Earth Record
Mineralogy and formation
Chrysanthemum coral is fossilized rugose or tabulate coral from the Paleozoic era (roughly 250-500 million years ago) where the original calcium carbonate skeleton has been replaced by silica, calcite, or other minerals during diagenesis. The characteristic flower-like patterns are cross-sections of individual coral polyp chambers (corallites) arranged in radiating or concentric patterns that resemble chrysanthemum blossoms.
The replacement process preserves the original biological architecture while converting the skeleton to more stable minerals. Found in limestone formations worldwide, with notable material from China, Indonesia, and the American Midwest.
Variable (Trigonal if silicified; Trigonal/Rhombohedral if calcite-replaced) structure
Chemical FormulaVariable (SiO2 if silicified; CaCO3/CaMg(CO3)2 if carbonate-replaced)Crystal SystemVariable (Trigonal if silicified; Trigonal/Rhombohedral if calcite-replaced)Mohs Hardness6.5Specific Gravity2.55-2.65 (silicified); 2.65-2.85 (calcite/dolomite replaced)LusterWaxy to vitreous (silicified); vitreous to dull (calcite-replaced)ColorWhite-BrownIMA StatusrockIMA NumberNo IMA number (ornamental stone, not approved species) [IMA List](https://ima-mineralogy.org/Minlist.htm) IndonesiaUSA (Florida)
Telling it apart
Dealers routinely blur chrysanthemum coral with chrysanthemum stone, fossil coral in general, and modern dyed coral cabochons. The first distinction is biological versus mineral aggregate origin. Chrysanthemum coral is actual fossil coral, so the flower pattern comes from corallite anatomy preserved by silicification or carbonate replacement. Chrysanthemum stone is usually a black limestone or clay matrix with radiating celestine, calcite, andalusite, or feldspar crystals that only mimic floral anatomy.
Dyed coral has porous color concentration and lacks the repeated chamber structure. What separates them fastest is magnification. Under a loupe, true fossil coral shows repeated polyp walls, septa, and cellular partitions arranged in a consistent colonial pattern. A crystal pseudoflower shows blades or sprays, not skeletal chambers. A drop of dilute acid on an inconspicuous spot can also help: carbonate-rich coral will fizz, silicified coral will not, while dyed material often leaks color at drill holes.
Fossil coral identification depends on preserved biological structure, not color or polish, and calling a non-fossil material coral is fundamentally dishonest.
Spotting the real thing
Chrysanthemum coral: fossilized coral should show natural coral structure (septa, tabulae) under magnification. The flower-like pattern is biological, not carved. Silicified specimens (Mohs 7) are harder than calcite-replaced specimens (Mohs 3, which effervesce in acid).
If the "coral" shows no internal biological structure under magnification, it may be carved stone rather than actual fossil.
Cross-referenceMindat ↗