Mikhail Fedonkin
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Mikhail Fedonkin
Academician Mikhail Aleksandrovich Fedonkin (russian: Михаи́л Алекса́ндрович Федо́нкин; born June 19, 1946) is a Russian paleontologist specializing in documentation of the earliest animals' body fossils, tracks, and trails. He has also described numerous Vendian-aged fossils including '' Hiemalora'', ''Cephalonega'', and '' Nimbia occlusa''. Early life Fedonkin was born in Orekhovo-Zuevo, Moscow Region, Russia. In 1969, Fedonkin presented a thesis titled "Biostratigraphy and paleontology of the Late Precambrian deposits of Kharaulakh Mountains, Northern Yakutia (Sakha)" to earn his MSc in Geology from Moscow State University. He went on to obtain a PhD in Stratigraphy\Paleontology (1978) and a Doctorate of Science in Paleobiology (1985) from the Geological Institute, USSR Academy of Sciences, Moscow for his dissertations on "Precambrian fauna and trace fossils from the Russian Platform north" and "Non-skeletal fauna of the Vendian and its pla ...
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Orekhovo-Zuyevo
Orekhovo-Zuyevo (russian: Оре́хово-Зу́ево, ) is an industrial city in Moscow Oblast, Russia, located east of Moscow in a forested area on the Klyazma River (a tributary of the Oka). Orekhovo (russian: Оре́хово), often pronounced only as ''Orekh'', is a Russian word which means "nut". The city was established in 1917 when three villages ( Orekhovo, Zuevo, and Nikolskoye) were merged, hence its name. Population: History The first known facts about what now is Orekhovo-Zuyevo date back to 1209. The place was mentioned in the Moscow Chronicles as the place called "Volochok" where the battle between Vladimir's prince Yury and Ryazan's prince Izyaslav took place. The name "Volochok" (or, as it was later called, "Zuyev Volochok") is derived from the Slavic word for "portage": a place where wooden ships were carried by land from one river to another. In this place in particular, the ships were usually moved by land between the Klyazma and Nerskaya Rivers. The vi ...
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Stratigraphy
Stratigraphy is a branch of geology concerned with the study of rock (geology), rock layers (Stratum, strata) and layering (stratification). It is primarily used in the study of sedimentary rock, sedimentary and layered volcanic rocks. Stratigraphy has three related subfields: lithostratigraphy (lithologic stratigraphy), biostratigraphy (biologic stratigraphy), and chronostratigraphy (stratigraphy by age). Historical development Catholic priest Nicholas Steno established the theoretical basis for stratigraphy when he introduced the law of superposition, the principle of original horizontality and the principle of lateral continuity in a 1669 work on the fossilization of organic remains in layers of sediment. The first practical large-scale application of stratigraphy was by William Smith (geologist), William Smith in the 1790s and early 19th century. Known as the "Father of English geology", Smith recognized the significance of Stratum, strata or rock layering and the importance ...
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