阿拉善荒漠区6种主要灌木植物叶片C:N:P化学计量比的季节变化

为了解同一生活型不同种植物叶片碳(C)、氮(N)、磷(P)生态化学计量学特征随季节变化的响应规律,在生长季不同月份,对阿拉善荒漠区6种主要灌木植物霸王(Zygophyllum xanthoxylum)、白刺(Nitraria tangutorum)、红砂(Reaumuria soongorica)、驼绒藜(Ceratoideslatens)、猫头刺(Oxytropis aciphylla)、沙冬青(Ammopiptanthus mongolicus)的物候期进行了连续的观察,并采集植物叶片,分析了其C、N、P含量及计量比在不同月份的变化.结果显示:1)同一生活型的6种植物的叶片C、N、P及C:N、C:P和N:P在整个生长季内的变化规律不同,且以上各指标季节间的变异系数在6种植物之间也存在差异;2)单个植物种叶片C、N、P含量及其计量比的季节变异分析显示,叶片C、N含量及C:N的季节变异较小,叶片P含量及C:P和N:P的季节变异较大,6种植物叶片C、N含量及C:N由于季节变异所计算的变异系数变化范围分别为0.60％-10.20％、6.09％-20.50％和5.87％-18.78％,6种植物叶片P含量的季节变异所产生的变异系数范围为16.43％-43.43％,叶片C:P和N:P的变异系数范围分别为8.48％-31.95％和11.86％-40.73％;3)综合分析6种植物叶片C、N、P及其计量比各指标在整个生长季节内的变异,变异系数由大到小排序为:P(28.85％)＞C:P(25.02％)＞N:P(22.18％)＞N(14.22％)＞C:N(12.48％)＞C(4.62％);4)生长季节与植物种类对植物叶片C、N、P及其计量比影响的交叉分析显示,植物叶片C、N含量的变异主要受植物种类影响,植物叶片P含量的变异主要受生长季节影响,植物叶片C:N、C:P和N:P的变异都主要受植物种类影响.     

Hypertonic activation of a non-selective cation conductance in HeLa cells and its contribution to cell volume regulation

In whole-cell recordings on single HeLa cells, the hypertonic activation of a cation conductance with a selectivity ratio P(Na):P(Li):P(K):P(Cs):P(NMDG):P(Ca):P(Cl) of 1.00:0.86:0.84:0.56:0.10:0.07:0.15 was observed. This (non-selective) cation conductance was reduced to 59 and 30% of maximal stimulation by Gd(3+) and flufenamate, respectively, but it was insensitive to amiloride (with each compound applied at 100 microm/l). As was determined by the Coulter counter technique, the cation conductance was the main mechanism of regulatory volume increase (RVI) in HeLa cells. Whereas a significant contribution of Na(+)/H(+) antiport was also detectable, Na(+)-K(+)-2Cl(-) symport most likely did not contribute to RVI.     

Inhibitory effect of saliva from secretors and non-secretors on binding of meningococci to epithelial cells

Abstract Carriage of Neisseria meningitidis B:4:P1.15 was higher among non-secretors during a school outbreak of meningitis; non-secretors had lower levels of anti-meningococcal salivary IgM. Flow cytometry was used to assess effects of secretor and non-secretor saliva on binding of B:4:P1.15 to buccal epithelial cells: (1) to assess inhibition by IgA and IgM; and (2) to assess contributions of salivary antibodies to inhibitory activities. Greater inhibition was obtained with secretor saliva: pooled ( P = 0.049); fresh ( P = 0.0001). Purified IgA ( P = 0.02) and IgM ( P = 0.03) were equally inhibitory. After absorption of anti-meningococcal antibodies, there was still significant inhibitory activity in the pools: secretors ( P = 0.018); non-secretors ( P = 0.005). These results indicate that both secretory immunoglobulins and other factors contribute to protection against colonisation by meningococci and might explain the increased carriage of B:4:P1.15 in this population.     

