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31.
Adolf Češka 《Folia Geobotanica》1966,1(3):93-100
Various possibilities of usingSörensen's coefficient of floristic similarity in plant sociology are summarized. A new formula (11), derived from that bySörensen and based on constancy values, is suggested in order to calculate the mean floristic similarity within a set of relevés. 相似文献
32.
Adolf Češka 《Folia Geobotanica》1966,1(2):93-100
Various possibilities of usingSörensen’s coefficient of floristic similarity in plant sociology are summarized. A new formula (11). derived from that bySörensen and based on constancy values, is suggested in order to calculate the mean floristic similarity within a set of relevés. 相似文献
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35.
Radovan Borojević 《Helgoland Marine Research》1967,15(1-4):116-119
Résumé 1. Les travaux deSarà (1953) et deBurton (1963) ont remis en question la valeur systématique des caractères morphologiques dans la classification des Eponges Calcaires, et ont proposé de considérer de nombreuses formes connues comme des variétés individuelles et régionales d'espèces très plastiques et variables. Nous avons essayé de préciser, par l'observation directe en plongée libre, la distribution et les préférences écologiques des Calcaires, de définir ainsi les limites naturelles de leurs populations, et d'étudier ensuite la variabilité des caractères morphologiques à l'intérieur de ces populations.2. Nous exposons ici l'exemple des espèces des genresClathrina etAscandra, étudiées en Adriatique, dans les régions de Marseille et de Roscoff. Leur distribution est en rapport direct et très précis avec l'exposition aux vagues et à la lumière, à tel point que sur une surface réduite plusieurs espèces se succèdent et se remplacent en fonction de l'exposition de l'endroit. Dans la règion de Roscoff cette distribution est plus large ce qui est dû aux effets des marées, mais les zones écologique préférentielles pour les espèces deClathrina ont pu être établies en fonction de l'importance de l'apport des sédiments par les eaux côtières.3. La possibilité de définir des populations dont la distribution est très précisemment délimitée malgré une coexistence dans un espace réduit, et qui ne sont pas réliées par les formes transitoires, permet d'éliminer l'hypothèse de la cospécificité de ces populations. Elle permet également d'établir les variations morphologiques possibles au sein d'une espèce, de retenir les caractères significatifs pour la classification, et finalement de distinguer les espèces qui se ressemblent morphologiquement. Dans le cas d'animaux qui, commeClathrina, possèdent très peu de caractères utilisables en systématique, c'est la seule façon de résoudre les problèmes de leur taxonomie.
The importance of research on the ecological distribution for the taxonomy of calcareous sponges
The particular difficulties of the taxonomy of calcareous sponges are due to their great plasticity and their capacity for adaptation which obscure the natural limits of species. An attempt was made to define the natural populations of the Mediterranean species of the generaClathrina andAscandra through a study of their ecological distributions. The populations not connected by the transitory forms were defined by their ecological preferences, and, as they are found in a close cohabitation, were treated as having the specific values. The variability of different morphological features is discussed, the features significant for taxonomy are pointed out and the morphologically close species are defined.相似文献
36.
Investigation of halophyte communities of Western substeppe ilmens of the Volga delta and their classification by theBraun-Blanquet method enabled us to distinguish 5 associations in this area:Suaedo salsae-Halocnemetum, Limonietum suffruticosi, Kalidietum foliati, Suaedo-Frankenietum, Suaedo-Petrosimonietum. These associations were united in the new allianceClimacoptero-Suaedion previously included in the orderHalostachyetalia ?opa 1939, the classPuccinellio-Salicornietea ?opa 1939. 相似文献
37.
The greening of the upper part of the outerAllium cepa L. bulb scales, in particular along the vascular regions, is limited to the hypodermal cells in which typical leucoplasts are transformed to normal and functional chloroplasts. This process is light dependent and cannot afterwards be reversed or modified by darkness. The changes in fine structure are described and briefly discussed.Dedicated to Prof. DrLothar Geitler on the occasion of his 90th birthday and 55 years after the publication of his Grundriß der Cytologie. 相似文献
38.
Lectins extracted from corn (Zea mays L.) kernel with Tris-HCl buffer pH 7.5 were isolated from the crude extract by affinity chromatography on Sepharose 6B-N-acetyl-d-galactosamine and Sepharose 6B-methylα-d-mannoside, and also by lectin affinity chromatography using concanavalin A and Lens culinaris lectin as ligands. According to preferential monosaccharide specificity, salt-soluble lectins of corn seed comprise at least two distinct types: N-acetyl-d-galactosamine-interactive and mannose-interactive lectins. The extracted lectins are unstable, with a tendency to form aggregates during storage. 相似文献
39.
Biological Trace Element Research - The ko-standardization method is suitable for routine multielement determinations by reactor neutron activation analysis (NAA). Investigation of NIST standard... 相似文献
40.
The areal distribution of organic C contents, 13C values, total N and P and biogenic Si contents in surficial sediments were used to study the distribution, origin and diagenetic transformations of sedimented biogenic debris in the eutrophic subalpine Lake Bled (Slovenia), which for most of the yearhas an anoxic hypolimnion. The influence of an allochthonous input, restricted to the western basin, was clearly traced by higher organic C and total N and P contents, higher 13C values, and higher sedimentation rate in comparison to the eastern basin. The low 13C values of sedimentary organic matter in the major part of the lake, lower than the 13C values of different types of organic matter, suggest that this sedimentary organic matter is most probably the product of a microbial community and not a residue of primary production.The temporal variation of benthic diffusive fluxes of NH4, Si and PO4, derived from modelling the pore water profiles, was related to sedimentation of phytoplanktonic blooms, while the PO4 fluxes were also dependent on changing redox conditions at the sediment-water interface in the period of the winter-spring overtum. The removal of PO4 in pore waters is probably due to the adsorption of phosphate and precipitation of apatite and vivianite. The budget of C, N and P at the sediment-water interface revealed a high recycling efficiency (>70%), also confirmed by the rather uniform (or only slightly decreasing) vertical profiles of organic C, total N and P in sediment cores and C/N and C/P ratios. The percentage of biogenic Si recycling is low (<10%), suggesting its removal in sediments. 相似文献