Rovno amber

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Extinct wasp Disogmus rasnitsyni
Paleogeographic context of the Rivne Amber in Eocene Europe
Klesiv

Rivne amber, occasionally called Ukrainian amber,

Early Oligocene, and suggested to be contemporaneous to Baltic amber (Prussian Formation
). Major exploration and mining of the amber did not start until the 1990s.

Geology

The

brown coals and carbonized vegetation. Both formations are sandy to clayey in texture, with the Obukhov having more clayey glauconite-quartz plus sandy loess, while the Mezhigorje is mostly medium to fine grained sands of a greenish gray tone, and with occasional iron impregnation and layering.[6]

Prehistoric use

Small amounts of rough, partially worked, and fully shaped amber have been recovered from Paleolithic and Neolithic sites in the Dnieper area. At a site near Mezhyrich, four large mammoth bone huts attributed to Cro-Magnon Homo sapiens included over 300 pieces of amber attributed to Rivne origins. Many of the amber pieces are roughly fashioned into triangular and circular shapes. Dating of the site ranges between 13,300 and 10,500 B.C., when the regions of Baltic amber deposits in Kaliningrad and Lithuania were still covered with ice-sheets. A small female statuette of carved amber was found near Dobranichevka, while a 12 cm (4.72 in) disc with a central hole, and a hunting scene carved on one side was found in a Globular Amphora culture tomb in the Dubno district of Ukraine.[3]

Mining

The main use of amber until the 20th century was for burning, and rarely was it shaped for crafts.[3] As such, before the 1990s amber recovery wasn't overseen by the Ukrainian government, with small amounts found after rains and thaws and during well construction and while the Kyiv-Kovel rail line was being built.[2] Small scale collecting of the amber started to gain momentum in the 1950s when granite deposits in the Klesiv area were beginning to be developed. At that time the amber was picked from drainage piles and tailings dumps of the granite quarries,[2] often limited in access by the quarry operators.[3] Following an increase in the amber for jewelry production in Kyiv, Lithuania, and Poland, during the 1970s investigation and eventual start of the Pugach quarry in Klesiv culminated in 1991. In 1993 the Ukrainian government first started state overseen mining, under the auspices of Ukrburshtyn and at the same time making other major amber mining illegal. The current mining, centered on the Pugach quarry is operated by Burshtyn-Ukrainy.[3]

90% of Ukrainian amber is extracted illegally and the trade is controlled by armed organised crime groups. The amber is extracted by pumping water into the sandy sediments forcing the amber to the surface, creating pits. Areas where the amber is found are often covered in pine-beech forest, which is illegally deforested to extract the amber. Annual volumes of amber extracted illegally are suggested to be around 300 tons.[7] The richest placer deposits of Rivne amber are associated with the Obukhiv (late Eocene) and Mezhigorje (early Oligocene) Formations; deposits in the Kyiv region are known to come from the base of the Mezhigorje Fm. [8] The majority of Rivne amber is mined from the lower part of the aforementioned Formation, with the most notable locality being the Pugach Quarry in Klesiv. [9]

Composition

Amber from the Klesiv deposit and others in Ukraine have up to 0.1%

succinite range, same as Baltic amber. Trace amounts of Pb, Y, Zn, Zr, and some other elements are present in Rivne amber. Small to no detectable amounts of those elements are detected in Baltic amber.[10]

Paleoecology

There are a number of arthropod taxa, ranging from planthoppers, such as

Collembola families Entomobryidae and Sminthuridae, 59.7% and 24.5% respectively of the Collembola fauna. Baltic amber fly families have a distinct percentage of families associated with aquatic and semi-aquatic habitats, such as Chironomidae, while the Rivne fly fauna includes nearly double the amount of Sciaridae, Tipulidae, Mycetophilidae and other families associated with leaf litter habitats, called the "Sciara" zone. This is also seen in the coleopterans. There is an overall smaller number of aphids, a condition suggesting a possible subtropical climate for the Rivne forest, while the percentage of the hymenopteran family Scelionidae suggests a drier climate as well.[2]

Taxa

There are several hundred families of arthropods identified from Rovno amber, with major reviews being compiled by Perkovsky et al (2003, 2007, 2010).

Plantae

Bryophyta

Marchantiophyta

Crustacea

Isopoda

Arachnida

Acari

Araneae

Myriapoda

Chilopoda

Diplopoda

Entognatha

Collembola

Insects

Archaeognatha

Blattodea

Coleoptera

Diptera

Ephemeroptera

Hemiptera

Hymenoptera

Isoptera

Lepidoptera

Mantodea

Family indeterminate

Mecoptera

  • Bittacidae

Neuroptera

Orthoptera

Plecoptera

Psocoptera

Raphidioptera

Thysanoptera

Trichoptera

Strepsiptera

Family indeterminate

References

  1. .
  2. ^ a b c d e Perkovsky, E. E.; Rasnitsyn, A. P.; Vlaskin, A. P.; Taraschuk, M. V. (2007). "A comparative analysis of the Baltic and Rovno amber arthropod faunas: representative samples". African Invertebrates. 48 (1): 229–245.
  3. ^ .
  4. .
  5. ^ .
  6. ^ Perkovsky, E. E.; Zosimovich, V. Y.; Vlaskin, A. P. (2003). "A Rovno amber fauna: a preliminary report". Acta Zoologica Cracoviensia. 46(Supplemental): 423–430.
  7. ^ Besser, Linton (2020-01-21). "Blasting the green earth in a rapacious hunt for precious stones". ABC News. Retrieved 2020-02-05.
  8. ^ Perkovsky, Evgeny E. "A Rovno amber fauna: a preliminary report". ResearchGate. Retrieved 19 June 2021.
  9. PMID 27615867
    . Retrieved 19 June 2021.
  10. ^ .
  11. .
  12. ^ .
  13. ^ Mamontov, Y. S.; Hentschel, J.; Konstantinova, N. A.; Perkovsky, E. E.; Ignatov, M. S. (2017). "Hepatics from Rovno amber (Ukraine), 6. Frullania rovnoi, sp. nov". Journal of Bryology: 1–6.
  14. S2CID 86059856
    .
  15. .
  16. .

External links