Effects of desertification on the C:N:P stoichiometry of soil,microbes, and extracellular enzymes in a desert grassland

为探讨荒漠草地沙漠化对“土壤-微生物-胞外酶”系统生态化学计量的影响机理, 该研究采用空间序列代替时间演替的方法, 研究了宁夏盐池荒漠草地沙漠化过程中土壤、土壤微生物及土壤胞外酶碳(C)、氮(N)、磷(P)生态化学计量的变异特征。结果表明: (1)随着荒漠草地沙漠化的不断加剧, 土壤C、N、P含量和土壤C:P、N:P均呈降低趋势, 而土壤C:N逐渐增加。(2)荒漠草地沙漠化过程中, 土壤微生物生物量C (MBC):微生物生物量P (MBP)、微生物生物量N (MBN):MBP和土壤β-葡萄糖苷酶(BG):N-乙酰氨基葡萄糖苷酶(NAG)逐渐降低, 而土壤BG:磷酸酶(AP)和NAG:AP基本表现为增加趋势。(3)随着荒漠草地沙漠化程度的加剧, 土壤微生物C利用效率CUE_C:N和CUE_C:P与土壤微生物N利用效率NUE_N:C和土壤微生物P利用效率PUE_P:C的变化趋势相反。(4)荒漠草地土壤、土壤微生物生物量和土壤胞外酶C:N化学计量(C:N, MBC:MBN, BG:NAG)与土壤、土壤微生物生物量和土壤胞外酶N:P化学计量(N:P, MBN:MBP, NAG:AP)显著负相关, 而土壤和胞外酶C:N化学计量(C:N, BG:NAG)与土壤和胞外酶C:P化学计量(C:P, BG:AP)显著正相关。土壤N:P与土壤MBN:MBP显著正相关, 而与土壤NAG:AP显著负相关。分析表明, 荒漠草地沙漠化过程中土壤微生物生物量及胞外酶活性随着土壤养分的变化而发生变化; 微生物-胞外酶C:N:P生态化学计量与土壤养分存在协变关系, 为理解荒漠草地土壤-微生物系统C、N、P循环机制提供理论依据。     

Effects of different nitrogen:phosphorus levels on the growth and ecological stoichiometry of Glycyrrhiza uralensis

Aims The increase in atmospheric nitrogen (N) deposition has accelerated N cycling of ecosystems, probably resulting in increases in phosphorus (P) demand of ecosystems. Studies on the effects of artificial N:P treatment on the growth and carbon (C), N, P ecological stoichiometry of desert steppe species could provide not only a new insight into the forecasting of how the interaction between soils and plants responses to long-term atmospheric N deposition increase, but also a scientific guidance for sustainable management of grassland in northern China under global climate change. Methods Based on a pot-cultured experiment conducted for Glycyrrhiza uralensis (an N-fixing species) during 2013 to 2014, we studied the effects of different N:P supply ratios (all pots were treated with the same amount of N but with different amounts of P) on aboveground biomass, root biomass, root/shoot ratio, and C:N:P ecological stoichiometry both in G. uralensis (leaves and roots) and in soils. Additionally, through the correlation analyses between biomass and C:N:P ecological stoichiometry in leaves, roots, and soils, we compared the differences among the C:N:P ecological stoichiometry of the three pools, and discussed the indication of C:N:P ecological stoichiometry in soils for the growth and nutrient uptake of G. uralensis. Important findings The results showed that, reducing N:P decreased C:P and N:P ratios both in G. uralensis (leaves and roots) and in soils but increased aboveground biomass and root biomass of G. uralensis, indicating that low to moderate P addition increased P availability of soils and P uptake of G. uralensis. However, excessive low N:P (high P addition) led to great decreases in soil C:P and N:P ratios, thus hindering N uptake and the growth of G. uralensis. C:N:P ratios in the two pools of G. uralensis (especially in leaves) had close correlations with soil C:N:P ratio, indicating that the change in soil C:N:P ratio would have a direct influence on plants. Our results suggest that, through regulating C:N:P ratio in leaves and soils, appropriate amounts of P addition could balance soil P supply and plant P demand and compensate the opposite influences of long-term atmospheric N deposition increase on the structure of desert steppe.     

氮磷添加对荒漠草原植物-凋落物-土壤生态化学计量特征的影响

为明确植物、凋落物和土壤养分含量及化学计量比对土壤中添加多种限制性养分的响应,阐明“植物-凋落物-土壤”连续体化学计量动态及各组分之间的协同作用,以宁夏荒漠草原为研究对象,于2018年开始进行氮(N)、磷(P)养分添加控制试验。试验处理包括对照(CK)、N添加、P添加、NP共同添加4个处理。结果表明：(1)NP共同添加显著增加了荒漠草原植物N和P含量、以及凋落物和土壤P含量,显著降低了荒漠草原植物C∶N和C∶P、以及土壤和凋落物C∶P和N∶P。P添加显著增加了荒漠草原植物、凋落物和土壤P含量,显著降低了植物、凋落物、土壤C∶P和N∶P。N添加分别增加了植物、凋落物N含量和N∶P,但对植物N含量影响未达到显著水平。(2)C、N、P含量和N∶P大小均表现为植物>凋落物>土壤,C∶N和C∶P均表现为凋落物>植物。(3)N添加提高了荒漠草原植物对P再吸收效率,降低了荒漠草原植物对N利用效率;P添加提高荒漠草原植物对N再吸收效率,降低荒漠草原对P的利用效率;NP共同添加提高了荒漠草原植物对N和P再吸收效率,降低了荒漠草原植物对N和P利用效率。(4)植物-凋落物-土壤的N、P含量...     

