Information:

• Subfossil copal can be distinguished from genuine fossil amber because it becomes tacky when a drop of a solvent such as acetone or chloroform is placed on it.
• The process in blue amber is surprisingly similar to phosphor.
• Baltic amber or succinite (historically documented as Prussian amber) is found as irregular nodules in marine glauconitic sand, known as blue earth.
• African copal and the kauri gum of New Zealand are also procured in a semi-fossil condition.
• Other deposits are found in Sicily, Romania, Burma, China, Japan, Canada, Mexico and the United States.
• Amber is used in jewelry.

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Details: It was cerebration since the 1850s that resin that became amber was produced by the tree Pinites succinifer. Access lately, it has been proposed, on the evidence of Fourier-transform infrared frequency spectroscopy (FTIR) analysis of yellow-brown and resin from support trees, that conifers of the fellowship Sciadopityaceae were responsible for. The merely extant agent of this home is JP umbrella pine, Sciadopitys verticillata.