backing.
- Inspect drill holesBeads can reveal internal continuity, dye accumulation, resin, and mixed mineral hardness.
- Escalate significant piecesMicroscopy, Raman spectroscopy, X-ray diffraction, and elemental analysis can resolve uncertain mineral phases.
Identification and Common Look-Alikes
| Material | Why it resembles fossil bone | Useful distinctions |
|---|---|---|
| Petrified wood | Silicified cellular plant tissue may form repeating pores, bands, and earth colors. | Look for grain direction, rays, growth rings, vessels, tracheids, and longitudinal plant structure rather than trabecular architecture. |
| Fossil coral | Corallites can create repeated honeycomb or flower-like patterns. | Coral commonly shows radial septa, repeated corallite centers, or colony-wide geometry absent from bone. |
| Septarian or brecciated stone | Cracks filled with calcite or chalcedony create polygonal networks. | Fracture polygons lack continuous anatomical walls, vascular canals, and cortex-to-interior relationships. |
| Spiderweb jasper | Dark lines divide colored silica into irregular fields. | Jasper webbing follows fractures or pigment boundaries rather than three-dimensional skeletal tissue. |
| Agate | Translucent chalcedony, mineral-filled cavities, and multiple colors may overlap visually. | Agate usually shows rhythmic banding, fortification patterns, or cavity-centered growth instead of a biological support network. |
| Resin or printed imitation | Surface graphics can reproduce a convincing mosaic. | Search for mold seams, bubbles, repeated motifs, low weight, soft plastic response, and pattern confined to the surface. |
| Other fossil vertebrate bone | The anatomy and mineralization can be genuinely bone-like because it is real bone. | Taxonomic separation requires formation, age, locality, anatomy, or associated records rather than cabochon pattern. |
Cutting, Orientation, and Finished Forms
The cutter does not create the fossil pattern but determines which anatomical plane becomes visible. Orientation can turn the same fragment into a compact cortical field, a broad trabecular mosaic, or a set of elongated vascular channels.
Cross-cut cabochon
Often produces the clearest polygonal mosaic by intersecting trabeculae and vascular canals across their length.
Longitudinal cabochon
Emphasizes channels, branching struts, and directional flow rather than compact cells.
Cortical slice
Shows fine vascular points, layered density, and subtle biological texture rather than large open windows.
Full-section slab
Can preserve the relationship among cortex, interior, fractures, matrix, and several mineral zones.
Backed cabochon
A thin fossil layer may be bonded to a stronger support. The construction can be practical but should be disclosed.
Stabilized rough
Resin impregnation can strengthen porous material before slabbing and reduce grain loss during polishing.
Map the anatomy before cutting
Wet the rough, inspect every face, and identify cortex, porous interior, fractures, sediment, and previous repairs.
Select the viewing plane
Choose cross-cut or longitudinal orientation according to the structure intended for the finished object.
Stabilize only where needed
Porous or fractured material may benefit from resin, but treatment should remain proportionate and documented.
Pre-polish patiently
Mixed hardness can cause pits and undercutting. A complete abrasive progression produces a more even surface.
Protect open edges
Thin trabeculae and fracture margins benefit from gentle bevels, broad settings, and avoidance of unsupported points.
Control workshop dust
Saw, grind, sand, and drill wet with effective extraction. Fossil material may contain silica, phosphate, carbonate, trace metals, resin, and locality-dependent mineral contaminants.
Assessing a Specimen or Polished Piece
There is no universal grading system for dinosaur bone. Scientific context, anatomical readability, mineral color, cutting quality, stability, treatment, and provenance represent different forms of significance.
Anatomical readability
Clear trabecular walls, vascular channels, cortex, or internal transitions make the fossil structure easier to interpret.
Mineral contrast
Distinct yet naturally integrated colors can clarify the pore network without overwhelming the anatomy.
Pattern continuity
Structure should continue across the face and into visible edges rather than ending as a superficial image.
Cut orientation
A well-selected plane reveals the intended anatomy and avoids reducing the pattern to disconnected fragments.
Condition
Open fractures, friable matrix, loose trabeculae, pits, backing failure, and unstable repairs affect handling and interpretation.
Context and treatment
Formation, locality, legal collection history, resin, backing, dye, reconstruction, and repair should be recorded separately.
| Factor | Favorable characteristics | Points to examine |
|---|---|---|
| Structure | Coherent anatomy with branching walls, channels, and depth. | Repeating printed pattern, isolated fragments, or loss of structure through excessive filling. |
| Color | Natural mineral variation integrated with pores and fractures. | Color pooling, surface-only saturation, coating, or altered adhesive. |
| Polish | Even reflective surface without drag, deep scratches, or severe undercutting. | Pits, orange peel, exposed resin, rounded detail, or polish residue. |
| Stability | Secure trabeculae, closed fractures, sound matrix, and supported edges. | Loose fragments, flexing backing, powdering, open seams, or hidden breaks. |
| Preparation | Necessary stabilization or backing carried out cleanly and disclosed. | Undocumented reconstruction, thick coating, concealed joins, or excessive resin. |
| Provenance | Formation, locality, land status, collector, and preparation records retained. | Taxonomic or locality claims based only on appearance. |
Locality, Provenance, and Responsible Acquisition
For vertebrate fossils, place is part of the object. Geological formation, bed, sedimentary environment, association, and legal collection history can be more informative than polished color.
