Anagrammeja & Tietoja | englanti sana TORTONIAN

Esimerkkejä TORTONIAN käyttämisestä lauseessa

• 2 million years (Ma) ago during the Tortonian age, while kinkajous split off from the other extant procyonids about 22.
• The base of the Tortonian Stage is at the last common appearance of calcareous nanoplankton Discoaster kugleri and planktonic foram Globigerinoides subquadratus.
• Anancus is an extinct genus of "tetralophodont gomphothere" native to Afro-Eurasia, that lived from the Tortonian stage of the late Miocene until its extinction during the Early Pleistocene, roughly from 8.
• As indicated by analysis of mt and nDNA sequences and calibrated with geological data, this genus' ancestors probably diverged from those of Mitu, their closest living relatives, in the Tortonian (early Late Miocene), some 8–7.
• Sinotherium ("Chinese Beast") is an extinct genus of single-horned elasmotheriine rhinocerotids that lived from the late Miocene (Tortonian - Messinian) to Early Pliocene.
• A species originally described to include Pliocene (Early Zanclean) specimen from Montpellier, France, later discoveries extended its range to late Miocene (latest Tortonian) Italy as well as Sahabi, Libya.
• Astroscopus countermani is an extinct species of stargazer described from a cranium found in Tortonian deposits of the Calvert Cliffs of what is now Maryland.
• The sandstones and siltstones were deposited in a shallow marine environment and preserve fossils dating back to the Middle to Late Miocene (Tortonian to Messinian, Clarendonian to Hemphillian in the NALMA classification) period.
• The coastal to marginally marine sandstone, siltstone, claystone, tuff and conglomerate formation dates to the latest Serravallian to Tortonian (Clarendonian to Hemphillian in the NALMA classification), from 12 to 8.
• At the base of the syn-rift sequence are 60 meters of Tortonian conglomerate with subrounded clasts derived from metamorphosed carbonate and quartzitic basement.
• Eucetotherium is a genus of cetotheriid mysticete from Miocene (Tortonian) marine deposits in the Russian Caucasus.
• Vampalus is a genus of cetotheriid mysticete from Miocene (Tortonian) marine deposits in the Russian Caucasus.
• In 1857 he published his most influential work Versuch einer neuen Klassifikation der Tertiär-Gebilde Europas (An Attempt at a New Classification of the Tertiary Formations of Europe) in which he classified the European Tertiary into 12 stages of which the Bartonian, Aquitanian, Tortonian, Astian, and Piacenzian still continue to be in use.

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