Carl Wiman

From Wikipedia, the free encyclopedia

Born
Carl Johan Josef Ernst Wiman

(1867-03-10)10 March 1867
Stockholm, Sweden
Died15 June 1944(1944-06-15) (aged 77)
Uppsala, Sweden
Carl Wiman
Black-and-white photograph of Carl Wiman
Carl Wiman in 1937, aged 70
Born
Carl Johan Josef Ernst Wiman

(1867-03-10)10 March 1867
Stockholm, Sweden
Died15 June 1944(1944-06-15) (aged 77)
Uppsala, Sweden
Resting placeUppsala gamla kyrkogård[1]
Alma materUppsala University
Scientific career
Fields
Institutions
ThesisÜber die Graptoliten (1895)
Doctoral advisorArvid Högbom

Carl Johan Josef Ernst Wiman (March 10, 1867 – June 15, 1944) was a Swedish palaeontologist, the first professor of palaeontology and historical geology at Uppsala University, and the father of Swedish vertebrate palaeontology.[2]

Wiman was instrumental in the construction of the Palaeontological Museum of Uppsala University (now part of the Museum of Evolution), which contains the largest collection of Chinese fossil vertebrate material outside China.[2]

He is responsible for naming the genera Helopus (renamed Euhelopus because Helopus was already in use) and Tanius,[3] and the species Pentaceratops fenestratus[4] and Parasaurolophus tubicen.[5] He was also the first to suggest that the hollow cranial crests of lambeosaurine duckbill dinosaurs could be used as a horn-like noisemaker.[5]

Family

Photograph of a 23-year-old Carl Wiman, 1890.[2]

Wiman was born on 10 March 1867 in the recently inaugurated Märsta railway station,[6] located on Husby-Odensala, Stockholm.[7][8] Wiman's father was a Swedish army captain and Märsta's station-master between 1866 and 1879. Wiman's mother was from Aachen, the daughter of a wealthy Catholic pharmaceutical chemist.[6]

Wiman's childhood was spent accompanying his father on excursions in Uppsala, an amateur naturalist who was also considered to have been a keen hunter. Through these, he gained an interest in all aspects of nature, and performed extensive observations of plants and animals, such as collecting insects. His enjoyment for geology was most likely influenced by visits to his mother's home, where he came upon outcrops of cretaceous chalk that correspond to the Maastricht Formation. In 1885, aged 18, he was introduced to the study of palaeontology by a maternal uncle, a hotel proprietor in Valkenburg who was an amateur geologist and palaeontologist.[6]

Education

In 1888 the 21-year-old Wiman began his studies at Uppsala University and in 1895 obtained his PhD degree with the thesis "Über die Graptoliten" (On Graptolites).[6]

Career

Later life

References

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