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  • Ant-plant interaction  (1)
  • Bohemian Massif  (1)
  • 2020-2022
  • 1995-1999  (2)
  • 1940-1944
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Biodiversity and conservation 4 (1995), S. 165-182 
    ISSN: 1572-9710
    Keywords: Ant-plant interaction ; extrafloral nectaries ; Malaysia ; lowland rain forest
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The first data on the taxonomic distribution and abundance of woody plants with extrafloral nectaries (EFN) from SE Asia are reported. The species richness and frequency of woody angiosperm plants with extrafloral nectaries was studied in the Pasoh Forest Reserve, a primary lowland forest in Peninsular Malaysia. EFN were present on 12.3% of the 741 species surveyed. 91 plant species belonging to 47 genera and 16 families were found to have EFN. Euphorbiaceae, Dipterocarpaceae, Rosaceae, Leguminosae, and Ebenaceae were the families most frequently bearing EFN whereas EFN were rare in the more primitive subclasses of the Magnoliopsida and common in the more advanced taxa (Dilleniidae, Rosidae, Asteridae). Most common were flattened glands associated with the leaf blade. A comparison with data from the Neotropics showed a great similarity in regard to the taxonomic distribution of plants with EFN. EFN-plants occupied 19.3% of the cover of the Pasoh Forest 50 ha plot. Species with EFN were under-represented among shrubs and trees of the understorey. We found an increase in the number of species with EFN as well as in their cover from the understorey to the canopy emergents. EFN were found more often among the abundant species (species with n〉500/50 ha). Percentage occurrence and cover of EFN-bearing plants in the 50 ha plot of primary forest was lower than recorded for secondary habitats in tropical areas. At present, in the core zone of the Pasoh Forest Reserve which has been investigated only few species known to indicate disturbance occur. Therefore most of the recorded EFN-species cannot be regarded as secondary forest plants. The interactions between ants and EFN-bearing plants appear to be rather facultative and nonspecific. In Pasoh we found 28 ant species from seven genera visiting EFN. Most of the EFN-associated ants belonged to the subfamily Myrmicinae while Ponerines were rare, a pattern which was also reported for the Neotropics.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 0016-7835
    Keywords: Key words Teplá ; Barrandian ; Cadomian orogeny ; Variscides ; Bohemian Massif ; Barrovian-type metamorphism
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The Cadomian basement of the Teplá–Barrandian unit is characterized by a classic Barrovian-type metamorphism, the degree of which increases considerably towards the west reaching amphibolite facies conditions in the Domaz˘lice crystalline complex (DCC). The number and volume of plutons also increases towards the west. The emplacement ages of the Te˘s˘ovice granite and the Mrac˘nice trondhjemite have been determined at 521.7±2 Ma and 523+4/–5 Ma, respectively, applying conventional U–Pb analyses of zircons. Pervasive high-temperature prolate fabrics and north-/northwest-dipping, dextral oblique-slip shear zones within the Mrac˘nice trondhjemite suggest a synkinematic melt emplacement within a Lower Cambrian transtensional setting. Transtension is probably related to early-stage rifting that introduced the separation of the Teplá–Barrandian unit (as part of Armorica) from Gondwana. Structural and petrological data of the country rocks show that the Barrovian-type metamorphism and two deformation stages (D1 with unknown kinematics and D2 top-to-the-north shearing) are older than the melt emplacement, and thus can be attributed to the Cadomian orogeny. The intrusion depth of both plutons is nearly the same (ca. 7 km), although the degree of Barrovian-type metamorphism differs significantly within the country rocks. This suggests late Cadomian eastward tilting of the metamorphic isograd planes. The weak post-plutonic, lower-greenschist to subgreenschist facies folding and thrusting result from Variscan northwest/southeast compression.
    Type of Medium: Electronic Resource
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