North America, Southwestern United States, Arizona, Late Triassic, ca. 225 million years ago. A massive and gorgeous slab of fossilized or petrified Araucaria tree trunk, sliced crossways and highly polished on both planar faces to showcase the broad interior rings of the tree - not only beautiful but providing invaluable information to researchers about the prehistoric climate. The exterior bark is fossilized, replaced by rough stone, while the smooth interior features incredible, colorful quartz, agate, and translucent crystalline structures. The hypnotic colors are pink, lilac, orange, gray-blue, and creamy white with semi-translucent quartz crystals. The polished surface is pleasantly tactile, and just like natural wood today the graining and coloration of each petrified slab is unique with special character. Many Araucaria fossils have indicated the changing climate and eras of drought during the tree's life, which affect the ring sizes. Size: 18.25" Diameter x 0.75" W (46.4 cm x 1.9 cm)
Fossilized trees from this time period come from the Chinle Formation of the southwestern USA, and the beautiful colors found in the formation - exemplified this fossilized tree slab - give the Painted Desert of Arizona its name. Due to plate tectonics, this area was near the equator on the supercontinent Pangaea during the Late Triassic, which gave it 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 discovered in the fossilized deposits in the region; usually identified as Araucarioxylon arizonicum, an extinct conifer tree (and the state fossil of Arizona). Fascinatingly, the Ancestral Puebloan people who lived in the region approximately 1000 years ago used petrified wood for making tools and even building houses!
Provenance: private southwestern Pennsylvania, USA collection, acquired prior to 2000
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#159991
Condition
Professionally cut and polished. Natural cavity that perforates fully through from one face to the other. Other natural chips and cavities throughout. Great coloration and large size.