Boris Choubert

Boris Choubert or Schuberth (1906 − December 3, 1983) was a Russian-French geologist. An adept of Wegener's theory, he was the first to precisely reconstruct the layout of the continental masses of Africa, America, Europe and Greenland prior to the fragmentation of Pangaea, thirty years before the article generally credited for this discovery.

Biography Of Russian origin, Boris Schuberth, better known as Choubert was born in Saint Petersburg in 1906. He left Russia for Finland in 1917, then for France in 1927. He studied geology at La Sorbonne for two years, then at the (now ) in Nancy, where he received his diploma of engineer-geologist.

In 1933 he was employed by the Government of Gabon (then a subdivision of French Equatorial Africa). In 1937 he defended his thesis on (Geologic study of ancient Gabon terrains).

In 1946 he was hired by the (presently IRD) and left for French Guiana. In 1949 he founded a multidisciplinary research organization which would become the (Institute of the French tropical America) in 1954, then the Guyana office of ORSTOM in 1964. At the end of his stay he was and the head of .

In 1960 he came back to continental France. In 1961 he joined the CNRS as a directeur de recherche, then the École des mines de Paris, where he stayed until his retirement in 1976. He then moved to Nice, where he was harboured by the laboratoire de géologie. He died in Nice on December 3, 1983.

Scientific studies Boris Choubert mainly dedicated himself to three geological fields, of which he significantly advanced the first two: prospecting and mining geology; geological mapping and structural geology; igneous petrology.

Mining geology In Gabon in 1934 Boris Choubert discovered the characteristic minerals, manganite and rhodochrosite, of a huge manganese deposit, which holds a quarter of all world reserves. In 1939 he discovered the first diamonds in the alluvial deposits of the Ikoy River basin, near Lambaréné (Estuaire Province, Gabon). He would show later that these deposits are of secondary origin, and that these diamonds come in fact from kimberlites, the same as those from South Africa. In Guyane he realized a detailed study of the gold mines of Saint-Élie and A Dieu Vat, and already drew attention to the problems generated by placer mining.

Geological mapping Boris Choubert achieved, alone or in collaboration, a great number of geological maps at various scales, from mine plans at 1/ to a global tectonic map at 1/, with a particular attention at the magmatic and metamorphic rocks of ancient formations. In 1935 he published a very important paper where he reconstructs Paleozoic and Precambrian ranges, and deduces the past existence and contours of the paleocontinent that predated the Atlantic Ocean opening. In French Guiana he tackles the geological map of the territory ( km) at 1/ scale, a map published in 1949 then, with more details, in 1960.

Boris Choubert and continental drift Continental drift in 1935 Evoked several times between 1596 and 1908, the continental drift concept was chiefly developed and advocated by the German meteorologist Alfred Wegener between 1912 et 1929, on the basis of different criteria, morphological (the nesting of continent shapes, like the Horn of Brazil and the Gulf of Guinea), stratigraphic (stratigraphic continuity between Africa and South America, and complementarity of Paleozoic cratons), paleoclimatic (similarity of Paleozoic striated pebbles of South Africa and South America) and paleontological (same fauna and flora during the Paleozoic era).

Wegener's studies obtained but limited success among the geological and geophysical community, for a number of reasons: in part because for every isolated argument one could appeal to coincidence or find some other explanation, but above all because the mechanisms that Wegener invoked as driving drift did not hold water. (Perhaps because himself was no geologist or geophysicist, too.) and du Toit, essentially because Choubert, instead of using coastlines, based his reconstitution on the 1000-m isobath, a much better representation of the limits of continental blocks.

That excellent fit was more convincing a proof of continental drift than previous attempts, which left a large gap between Africa and South America. For his reconstruction Boris Choubert dared for the first time the idea that the Iberian Peninsula suffered, after the Triassic, a rotation with respect to the rest of Europe. He also swept the Mid-Atlantic Ridge problem by explaining that it formed posteriorly to Atlantic Ocean opening. The Caribbean Sea does not fit as well as the rest but, as it is known today, it was seriously affected by Cenozoic tectonics.

Boris Choubert drew the theory farther than Wegener, who had only considered post-Triassic continental drift. By reconstructing the Paleozoic mountain ranges across the Atlantic (Caledonian range, Hercynian range et Appalachians), he made clear that they were formed by the compression of sediments that had been accumulated between three Precambrian cratons (Canadian Shield and Fennoscandian Shield at north, Gondwana at south). Withdrawing those ranges he concluded that the three cratons had made a single continent at the end of the Precambrian, which was later fragmented during the Paleozoic. Hence he realized that continental drift is a general process, which has affected the Earth all along its geological history.

The fit by Bullard, Everett and Smith Reconstruction by Bullard et al. of the America-Greenland-Europe-Africa supercontinent (1965). Thirty years later, Edward Bullard and co-authors published a paper in which a reconstruction similar to Choubert's was achieved with the help of a computer, through the numerical minimisation of distances between continental blocks. This paper rapidly acquired a great reputation among the scientific community, whereas Choubert's work had remained almost unnoticed (and it is even not cited in Bullard et al.'s paper).

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