Structural Roles of Polyoma Virus Proteins

The superhelical, closed circular form of polyoma deoxyribonucleic acid (DNA) (Co 1) is bound in a 25S DNA-protein complex to the viral histone-like proteins after alkaline disruption of the virion. Nicked viral DNA or linear DNA are largely free of protein. Most of the viral protein disruption is in the form of capsomeres, sedimenting principally at 10S and 7S. Despite the relatively constant ratio of 10S to 7S material in many preparations, (1:5.5 to 1:6.0, respectively), the two classes of capsomeres are indistinguishable by electron microscopy and contain only P(2), P(3), and P(4) in molar ratios of approximately 5:1:1 or 6:1:1, respectively. Material with sedimentation rates of approximately 1 to 3S is enriched for P(5) and contains small amounts of P(2), P(3), and P(4). During the in vitro reassembly of DNA-free, shell-like particles from disrupted virus, proteins P(1), P(2), P(3), P(4), and P(7) are reincorporated efficiently, whereas P(5) and P(6) are not. The presence in empty reassembled particles of histone-like protein, expecially P(7), implies that at least this one of the minor protein components of the virion may participate in protein-protein interactions with other components of the capsid.     

氮沉降和经营强度对毛竹林凋落叶生态化学计量特征的影响

为探讨氮沉降和经营强度对毛竹凋落叶化学计量特征的影响,研究了不同强度模拟氮沉降(低氮: 30 kg N·hm^-2·a^-1;中氮: 60 kg N·hm^-2·a^-1;高氮: 90 kg N·hm^-2·a^-1)对两种经营强度(粗放经营和集约经营)毛竹林凋落叶生态化学计量特征的影响.结果表明: 相比于粗放经营,集约经营使毛竹凋落叶C、N、P含量分别显著提高9.3%、32.4%和22.7%, 而C∶N、C∶P和N∶P分别显著降低17.4%、54.3%和44.6%.粗放经营条件下,低、中氮沉降显著提高了毛竹凋落叶C、N、P含量,但显著降低了C∶N、C∶P和N∶P;高氮沉降显著提高了C、N含量及C∶P、N∶P,但显著降低了P含量.集约经营条件下,低氮沉降显著提高了毛竹凋落叶P含量,降低了C含量及C∶P、N∶P;中氮沉降显著提高了N、P含量,降低了C含量及C∶N、C∶P和N∶P;高氮沉降显著提高了C∶N、C∶P和N∶P,降低了P含量.经营方式和氮沉降的交互作用显著影响了凋落叶除C∶N以外的生态化学计量特征.毛竹凋落叶P与土壤P含量呈显著相关.     

Site-specific cleavage of the 40S ribosomal subunit reveals eukaryote-specific ribosomal protein S28 in the subunit head

After resolving the crystal structure of the prokaryotic ribosome, mapping the proteins in the eukaryotic ribosome is a challenging task. We applied RNase H digestion to split the human 40S ribosomal subunit into head and body parts. Mass spectrometry of the proteins in the 40S subunit head revealed the presence of eukaryote-specific ribosomal protein S28e. Recombinant S28e was capable of specific binding to the 3′ major domain of the 18S rRNA (K_a = 8.0 ± 0.5 × 10⁹ M⁻¹). We conclude that S28e has a binding site on the 18S rRNA within the 40S subunit head.

