Background

Joachim Barrande was born on August 11, 1799, at Saugues, Haute Loire, France. The Barrande family were been documented in Saugues since the end of the 16th century. The father, Augustin Barrande, was a well-to-do land owner and textile-merchant. Besides two daughters, he had three sons who he sent to be educated at the College Stanislas in Paris. The mother, Charlotte-Louise, born Torrent, came from a family of royal officers, known in Saugues since the 16th century.

Education

Barrande was educated in Paris at the École Polytechnique and the École des Ponts et Chaussées where he focused on natural sciences. He went to lectures of Georges Cuvier, Jean B. Lamarck, Alexander Brongniart and other great naturalists of that time.

Career

Although Barrande had received the training of an engineer, his first appointment was that of tutor to the due de Bordeaux (afterwards known as the comte de Chambord), grandson of Charles X, and when the king abdicated in 1830, Barrande accompanied the royal exiles to England and Scotland, and afterwards to Prague. Settling in that city in 1831, he became occupied in engineering works, and his attention was then attracted to the fossils from the Lower Palaeozoic rocks of Bohemia. The publication in 1839 of Murchison's Silurian System incited Barrande to carry on systematic researches on the equivalent strata in Bohemia. For ten years (1840 - 1850) he made a detailed study of these rocks, engaging workmen specially to collect fossils, and in this way he obtained upwards of 3500 species of graptolites, brachiopoda, mollusca, Crustacea (particularly trilobites) and fishes.

In 1843 Barrande invited a Scottish geologist Sir Roderick Murchison to visit Bohemia. Murchison confirmed that all fossils are of Silurian age (Cambrian to Devonian in today's concept). After Murchinson´s pattern, Barrande decided to write a treatise about Silurian fossils of Central Bohemia. The first volume of the "Systême silurien du centre de la Bohême" was published in 1852. In his life Barrande published 22 volumes, which make almost 6000 pages and over 1000 lithographic plates in total. More than 3550 species of Paleozoic organisms (trilobites, crustaceans, cephalopods, bivalves, brachiopods and others) were described and illustrated. Owing to Barrande’s technical education all descriptions and illustrations of the fossils were very precise. That is one of the reasons why his work is unique even for today´s standards.

The term Silurian was employed by Barrande, after Murchison, in a more comprehensive sense than was justified by subsequent knowledge. Thus the Silurian rocks of Bohemia were divided into certain stages (A to H) - the two lowermost, A and В without fossils (Azoic), succeeded by the third stage, C, which included the primordial zone, since recognized as part of the Cambrian of Sedgwick. The fourth stage (Stage D), the true lower Silurian, was described by Barrande as including isolated patches of strata with organic remains like those of the Upper Silurian. These assemblages of fossils were designated "Colonies, " and regarded as evidence of the early introduction into the area of species from neighbouring districts, that became locally extinct, and reappeared in later stages. The interpretation of Barrande was questioned in 1854 by Edward Forbes, who pointed to the disturbances, overturns and crumplings in the older rocks as affording a more reasonable explanation of the occurrence of strata with newer fossils amid those containing older ones. Other geologists subsequently questioned the doctrine of "Colonies."

In 1883 Barrande went to Frohsdorf in Vienna, where he found his former ward of Henry of Chambord on his deathbed. A few hours after his arrival, however, Henry died. Barrande took care of Chambord’s testament. He unfortunately fell ill with pneumonia during the work and died on October 5th 1883 at the age of 84. Barrande dedicated his huge collection, library, field notes, and 10,000 Guldens to the National Museum.

Achievements

• 

  Barrande greatest achievement was in the meticulous work that he started in 1840 and continued until his death collecting, describing, and drawing the fossils of the central Bohemian basin - this area has been called the Barrandian ever since. The results formed the outstanding monograph Système silurien du centre de la Bohême (Prague, 1852-1902), which appeared in eight parts forming thirty quarto volumes. Because this work is so comprehensive, its drawings so accurate, and its descriptions so fine, it is still used as a reference book by paleontologists.
  
