ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 2015-2019  (3)
Collection
Years
Year
  • 1
    Publication Date: 2016-07-16
    Description: The contributions of the La Plata Museum to the geology of Argentina began following the exploratory trips of its founder, F.P. Moreno, in the 1870s. The geological expeditions of the La Plata Museum started in the 1880s and covered the Andean region, although they were focused in the Patagonian Andes. They became more important from 1893 when they were related to explorations aimed at fixing the boundary between Argentina and Chile. Within 10 years the geographical and geological bases of large and almost unknown regions were established. R. Hauthal studied the area between the Last Hope Inlet and Lake Belgrano, defining its stratigraphy and publishing the first geological map of the Cordilleran region between c. 49° 30' and 52° S. The geology between Lake Buenos Aires and the Rio Negro (41–47° S) was established by Santiago Roth. The stratigraphic succession, facies and structural changes through the Argentine–Chilean Cordillera at the latitude of Lake Nahuel Huapi and Lake Lacar were studied by L. Wehrli, while studies at the latitude of Neuquén and Mendoza (36–39° S) were carried out by C. Burckhardt. Mesozoic and Cenozoic fossils were studied either in the Museum or abroad. Supplementary material: Map of southern South America (Argentina and Chile) showing the distribution of towns in 1870 is available at http://doi.org/10.6084/m9.figshare.c.3283385.v1
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2016-07-01
    Description: Joaquín Frenguelli was born in Rome, Italy in 1883 and died in Santa Fe, Argentina in 1958. After receiving his PhD in medicine from Rome University, he moved to Argentina in 1911 and worked as a medical doctor in the cities of Santa Fe and Córdoba until 1929. From 1920 until 1933 he was a professor of geology at the Littoral National University. In 1934 he moved to La Plata, where he was director of the Museum of Natural Sciences (1935–46). The scientific work of Frenguelli is characterized by its scope and excellence and its main focus was on the Late Cenozoic. Frenguelli modified the chronology of the stratigraphic scheme of the Pampas region, proposed a relationship with climatic episodes and then expanded it, directly or indirectly, to the whole record of the Late Cenozoic in Argentina. His contributions on diatoms and other microscopic organic remains, as well as on fossil vertebrates and invertebrates, were related to the environmental setting of the Late Cenozoic. In the 1940s, Frenguelli also worked on the fossil plants of the continental Upper Palaeozoic and Early Mesozoic rocks of Argentina. As a result, he characterized the Triassic successions, introducing new stratigraphic units and discussing their relationships and chronology.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2016-10-08
    Description: Coleoid specimens from the Jurassic of northern Chile are included in two different species of Trachyteuthis , i.e., T. covacevichi Fuchs and Schultze, 2008 and T. chilensis n. sp., and in a new genus and a new species, Pseudoteudopsis perezi n. gen. n. sp. The specimens described and figured are from two different areas in northern Chile. Those referred to Pseudoteudopsis perezi n. gen. n. sp. came from a locality north of Calama and are associated with ammonites indicating the lower Callovian uppermost bodenbenderi to lowermost proximum zones ( gracilis Standard Zone) of the Andean ammonite zonation. Those described as T. covacevichi and T. chilensis n. sp. came from the Cordillera de Domeyko, northeast of Taltal, and are associated with ammonites indicating the middle Oxfordian transversarium Zone.
    Print ISSN: 0022-3360
    Electronic ISSN: 1937-2337
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...