Ambre birman - Feuille - 7 mm - Ambre

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€ 1
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Manuel Quiring
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Estimation  € 200 - € 250
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Ambre birman naturel feuille, 7 mm, du Cenomanien supéieur du Crétacé (environ 100 millions d’années), poli, poids 0,19 g, origine Myanmar.

Résumé assisté par IA

Description fournie par le vendeur

Burmese Amber - Leaf 7 mm

Cretaceous Period : Cenomanian Stage (100.5 - 93.9 million years ago )
Origin : Hukawng Valley - Myanmar

Amber size : 12.4x7.4x3.3 mm
Inclusion size : 7 mm
Weight : 0.19 g

Burmese amber, also known as burmite comes mainly from the Hukawng Valley in northern Myanmar. It dates back to nearly 100 million years, the early Cenomanian stage of the late Cretaceous period. During that period angiosperm plants started to replace the gymnosperms. This is one of the most important periods in the evolution of life on earth and the formation of modern flora and fauna


Pictures are taken with special magnification equipment to show a better view of the inclusions. Please check carefully the size of the amber and inclusion before bidding !

Burmese Amber - Leaf 7 mm

Cretaceous Period : Cenomanian Stage (100.5 - 93.9 million years ago )
Origin : Hukawng Valley - Myanmar

Amber size : 12.4x7.4x3.3 mm
Inclusion size : 7 mm
Weight : 0.19 g

Burmese amber, also known as burmite comes mainly from the Hukawng Valley in northern Myanmar. It dates back to nearly 100 million years, the early Cenomanian stage of the late Cretaceous period. During that period angiosperm plants started to replace the gymnosperms. This is one of the most important periods in the evolution of life on earth and the formation of modern flora and fauna


Pictures are taken with special magnification equipment to show a better view of the inclusions. Please check carefully the size of the amber and inclusion before bidding !

Détails

Spécimen
Burmese Amber - Leaf - 7 mm
Pays d’origine
Myanmar
Période géologique
Crétacé, Supérieur (100,5 - 66 millions d’années)
Condition
Naturel
Traitement
Poli
Poids
0,19 g
Vendu par
LuxembourgVérifié
84
Objets vendus
100%
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