  Another Barrande’s achievement was accomplished through his meticulous efforts in distinguishing metamorphosis in several species of trilobites, and he even identified embryonic states. He described Sao hirsuta, of which twenty naturally occurring forms had previously been identified as eighteen species in ten genera.
  
  During his career, Barrande gathered an enormous collection of scientific manuscripts, and his library was a valuable contribution to the Prague Museum after his death.
  
  In recognition of his great input into the study of fossils and geology, Barrande was elected a Foreign Honorary Member of the American Academy of Arts and Sciences in 1875. In 1884 the Barrande Rocks in Prague was named in honor of the scientist and massive plaque with Barrande's name was added at the rocks. Also, in recognition of his important researches the Geological Society of London in 1855 awarded to him the Wollaston medal. On 24 February 1928 all district of Prague, Barrandov, was named in his honor.

Works

More photos

• book

  • Nouveaux Trilobites Supplément à la Notice Préliminaire sur le Systême Silurien Et les Trilobites de Bohême
  • Crustacés divers et poissons des dépôts siluriens de la Bohème 1872
  • Céphalopodes siluriens de la Bohême 1867
  • Défense des colonies 1861
  • Notice Préliminaire sur le Systême Silurien Et les Trilobites de Bohême
  • Réapparition Du Genre Arethusina Barr 1868
  • Brachiopodes: Études Locales 1879
  • Acéphalés: Études Locales Et Comparatives
  • Systême Silurien Du Centre De La Bohême: Trilobites 1852
  • On the primordial fauna and the taconic system 1860
  • Defense des colonies 1861
  • Distribution des ceIphalopodes dans les contreIes siluriennes : extrait du SysteI‚me silurien du centre de la BoheI 1870
  • Letter to M. Joachim Barrande, on the Taconic rocks of Vermont and Canada 1862 [Leather Bound] 1862
  • Bryozoaires, Hydrozoaires Et Partie Des Anthozoaires
  • Etudes Sur La Graptolites de Boheme. Suite de L'Ouvrage: Systeme Silurien Du Centre de La Boheme 1894

Views

Barrande was dedicated to the Cuvierian conception of the constancy of species, which he acquired during his early training in Paris and never abandoned. Similarly, he persevered in his conception of “colonies,” assemblages of more recent fauna found intercalated among older strata. They supposedly resulted from migrations, although his opponents argued that these anomalies were due to tectonic disturbances of the strata.

In an international controversy over the status of the Taconic system, proposed by the American geologist Ebenezer Emmons, Barrande actively joined Jules Marcou in supporting Emmons’ claim to be the true discoverer of the primordial fauna.

Membership

In 1870, Barrande was elected a foreign member of the Royal Swedish Academy of Sciences. He was also a member of the American Academy of Arts and Sciences.

Personality

Quotes from others about the person

• In his obituary, Gustav Laube presented a truthful characteristic of Barrande:
  
  ”Conservative in his entire being, as required by his relations to the legitimist French party, and also in science; he remained a pupil and devotee of Cuvier till his death and, therefore, a natural opposer of the evolutionary teaching and the theory of evolution”.

Connections

Father:

Augustin Barrande

associate:

Charles Lyell

In 1851 Charles Lyell pointed out in the Quarterly Journal of the Geological Society of London, on the basis of some of Barrande’s preliminary studies:

"... it is not the least interesting circumstance attending these discoveries, to learn that all these fossils were obtained from a superficial area, not more extensive than one-sixtieth part of the Adriatic; and they certainly show that the Silurian Fauna was not only as rich, but as much influenced by geographical conditions, or as far from being uniform throughout the globe, as that of any subsequent era."

teacher:

Georges Cuvier

teacher:

Jean-Baptiste Lamarck

teacher:

Alexandre Brongniart

colleague:

Gustav Laube

References

• Dictionary of scientific biography
  1970