North America, Southwestern United States, Arizona, Late Triassic, ca. 225 million years ago. A massive and gorgeous slab of fossilized or petrified tree trunk sliced lengthwise like a plank, then highly polished on both sides to showcase the amazing colors. Millions of years ago this tree died, but the wood was preserved through fossilization and the organic material was replaced by stone- the vibrant structures made of quartz and agate. The natural knots and striations of the wood are present - the gaps infilled with quartzite banding. These colors are otherworldly and drastically different than what the original wood must have been, and this slab has hues that look like they were taken from Jupiter or Saturn: warm hues of red and maroon, purple, ochre yellow, with creamy white and lilac blue striations and swirls throughout. The flat face is sealed to protect the surface and this slab could be mounted as a tabletop! Size: 23.5" L x 1.75" W x 46.5" H (59.7 cm x 4.4 cm x 118.1 cm)
Fossilized trees from this time period come from the Chinle Formation of the southwestern USA, and the beautiful colors found in this formation - exemplified by the colors of this fossilized tree - give the Painted Desert of Arizona its name. During the Late Triassic, because of plate tectonics, this area was near the equator on the supercontinent Pangaea, with a humid, sub-tropical climate. It was a floodplain below mountains to its south and a sea to its west; as a result, massive trees washed down from the mountains and came to rest in sediments that preserved them and fossilized them. The petrification process involves the rapid burial of the tree or pieces under sediment which prevents the usual decay. Flooding and volcanic activity are usually responsible for creating the layers of sand, silt, and ash needed to create the right types and amount of sediment. Mineralized water can then permeate through the wood, coating cell walls and filling the intercellular cavities which then fossilizes into stone. The detailed preservation of the wood, including knots, rings, and bark, are possible because the organic wood molecules become coated and surrounded with smaller silica molecules. Nine different species of tree have been identified in the fossilized deposits in the region; this example may be Araucarioxylon parazonium, an extinct conifer tree (and the state fossil of Arizona), which is often found. Fascinatingly, the Ancestral Puebloan people who lived in the region approximately one thousand years ago used petrified wood for making tools and even building houses!
Provenance: private Berthoud, Colorado, USA collection
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#170383
Condition
Professionally prepared and polished. Stable fissures throughout from fossilization process, and minor infill with sealant to gaps on peripheries. One face is highly polished and covered in a clear fixative coating and the verso is covered in an opaque protective sealant to reinforce the piece.