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EA Dukhanina TI Lukyanova EA Romanova V Guerriero NV Gnuchev GP Georgiev DV Yashin LP Sashchenko 《Cell cycle (Georgetown, Tex.)》2015,14(22):3635-3643
PGRP-S (Tag7) is an innate immunity protein involved in the antimicrobial defense systems, both in insects and in mammals. We have previously shown that Tag7 specifically interacts with several proteins, including Hsp70 and the calcium binding protein S100A4 (Mts1), providing a number of novel cellular functions. Here we show that Tag7–Mts1 complex causes chemotactic migration of lymphocytes, with NK cells being a preferred target. Cells of either innate immunity (neutrophils and monocytes) or acquired immunity (CD4+ and CD8+ lymphocytes) can produce this complex, which confirms the close connection between components of the 2 branches of immune response. 相似文献
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阿尔泰山是欧亚大陆最为宏伟的山脉之一,其中段的西南坡坐落于中国新疆境内,众多具温带性质的藓类植物分布于此。作者在对阿尔泰山进行苔藓植物区系调查过程中,发现了分布于阿尔泰山的喀纳斯自然保护区及布尔津县禾木乡的2个藓类植物中国新记录种——隶属曲尾藓科的短叶曲尾藓[Dicranum brevifolium(Lindb.)Lindb.]和卷叶小曲尾藓[Dicranella crispa(Hedw.)Schimp.]。由地理分布可知,短叶曲尾藓和卷叶小曲尾藓在中国皆为稀有种类。 相似文献
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Frantiek Krahulec Hana Sklov Tom Herben Vra Hadincov Radka Wildov Sylvie Pech
kov 《应用植被学》2001,4(1):97-102
Abstract. Sheep grazing was investigated as an alternative to traditional management of meadows in the Krkono?e Mts. Until the second World War these meadows were mown in mid‐summer and grazed by cattle for the rest of the season. Subsequent abandonment of the meadows has resulted in decreasing species richness. Degradation phases of the former communities have been replacing the original species‐rich vegetation. Significant changes were apparent six years after the introduction of sheep grazing. In grazed plots the proportion of dominant herbs (Polygonum bistorta and Hypericum maculatum) decreased and grasses (Deschampsia cespitosa, Festuca rubra, Agrostis capillaris, Anthoxanthum alpinum) increased. The increase in grasses was positively correlated with an increase in several herbs. The proportion of some herbs increased despite being selectively grazed (Adenostyles alliariae, Melandrium rubrum, Veratrum lobelianum). Any losses caused by grazing of mature plants were probably compensated by successful seedling establishment. Cessation of grazing resulted in significant changes in vegetation within three years. The cover of nitrophilous tall herbs and grasses (e.g. Rumex alpestris, Holcus mollis, Deschampsia cespitosa, Geranium sylvaticum) increased in the abandoned plots. In the plots grazed for nine years cover of species‐rich mountain meadow species increased (e.g. fine‐leaved grasses, Campanula bohemica, Potentilla aurea, Viola lutea, Silene vulgaris). The main conservation risk is the expansion of a competitive species with low palatability, Deschampsia cespitosa. This species can be suppressed by a combination of grazing and mowing. In order for grazing to be effective, the number of sheep should be proportional to meadow production. This may be difficult to maintain as production is variable and is impossible to predict at the beginning of a growing season. A large part of the biomass may thus remain intact in some years. Negative effects of grazing may be, at least partly, eliminated by a combination of cutting and grazing. 相似文献
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Summary The present paper presents results of stratigraphical, sedimentological and micropalaeontological investigations of an olistolith
from the Büd?skút area in the Bükk Mts (NW Hungary). The olistolith consists of Norian sub- and peritidal platform carbonates
(Büd?skút lime-stone). During early diagenesis dissolution cavities originated which where filled by ostracodal mudstones.
Other cavities first were wallpapered by evinospongial crusts and later filled either by ostracodal mudstones or by brick-red
haematitic material (weathered bauxite). The evinospongial crusts show stromatolite-like structures and their forming therefore
is supposed to be organically (microbially) induced.
During the Early up to the Late Jurassic the host rock was dissected by neptunian dykes. The internal sediment's faunal content
reveals that the dykes formed during the (?) Hettangian/Sinemurian and the Toarcian— Oxfordian age.
A comparison of the Büd?skút limestone neptunian dyke internal sediments with the Bükk parautochthonous and the Szarvasko-Mónosbél
nappe complex sedimentary columns shows no similarities. Therefore the Büd?skút olistolith is interpreted as an exotic body
within the Bükk Mts. 相似文献
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