Morrison Formation
Late Jurassic strata across the western United States are a major source of dinosaur fossils and much material traditionally described as western gembone.
Other Mesozoic formations
Dinosaur-bearing rocks occur worldwide from the Late Triassic through the end of the Cretaceous, with different preservation styles and mineral assemblages.
Commercial cutting centers
A place where material was slabbed, stabilized, or polished is not necessarily its geological source.
Private land
Legality depends on land ownership, permission, jurisdiction, export rules, and the circumstances of collection.
Public land
Rules differ by country and agency. In the United States, vertebrate fossils on federal public lands are not casual-collection material.
Museum and research material
Scientific specimens may carry restrictions, repository obligations, specimen numbers, and permanent public ownership.
| Record | Why it matters |
|---|---|
| Geological formation and member | Constrains age, environment, and the animals known from the deposit. |
| Precise locality | Connects the specimen with regional geology and collecting history. |
| Land status and permission | Establishes whether collection and transfer were authorized. |
| Collector and date | Supports chain of custody and may connect the fragment with field notes. |
| Preparation history | Records cutting, stabilization, backing, repair, coating, and reconstruction. |
| Earlier labels and photographs | Preserve information that may disappear when ownership or mounting changes. |
Care, Storage, and Handling
Care follows the weakest part of the object: soft mineral infill, open fracture, porous sediment, resin, adhesive, backing, thin trabecula, or fragile matrix.
Routine cleaning
Use lukewarm water, mild neutral soap, and a soft cloth or brush. Keep washing brief and dry the object promptly.
Protect the polish
Remove loose grit before wiping and store away from sapphire, topaz, diamond, and other harder materials.
Avoid unnecessary acids
Acid can attack calcite-rich fillings, matrix, labels, and some repairs even when the surrounding silica remains intact.
Avoid strong heat
High temperature and rapid change may affect opal, resin, adhesive, backing, and existing fractures.
Use manual cleaning when uncertain
Steam and ultrasonic cleaning are unsuitable when treatment, construction, porosity, or fracture condition is unknown.
Support display pieces
Use broad padded stands that carry the matrix rather than narrow points pressing against exposed fossil structure.
| Risk | Possible effect | Preferred approach |
|---|---|---|
| Hard impact | Chipped edge, broken trabecula, opened fracture, or detached backing. | Use protective settings and padded storage. |
| Abrasive grit | Fine scratches and a dulled polish. | Rinse or lift away dust before wiping. |
| Prolonged soaking | Water penetration into matrix, resin boundaries, repairs, or porous zones. | Keep cleaning brief and dry at room temperature. |
| Ultrasonic vibration | Expanded fractures, loose pore fillings, or adhesive failure. | Use manual cleaning. |
| Steam or repair heat | Thermal stress, opal damage, resin alteration, or backing failure. | Avoid steam and remove the object before hot metalwork. |
| Dry cutting or grinding | Airborne silica, phosphate, carbonate, resin, and trace-mineral dust. | Use wet methods, local extraction, and appropriate workshop controls. |
Deep-Time Perspective
Modern reflective interpretations of fossil bone often draw on preserved structure, adaptation, evidence, continuity, and the difference between an object and its context. These are contemporary readings rather than one universal ancient tradition.
Structure
A network of many small supports can carry more than one solid mass, offering a useful image for resilient systems.
Transformation without erasure
Minerals alter the substance of the bone while preserving much of its form, suggesting change that retains meaningful continuity.
Evidence
Claims become stronger when anatomy, formation, locality, and records agree, providing a model for separating observation from assumption.
Scale
Deep time places immediate concerns within a larger horizon without making present action less important.
Context
A fragment becomes more informative when connected to its surrounding bed, landscape, and history.
Repair and record
Fractures can be stabilized, but honest documentation preserves the distinction between original structure and later intervention.
Observe the structure
- Name the present situation without interpretation.
- List the supports already carrying it.
- Identify one missing connection rather than one missing force.
- Choose a small action that strengthens that connection.
Separate evidence from story
- Write what is directly known.
- Write what has been inferred.
- Mark what evidence would confirm or revise the inference.
- Act only at the confidence level the evidence supports.
Preserve the context
- Record what happened before the present moment.
- Identify the conditions shaping the current result.
- Retain one useful record before making a change.
- Review what the change reveals rather than only what it removes.
Continue Into the Specialist Dinosaur Bone Guides
These articles examine the material through fossil anatomy, mineral preservation, geology, provenance, history, cultural interpretation, and grounded symbolic practice.
Frequently Asked Questions
What is dinosaur bone in the lapidary trade?