Structured summary

MINT-8044084: S8 (uniprotkb:P62241) and S19 (uniprotkb:P39019) colocalize (MI:0403) by cosedimentation through density gradient (MI:0029)MINT-8044095: S8 (uniprotkb:P62241), S19 (uniprotkb:P39019) and S13 (uniprotkb:P62277) colocalize (MI:0403) by cosedimentation through density gradient (MI:0029)MINT-8044024: S29 (uniprotkb:P62273), S28 (uniprotkb:P62857), S21 (uniprotkb:P63220), S20 (uniprotkb:P60866), S26 (uniprotkb:P62854), S25 (uniprotkb:P62851), S12 (uniprotkb:P25398), S17 (uniprotkb:P08708), S19 (uniprotkb:P39019), S14 (uniprotkb:P62263), S16 (uniprotkb:P62249) and S11 (uniprotkb:P62280) colocalize (MI:0403) by cosedimentation through density gradient (MI:0029)MINT-8044065: S29 (uniprotkb:P62273), S28 (uniprotkb:P62857), S19 (uniprotkb:P39019), S14 (uniprotkb:P62263) and S16 (uniprotkb:P62249) colocalize (MI:0403) by cosedimentation through density gradient (MI:0029)     

Proliferating cell nuclear antigen in the cytoplasm interacts with components of glycolysis and cancer

Proliferating cell nuclear antigen (PCNA) is involved in a wide range of functions in the nucleus. However, a substantial amount of PCNA is also present in the cytoplasm, although their function is unknown. Here we show, through Far-Western blotting and mass spectrometry, that PCNA is associated with several cytoplasmic oncoproteins, including elongation factor, malate dehydrogenase, and peptidyl-prolyl isomerase. Surprisingly, PCNA is also associated with six glycolytic enzymes that are involved in the regulation of steps 4-9 in the glycolysis pathway.

Structured summary

MINT-7995351: G3P (uniprotkb:P04406) and PCNA (uniprotkb:P12004) colocalize (MI:0403) by fluorescencemicroscopy (MI:0416)MINT-7995334: ENOA (uniprotkb:P06733) and PCNA (uniprotkb:P12004) colocalize (MI:0403) by fluorescencemicroscopy (MI:0416)MINT-7995368: ALDOA (uniprotkb:P04075) and PCNA (uniprotkb:P12004) colocalize (MI:0403) by fluorescencemicroscopy (MI:0416)MINT-7995141: G3P (uniprotkb:P04406) binds (MI:0407) to PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995182: ENOA (uniprotkb:P06733) binds (MI:0407) to PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995132: G3P (uniprotkb:P04406) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995228: PRDX6 (uniprotkb:P30041) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995220: CAH2 (uniprotkb:P00918) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995114: Triosephosphateisomerase (uniprotkb:P60174) binds (MI:0407) to PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995244: K2C7 (uniprotkb:P08729) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995252: ANXA2 (uniprotkb:P07355) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995122: Triosephosphateisomerase (uniprotkb:P60174) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995093: ALDOA (uniprotkb:P04075) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995148: PGK1 (uniprotkb:P00558) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995158: PGAM1 (uniprotkb:P18669) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995166: PGAM1 (uniprotkb:P18669) binds (MI:0407) to PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995105: ALDOA (uniprotkb:P04075) binds (MI:0407) to PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995260: PPIA (uniprotkb:P62937) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995173: ENOA (uniprotkb:P06733) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995268: EF1A (uniprotkb:P68104) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995236: MDHM (uniprotkb:P40926) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995189: RSSA (uniprotkb:P08865) physicallyinteracts (MI:0915) with PCNA (uniprotkb:P12004) by farwesternblotting (MI:0047)MINT-7995282: PCNA (uniprotkb:P12004) physicallyinteracts (MI:0915) with ALDOA (uniprotkb:P00883) and G3P (uniprotkb:P46406) by antibaitcoimmunoprecipitation (MI:0006).     

复合螺旋藻多糖对人结肠癌HT29细胞的抑制作用

研究复合螺旋藻多糖对人结肠癌HT29细胞的抑制作用。螺旋藻多糖（PSP）与银杏叶有效成分（GBE）1：1比例复合组、1：2比例复合组和2：1比例复合组对人结肠癌HT29细胞的抑瘤率,高剂量时分别比空白对照组提高68．04％（P〈0．01）、59．88％（P〈0．01）和58．82％（P〈0．01）;中剂量时分别比空白组提高47．52％（P〈0．01）、51．98％（P〈0．01）和40．31％（P〈0．01）;低剂量时分别比空白对照组提高39．70％（P〈0．01）、29．88％（P〈0．01）和27．31％（P〈0．01）。各复合制剂组的抑瘤率都高于相对应剂量的单一成分组,PSP与GBE联合使用对抑制人结肠癌HT29细胞能产生协同增效作用。     

