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| | alb21-3 |
 | | DORASHAMIAN, INDUAN, OLENEKIAN, ANISIAN, LADINIAN, CARNIAN, NORIAN AND RHAETIAN CARBONATES OF RUSSIA: |
 | | Abundance and high taxonomic diversity of the Albaillellaria from lower Dorashamian cherts of the Pantovyj and Skalistyj Creek basins and Amba Mount area (Sikhote-Alin) and from conteporaneous flyschoid strata of the Orel Mount area (South Primorye) seem to be caused by optimal temperature conditions. |
 | | It is possible that appearance of the polysegmental Nassellaria was related to the Anisian warmth and transgression, although the spherical Spumellaria, as was recently recognized in North Caucasus (Kapustina and Svinyach'ya Ravine, Mamryuk, Rufabgo) and South Primorye (Abrek Bay), was a dominant group among the microfossils in both Induan-Olenekian strata and during the Olenekian-Anisian transition. |
| www.biologie.uni-hamburg.de /b-online/kerp/Albart13.htm (827 words) |
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