Bitterfeld amber

The Baltic region is home to the largest known deposit of amber, called Baltic amber or succinite. It dates from 44 million years ago (during the Eocene epoch). It has been estimated that these forests created more than 100,000 tons of amber. Today, more than 90% of the world's amber comes from Kaliningrad Oblast of Russia. It is a major source of income for the region; the local Kaliningrad Amber Combine extracted 250 tonnes of it in 2014, 400 tonnes in 2015.

The term "Baltic amber" is generic, so amber from the Bitterfeld brown coal mines in Saxony (Eastern Germany) sometimes is included the same name. Bitterfeld amber was previously believed to be only 20–22 million years old (Miocene), but a comparison of the animal inclusions revealed that it is most probably genuine Baltic amber that has only been redeposited in a Miocene deposit. Other sources of Baltic amber have been listed as coming from Poland and Russia.

Because Baltic amber contains about 8% succinic acid, it is also termed succinite.

It was thought since the 1850s that the resin that became amber was produced by the tree Pinites succinifer, but research in the 1980s came to the conclusion that the resin originates from several species. More recently, it has been proposed, on the evidence of Fourier-transform infrared microspectroscopy (FTIR) analysis of amber and resin from living trees, that conifers of the family Sciadopityaceae were responsible. The only extant representative of this family is the Japanese umbrella pine, Sciadopitys verticillata.

The structure of Baltic amber (succinite) is complex. It is not a polymer, because it is not composed of a repeating pattern of «mers» of the same type. Rather it has a macromolecular structure arranged in a crosslinked network, in which the pores (free spaces) are filled by components of molecular structure (e.g. by mono- and sesquiterpenes). Thus the chemical structure of the amber may be described as a supramolecule. The structure makes the amber denser, harder and more resistant to external factors. It make also possible a good preservation of plant and animal inclusions.

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