| The oldest ambers with included animal fossils date back to the Cretaceous, with the best known occurrences being those from Lebanon, France, Burma and New Jersey (USA). This small collection consists of examples from Burma and New Jersey.
The New Jersey examples come from the Raritan Formation (Turonian, ca 90 Ma), excavated (from lignite occurring 6 to 10 feet below the surface) by Jon Stanislawczyk, at a locality near Sayreville, New Jersey, USA. The amber was produced by a forest of Cupressaceae in a warm temperate or sub-tropical environment (Grimaldi et al. 2000). The burmite examples are of Cenomanian-Albian (ca 100 Ma) age and come from Main Khun, Tanai Township, Kachin State, Burma (Myanmar). Burmese amber was formed by a conifer, perhaps Metasequoia, in a tropical palaeoenvironment (Grimaldi 2003). There are some fine illustrations of the flow of low viscosity resin in these specimens. See the multi-flow pendulous "stalactite" from New Jersey (upon which a wasp landed only to be engulfed by the next flow) and the longitudinally stretched wasp from Burma. One of the Burmese dipterans also shows both wings swept forwards against the head. |
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