It is mineralized fossil vertebrate bone cut to reveal internal structure. Material called gembone is often silica-rich and polishable, but mineral composition and taxonomic certainty vary.
Is every piece sold as dinosaur bone definitely from a dinosaur?
No. Fossil bone from mammals, crocodilians, marine reptiles, turtles, fish, and other vertebrates can look similar after polishing. Dinosaur attribution should be supported by formation, age, locality, anatomy, or provenance.
What does gembone mean?
Gembone is a lapidary term for fossil bone that can be cut and polished attractively, usually because mineralization has strengthened its pore network. It is not a formal taxonomic or mineralogical name.
Are the visible polygons fossilized bone cells?
Usually not. The bold mosaic commonly represents trabecular spaces, vascular cavities, and mineral-filled pores. Individual osteocytes and their lacunae are much smaller.
What is the difference between permineralization and replacement?
Permineralization fills the natural pore system with minerals. Replacement removes original material while another mineral occupies its place. Both can occur in the same fossil.
Is agatized bone made entirely of agate?
Not necessarily. The term commonly indicates substantial chalcedony or microcrystalline quartz, but original bone mineral, calcite, sediment, iron oxides, and other phases may remain.
Why is some fossil bone red or orange?
Iron oxides and hydroxides commonly create rust, red, brown, orange, ochre, and yellow colors during burial or later weathering.
What produces black areas?
Manganese oxides, iron-rich phases, organic matter, dark sediment, or later fracture coatings can produce black and charcoal tones.
Why are some pore fillings blue-gray or greenish?
Fine silica, inclusions, trace minerals, scattering, and the optical effect of translucent material over a dark background can create muted blue-green or gray color.
How hard is fossil bone?
It depends on mineralization. Calcite-rich areas may be near Mohs 3, while well-silicified material may approach Mohs 7.
Can dinosaur bone be worn in rings?
Stable, well-silicified material can be used in protected ring settings. Open fractures, soft infill, thin trabeculae, opal, backing, and resin require more conservative wear.
Why is some material stabilized?
Resin can strengthen porous or fractured bone, reduce grain loss, and improve polish. Stabilization is a preparation method rather than evidence that the fossil is false.
What is a backed cabochon?
It is a thin fossil layer bonded to a stronger support. Backing can improve durability but should be visible in documentation and considered during cleaning or repair.
Can fossil bone be dyed?
Yes. Dye may deepen color or increase contrast, particularly in porous material. Concentration in cracks, pits, drill holes, and surface-reaching pores can provide clues.
How can fossil bone be separated from petrified wood?
Petrified wood commonly shows grain, rays, growth rings, vessels, or aligned plant cells. Bone shows cortical tissue, trabecular structure, vascular canals, and marrow spaces.
How can it be separated from fossil coral?
Fossil coral often preserves repeated corallite centers and radial septa. Bone architecture is less regularly radial and may show a cortex-to-interior relationship.
How can it be separated from septarian stone?
Septarian patterns are fracture networks filled by minerals. They do not preserve branching trabeculae or vascular canals.
Does pattern continuing through the edge prove dinosaur origin?
It supports a natural three-dimensional structure but does not identify the taxon. Genuine non-dinosaur vertebrate bone also continues through the object.
Where does classic North American gembone come from?
Much historically recognized material is associated with Late Jurassic rocks of the western United States, especially the Morrison Formation, although fossil bone occurs in many other formations and countries.
Can dinosaur bone be casually collected on United States federal public land?
Vertebrate fossils on federal public lands are generally protected and require authorized scientific collection rather than casual collecting. Rules differ on private, state, tribal, and other national lands.
Why is provenance important?
Formation, locality, land status, collector, date, and preparation history support age, taxonomic interpretation, legality, and scientific value.
Can fossil bone be radioactive?
Some fossil bone can incorporate uranium during burial, particularly in uranium-bearing sedimentary settings. Most material cannot be judged from appearance alone, so locality records and screening are useful for unusual specimens or substantial workshop processing.
How should polished fossil bone be cleaned?
Use lukewarm water, mild neutral soap, and a soft cloth or brush. Keep contact brief and dry promptly.
Can it be cleaned ultrasonically?
Manual cleaning is safer because vibration may affect fractures, loose infill, resin, backing, or adhesive.
Can it be steam cleaned?
Steam is best avoided because rapid heating may stress fractures and affect opal, resin, adhesive, or backing.
Is acid safe on silicified bone?
Even when silica-rich areas resist mild acid, associated calcite, matrix, labels, resin, and repairs may not. Acid cleaning is unnecessary for finished material.
What precautions matter during cutting?
Use wet methods, effective local extraction, and appropriate personal protection. Mixed fossil material may generate silica, phosphate, carbonate, resin, and trace-mineral dust.
What should appear on a specimen record?
Record the most defensible material name, visible anatomy, mineralization, formation and age, locality, legal collection basis, preparation, treatment, dimensions, condition, and provenance.