Boris Choubert or Schuberth was a 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 Institut de géologie appliquée in Nancy, where he received his diploma of engineer-geologist. In 1933 he was employed by the Government of Gabon. In 1937 he defended his thesis on Étude géologique des terrains anciens du Gabon. In 1946 he was hired by the Office de recherche scientifique d'outre-mer and left for French Guiana. In 1949 he founded a multidisciplinary research organization which would become the Institut de l'Amérique tropicale française in 1954, then the Guyana office of ORSTOM in 1964. At the end of his stay he was inspecteur général de l'ORSTOM and the head of Bureau de recherches géologiques de laGuyane. 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:
In 1939 he discovered the first diamonds in the alluvial deposits of the Ikoy River basin, near Lambaréné. 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.
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.
Evoked several times between 1596 and 1908, the continental drift concept was chiefly developed and advocated by the German meteorologistAlfred Wegener between 1912 et 1929, on the basis of different criteria, morphological, stratigraphic, paleoclimatic and paleontological. 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. Boris Choubert was aware of studies by the South-African geologist Alexander du Toit, who had evidenced the great similarity of ancient South-American, West-African and South-African formations and was a supporter of Wegener's theory. Working on rocks from Gabon, Congo and Brazil, Boris Choubert confirmed the findings of du Toit and in turn became a fervent supporter of continental drift.
Reconstruction of the pre-Atlantic paleocontinent
Boris Choubert published in 1935 a reconstruction of the relative positions of America, Africa and Europe before the Triassic. This reconstitution was much more precise than the previous proposals by Wegener 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 timethe 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 Cenozoictectonics. 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, he made clear that they were formed by the compression of sediments that had been accumulated between three Precambrian cratons. 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
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.