生态系统演替过程中土壤与微生物碳氮磷化学计量关系的变化

土壤碳(C)、氮(N)、磷(P)化学计量特征会显著影响微生物的生长、群落结构、生物量C:N:P化学计量及其代谢活动。然而生态系统演替过程中土壤-微生物C:N:P化学计量的时间格局及其协调关系还不明确。为此, 该研究收集了2016年5月以前发表的文献中19个生态系统演替序列(包括13个森林、6个草地生态系统)的土壤-微生物生物量C:N:P研究结果, 整合分析了其中土壤-微生物生态化学计量的时间动态, 结果表明: (1)生态系统演替过程中土壤C:N没有一致的时间格局, 而土壤C:P和N:P均随演替进程显著增加, 其中土壤C:N:P与演替时间之间线性关系的斜率与相应演替序列的初始土壤有机C含量呈负相关关系。(2)演替进程中土壤-微生物生物量C:N:P没有一致的时间格局。(3)微生物生物量C占土壤有机C百分比(qMBC)、微生物生物量N占土壤全N百分比、微生物生物量P占土壤全P百分比均随着演替进程而显著增加, 即单位资源所能支持的微生物生物量随着演替进程而增加, 这与宏观生态系统演替理论相符。(4) qMBC随着土壤C:N、C:P和N:P以及C:N、C:P和N:P化学计量不平衡性(即土壤C:N、C:P和N:P分别除以微生物生物量C:N、C:P和N:P)的增加而减小; 其中, C:N、C:P和N:P化学计量不平衡性解释了qMBC变异性的37%-57%, 是演替时间解释率的7-17倍, 表明土壤-微生物生态化学计量关系对qMBC演替动态有重要影响。该研究强调了生态化学计量学理论和生态系统演替理论在土壤微生物时间动态研究中的重要作用, 表明适当地融合生态学宏观理论于土壤微生物研究可以加深对土壤-微生物生态过程的认识。     

Carbon,nitrogen and phosphorus net mineralization in organic horizons of temperate forests: stoichiometry and relations to organic matter quality

The rates of mineralization processes influence C sequestration and soil fertility, but despite their importance for ecosystem functioning, C, N and P net mineralization rates are seldom investigated together. Hence, we studied the relationships between net mineralization rates and organic matter stoichiometry in an 8-week incubation experiment with Oi, Oe and Oa horizon material of six beech, one spruce and one pine site. We determined C, N and P net mineralization rates, organic C quality and C:N:P stoichiometry. Net N mineralization only occurred below molar organic matter C:N ratios of 40 (Oi) or 28 (Oa) and N:P ratios of 42 (Oi) or 60 (Oa), and increased with decreasing C:N and N:P ratios. Net P mineralization only occurred below C:P ratios of 1400 (Oi) and N:P ratios of 40 (Oi), and increased with decreasing C:P and N:P ratios. Net N and P mineralization were strongly positively correlated with each other (r = 0.64, p < 0.001), whereas correlations of both net N and net P mineralization with C mineralization were weak. The average C:N:P stoichiometry of net mineralization was 620:4:1 (beech, Oi), 15,350:5:1 (coniferous, Oi), 1520:8:1 (Oe) and 2160:36:1 (Oa). On average, ratios of C:N net mineralization were higher, and ratios of N:P net mineralization lower than organic matter C:N and N:P ratios. This difference contributed to the decrease of C:N ratios and increase of N:P ratios from the Oi to the Oa horizons. In conclusion, the study shows that C, N and P net mineralization rates were closely correlated with the organic matter stoichiometry and that these correlations were modified by the degree of decomposition of the organic matter.     

Characterisation of the interaction of colicin A with its co-receptor TolA

Colicin A enters Escherichia coli cells through interaction with endogenous TolA and TolB proteins. In vitro, binding of the colicin A translocation domain to TolA leads to unfolding of TolA. Through NMR studies of the colicin A translocation domain and polypeptides representing the individual TolA and TolB binding epitopes of colicin A we question if the unfolding of TolA induced by colicin A is likely to be physiologically relevant. The NMR data further reveals that the colicin A binding site on TolA is different from that for colicin N which explains why there is a difference in colicin toxicity for E. coli carrying a TolA-III homologue from Yersina enterocolitica in place of its own TolA-III.

