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11.
K. D. SMITH 《Ibis》1974,116(2):155-164
The changes brought about by the introduction of Eucalyptus into Africa on the ecology of birds are outlined, in so far as its contribution as a habitat, as a food-source, and for other uses is concerned. Species known to breed in gums are listed, together with notes on habitat preference, and its limitations in comparison with the indigenous resources are discussed. 相似文献
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Interactions of Abscisic Acid, Cytokinin and Gibberellin in the Control of Betacyanin Synthesis in Seedlings of Amaranthus caudatus 总被引:2,自引:0,他引:2
In de-rooted seedlings of Amaranthus caudatus L., betacyanin synthesis induced by white light or cytokinin was inhibited by abscisic acid (ABA) or a mixture of gibberellins A4 and A7 (GA4/7). The GA4/7 and ABA effects were additive. Thus ABA inhibited the cytokinin action but had no effect on the gibberellin response. 相似文献
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Whereas zoospores of six cultures of O. brassicae were immobile after treating in glycine solution at 35–40°C for 10 min, those of a cucurbit culture of O. radicale were immobile only after heating at 45°C. Further, O. radicale multiplied in cucumber at 20°, 30° and 35°C, whereas O. brassicae multiplied at 20°, but not 30° or 35°C. Such differences in reaction to temperature might sometimes be useful in separating mixtures of the two species in common hosts such as cucumber. 相似文献
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Nitrogen (N) mineralization rates and the temperature response patterns of mineral N production in surface (0–7.6 cm) soils were compared in laboratory incubation studies based on disturbed, composite samples. Seasonal variation in the field levels of mineral N, and mineralization potential of intact (7.6 × 5.6 cm diameter) soil cores, were also investigated. Ammonification proceeded rapidly in each soil. Nitrification did not occur in grassy forest (GF) soil but was active in both layered forest (LF) and mossy forest (MF) soils, especially the former. Total mineral N production was greatest in MF and least in LF. Ammonification in disturbed samples was maximal at 50°C in all three soils with a secondary peak at 10°C in LF soil. Nitrification in LF and MF soils was most rapid at 25°C. Several species of ammonifying bacteria with different temperature optima were isolated, indicating that the process of ammonification is a composite of the activities of a variety of decomposer microbes. Mean field levels of mineral N and NH4–N throughout the year were greatest in MF and least in LF. Seasonal fluctuations in NH4–N were evident, concentrations being universally low in mid-winter (about 1.5 μgg-1), increasing to a maximum in late summer (about 5 μg g-1 in LF: 16–18 μg g-1 in GF and MF). Field levels of NO3–N were more constant and never more than 5 μg g-1 in any community. Both total mineralization and ammonification in intact cores were greatest in MF and least in LF while nitrification was greatest in LF and almost negligible in GF, thus confirming the results obtained with disturbed samples. The potential for mineralization was large in mid-winter when the amount of mineral N was very low, and small in late summer when field levels were higher: this is interpreted as indicating that seasonal climatic factors regulate the availability of substrates for decomposers. Spatial variability in field levels of mineral N and mineral N production in the laboratory was evidenced by significant ‘sampling site’ effects in each community: however, at the sampling intensity used, the presence of bark mounds around Eucalyptus saligna trees could not be shown to affect these attributes. The inability of GF soil to nitrify when incubated in the laboratory could not be ascribed to a high C/N ratio, low pH, lack of substrate ammonium, or a low population of autotrophic nitrifying bacteria. No attempt was made to investigate the presence of allelopathic nitrification inhibitors. No evidence was obtained to support the view that nitrification is atypical of climax communities in situ. The most productive forest (LF) had the greatest capacity to nitrify and the least productive community (GF) the smallest capacity to do so. 相似文献
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An account is given of sperm competition in Locusta migratoria, for cases where the competing ejaculates occur either as one per oviposition cycle or as two per cycle. These situations exert quite different sperm competition effects; evolutionary reasons for this are discussed. The adaptive value of the male precopulatory passive phase behaviour is considered in relation to sexual selection and sperm competition. 相似文献
20.
THOMAS J. SIMONSEN 《Biological journal of the Linnean Society. Linnean Society of London》2006,89(4):627-673
Species-level phylogeny of the Butterfly tribe Argynnini is established based on 141 characters derived from wing and genitalia morphology of both sexes. The Argynnini can be divided into three subtribes; Yrameina comprising Yramea and Boloria s . l ., Argynnina comprising Prokuekenthaliella , Issoria , Brenthis , and all the 'large fritillary' species joined in the genus Argynnis s . l . and a new subtribe Euptoietina comprising only the genus Euptoieta . The classical genus Issoria s . l . is polyphyletic regarding Yramea and possibly paraphyletic regarding the two Afrotropic species baumanni and hanningtoni ; these two species are tentatively transferred to the old genus/subgenus Prokuekenthaliella . Surprisingly, one Afrotropic species, Issoria smaragdifera is closely related to the East Palaearctic Issoria species. A revised classification of Argynnini is proposed based on the obtained phylogeny. Studies of larval host plants based on the obtained phylogeny suggest that the ancestral Argynnini used Passiflora and Violaceae, but already the ancestor of Yrameina + Argynnina was probably specialized on Violaceae. Whereas the Boloria species have turned to other food plants such as Dryas , Vaccinium and Salix on several occasions, only Brenthis among the Argynnina use other host plants than Viola (mainly Rosaceae). The habit of laying eggs away from the food plant has probably evolved twice within Argynnina. © 2006 The Linnean Society of London, Biological Journal of the Linnean Society , 2006, 89 , 627–673. 相似文献