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  • Other Sources  (2)
  • Anden  (1)
  • Porifera  (1)
  • English  (2)
  • Russian
  • 1995-1999  (2)
  • 1960-1964
  • 1945-1949
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  • 1995-1999  (2)
  • 1960-1964
  • 1945-1949
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  • 1
    facet.materialart.
    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-17
    Description: Contents ; List of Contributors ; Introduction ; I. General Problems of Sponge Biology. S. M. Efremova: Once more on the position among Metazoa - Gastrulation and germinal layers of sponges ; N. N. Marfenin: Sponges viewed in the light of up-to-date conception on coloniality ; A. V. Ereskovsky & G. P. Korotkova: The reasons of sponge sexual morphogenesis peculiarities II. Developmental Biology of Sponges. O. M. Ivanova-Kazas: Analysis of the sponges ontogeny at sexual reproduction ; R. P. Anakina: The cleavage specifity in embryos of the Barents Sea sponge Leucosolenia complicata Montagu (Calcispongiae, Calcaronea) ; L. V. Ivanova: New data about morphology and metamorphosis of the spongillid larvae (Porifera, Spongillidae). 1. Morphology of the free-swimming larvae ; L. V. Ivanova: New data about morphology and metamorphosis of the spongillid larvae (Porifera, Spongillidae). 2. The metamorphosis of the spongillid larvae ; L. V. Ivanova & V. V. Semenov: Feeding habits of the larvae of sponges ; N. A. Sizova & A. V. Ereskovsky: Ultrastructural peculiarities of the early embryogenesis in a White Sea sponge Halisarca dujardini (Demospongiae, Dendroceratida) ; III. Ecology of Sponges. R. P. Anakina & E. I. Slepian: Spiculas' malformations of freshwater sponges as indicators of water environment in St. Petersburg City ; A. S. Plotkin & A. V. Ereskovsky: Ecological aspects of asexual reproduction of the White Sea sponge Polymastia mammillaris (Demospongiae, Tetractinomorpha) in Kandalaksha Bay ; I. S. Smirnov & V. M. Koltun: Symbiosis of the antarctic sponge genus lophon (Porifera) and ophiuroid genus Ophiurolepis (Ophiuroidea, Echinodermata) ; IV. Palaeontology and Systematics. L. V. Bolshakova: Stromatoporoids - the fossil sponges ; E. V. Veinberg, 0. M. Khlystov, S. S. Vorobyova, E. G. Kornakova, 0. V. Levina, S. M. Efremova, & M. A. Grachev: Distribution of sponge spicules in sediments of the underwater Akademichesky ridge of Lake Baikal ; K. R. Tabachnik & C. Levi: Amphidiscophoran Hexasterophora (Part I & II) ;
    Description: conference
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Porifera ; Paläobiologie
    Language: English
    Type: doc-type:book
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  • 2
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften Freie Universität Berlin
    In:  SUB Göttingen | 98 B 4059
    Publication Date: 2024-05-03
    Description: Die Andenkordillere entstand entlang des westlichen Randes von Südamerika aufgrund der Subduktion der ozeanischen Nazca-Platte unter die kontinentale Südamerikaplatte seit dem Jura. Als solche werden die Anden als ein klassisches Beispiel eines Orogens entlang eines aktiven Kontinentalrandes betrachtet. Obwohl die gegenwärtige Physiographie das Ergebnis der Andinen Tektonik ist, sind die Zentralanden das Ergebnis von einem komplexen Zusammenspiel von Präkambrischen und Paläozoischen Terrane-Akretionen und Phasen von Kompression und Extension. Die Puna und die Ostkordillere spielen in diesem Zusammenhang eine entscheidende Rolle in der tektonischen Entwicklung der Zentralanden. Die vorliegende Untersuchung befasst sich mit dem Gebiet der nördlichen argentinischen Puna und der Ostkordillere, von etwa 22°S bis 24°S und 65 °W bis 66°30' W. Es wurden etwa 1200 km Seismik interpretiert, deren Ergebnis als Randbedingung in die Konstruktion des gravimetrischen 3D Modells des Gebietes einging.
    Description: The Andes Mountains developed along the western margin of SouthAmerica in response to the subduction of the oceanic Nazca Plate below the South American plate since the Jurassic times. It is considered as one of the classic examples of a mountain chain developed in an active continental margin. Although their present physiography is given by the Andean tectonics, the Central Andes are the result of complex interplay of Precambrian and Paleozoic terrane accretion and phases of compression and extension. The Puna and Eastern Cordillera represent key elements in the tectonic evolution of the Central Andes. The present study covers a region of the northern Puna and Eastern Cordillera extending from approximately 22°S to 24°S and 65 °W to 66°30'W in Argentina. About 1200 km of seismic lines were interpreted and were used as a geometrical constraint for the construction of a 3D gravity model of the area.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:558 ; Anden ; Argentinien ; Seismik
    Language: English
    Type: doc-type:book
    Format: 192
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