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Biological insurance theory predicts that, in a variable environment, aggregate ecosystem properties will vary less in more diverse communities because declines in the performance or abundance of some species or phenotypes will be offset, at least partly, by smoother declines or increases in others. During the past two decades, ecology has accumulated strong evidence for the stabilising effect of biodiversity on ecosystem functioning. As biological insurance is reaching the stage of a mature theory, it is critical to revisit and clarify its conceptual foundations to guide future developments, applications and measurements. In this review, we first clarify the connections between the insurance and portfolio concepts that have been used in ecology and the economic concepts that inspired them. Doing so points to gaps and mismatches between ecology and economics that could be filled profitably by new theoretical developments and new management applications. Second, we discuss some fundamental issues in biological insurance theory that have remained unnoticed so far and that emerge from some of its recent applications. In particular, we draw a clear distinction between the two effects embedded in biological insurance theory, i.e. the effects of biodiversity on the mean and variability of ecosystem properties. This distinction allows explicit consideration of trade-offs between the mean and stability of ecosystem processes and services. We also review applications of biological insurance theory in ecosystem management. Finally, we provide a synthetic conceptual framework that unifies the various approaches across disciplines, and we suggest new ways in which biological insurance theory could be extended to address new issues in ecology and ecosystem management. Exciting future challenges include linking the effects of biodiversity on ecosystem functioning and stability, incorporating multiple functions and feedbacks, developing new approaches to partition biodiversity effects across scales, extending biological insurance theory to complex interaction networks, and developing new applications to biodiversity and ecosystem management.  相似文献   
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Follow-up data on a girl with 3 beta-hydroxysteroid dehydrogenase deficiency at a pubertal bone age are presented. On examination at age 14.7 years (bone age 12 years), there was no spontaneous breast development. On treatment with hydrocortisone and fludrocortisone, most steroids with the exception of increased 17OH-pregnenolone in plasma and delta 5-pregnenetriol and pregnanetriol in urine, were normal. After 1 week off hydrocortisone, plasma 17OH-pregnenolone, DHA and delta5-androstenediol and urinary delta 5-pregnenetriol and pregnanetriol increased markedly, while plasma 17OH-progesterone increased only slightly. On increased hydrocortisone medication, there was no response of plasma estradiol to HMG. This first observation of a pubertal girl with 3 beta-hydroxysteroid dehydrogenase deficiency indicates that in this patient, the defect persists at a pubertal bone age and that it is not limited to the adrenals, but also affects the ovaries. Girls with this type of defect thus require estrogen replacement at a bone age of about 12 years. The large quantities of pregnanetriol in the urine are not due to an incomplete defect or an additional 21-hydroxylase deficiency, but most likely to the peripheral or hepatic conversion of 17OH-pregnenolone or delta 5-pregnenetriol.  相似文献   
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Aim The high amount of species diversity concentrated in southern Africa has been attributed to palaeoclimatic factors, and the timing of radiations in some taxa corresponds to global palaeoclimatic trends. Using dwarf chameleons (Bradypodion: Chamaeleonidae) as a model system, we explored the relationship between palaeoclimatic fluctuations and cladogenesis with respect to both temporal and spatial patterns in an effort to understand the process of speciation in southern Africa. Location South Africa, with particular emphasis on the Cape Floristic Region and the Maputaland–Pondoland–Albany hotspot. Methods Mitochondrial sequence data (ND2 and 16S) were used to estimate the timing of major radiations and to examine the number of lineages through time. A dated phylogeny was constructed using Bayesian phylogenetic reconstruction, and a Bayesian relaxed molecular clock was used to estimate divergence times. Spatial data and lineage‐through‐time plots were used to identify geographic regions that underwent diversification in connection with major climatic events. Both parsimony and likelihood optimizations of habitat type on the phylogeny were used to determine whether major habitat shifts have occurred. On a coarse scale (half‐degree grid cells), phylogenetic diversity (sum of the branch lengths linking terminals) was compared with species richness (absolute number of species) to identify areas of conservation importance. Results The complete species phylogeny of dwarf chameleons shows that the timing and mode of diversification exhibit spatio‐temporal patterns that link to phases in the evolution of southern Africa’s climate over the last 14 Myr. Optimizations of habitat on the phylogenetic tree show a progression from closed to open habitats since the Mid‐Miocene, corresponding to the shift from C3 to C4 environments, and later with the development of south‐western Africa’s winter‐rainfall regime. These shifts are not simultaneous across the region, with different geographic centres of diversity generated during different time periods. Main conclusions Regions that are prominent centres of chameleon diversification are encompassed by the current biodiversity hotspots as shown by chameleon species richness and phylogenetic diversity. Diversity within the Cape Floristic Region appears to be the result of a Late Pliocene radiation, whereas the diversity encompassed within the Maputaland–Pondoland–Albany hotspot is an aggregate of asynchronous radiation events, probably influenced by lineage losses. Overall, dwarf chameleons have experienced a shift in habitat types, with recent radiations occupying open habitats, and older lineages persisting in relictual forested habitats, corresponding to the continental shift of vegetation types since the Miocene Climatic Optimum.  相似文献   
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