Structured summary

MINT-7888512: TolA (uniprotkb:P19934) and Col-A (uniprotkb:P04480) bind (MI:0407) by nuclear magnetic resonance (MI:0077)MINT-7888526: TolA (uniprotkb:P19934) and TolB (uniprotkb:P0A857) bind (MI:0407) by nuclear magnetic resonance (MI:0077)MINT-7888999: TolA (uniprotkb:P19934), TolB (uniprotkb:P0A855) and Col-A (uniprotkb:P04480) physically interact (MI:0915) by molecular sieving (MI:0071)MINT-7888982: TolA (uniprotkb:P19934), TolB (uniprotkb:P0A855) and Col-A (uniprotkb:P04480) physically interact (MI:0915) by nuclear magnetic resonance (MI:0077)     

S100 proteins regulate the interaction of Hsp90 with Cyclophilin 40 and FKBP52 through their tetratricopeptide repeats

S100 proteins are a subfamily of the EF-hand type calcium sensing proteins, the exact biological functions of which have not been clarified yet. In this work, we have identified Cyclophilin 40 (CyP40) and FKBP52 (called immunophilins) as novel targets of S100 proteins. These immunophilins contain a tetratricopeptide repeat (TPR) domain for Hsp90 binding. Using glutathione-S transferase pull-down assays and immunoprecipitation, we have demonstrated that S100A1 and S100A2 specifically interact with the TPR domains of FKBP52 and CyP40 in a Ca²⁺-dependent manner, and lead to inhibition of the CyP40-Hsp90 and FKBP52-Hsp90 interactions. These findings have suggested that the Ca²⁺/S100 proteins are TPR-targeting regulators of the immunophilins-Hsp90 complex formations.

Structured summary

MINT-7710442: FKBP52 (uniprotkb:Q02790) physically interacts (MI:0915) with S100A6 (uniprotkb:P06703) by competition binding (MI:0405)MINT-7710192: Cyp40 (uniprotkb:P26882) binds (MI:0407) to S100A1 (uniprotkb:P35467) by pull down (MI:0096)MINT-7710412: Cyp40 (uniprotkb:P26882) physically interacts (MI:0915) with S100A2 (uniprotkb:P29034) by competition binding (MI:0405)MINT-7710374: FKBP52 (uniprotkb:Q02790) binds (MI:0407) to S100A2 (uniprotkb:P29034) by pull down (MI:0096)MINT-7710452: Cyp40 (uniprotkb:P26882) physically interacts (MI:0914) with S100A2 (uniprotkb:P29034) and Hsp90 (uniprotkb:P07900) by anti tag coimmunoprecipitation (MI:0007)MINT-7710387: FKBP52 (uniprotkb:Q02790) binds (MI:0407) to S100A6 (uniprotkb:P06703) by pull down (MI:0096)MINT-7710279: FKBP52 (uniprotkb:Q02790) physically interacts (MI:0915) with S100A1 (uniprotkb:P35467) by competition binding (MI:0405)MINT-7710224: FKBP52 (uniprotkb:Q02790) binds (MI:0407) to Hsp90 (uniprotkb:P07900) by pull down (MI:0096)MINT-7710464: Cyp40 (uniprotkb:P26882) physically interacts (MI:0914) with S100A6 (uniprotkb:P06703) and Hsp90 (uniprotkb:P07900) by anti tag coimmunoprecipitation (MI:0007)MINT-7710249: Cyp40 (uniprotkb:P26882) binds (MI:0407) to Hsp90 (uniprotkb:P07900) by pull down (MI:0096)MINT-7710422: Cyp40 (uniprotkb:P26882) physically interacts (MI:0915) with S100A6 (uniprotkb:P06703) by competition binding (MI:0405)MINT-7710348: Cyp40 (uniprotkb:P26882) binds (MI:0407) to S100A2 (uniprotkb:P29034) by pull down (MI:0096)MINT-7710208: FKBP52 (uniprotkb:Q02790) binds (MI:0407) to S100A1 (uniprotkb:P35467) by pull down (MI:0096)MINT-7710265: Cyp40 (uniprotkb:P26882) physically interacts (MI:0915) with S100A1 (uniprotkb:P35467) by competition binding (MI:0405)MINT-7710361: Cyp40 (uniprotkb:P26882) binds (MI:0407) to S100A6 (uniprotkb:P06703) by pull down (MI:0096)MINT-7710476: FKBP52 (uniprotkb:Q02790) physically interacts (MI:0914) with S100A2 (uniprotkb:P29034) and Hsp90 (uniprotkb:P07900) by anti tag coimmunoprecipitation (MI:0007)MINT-7710316: FKBP52 (uniprotkb:Q02790) physically interacts (MI:0914) with S100A1 (uniprotkb:P35467) and Hsp90 (uniprotkb:P07900) by anti tag coimmunoprecipitation (MI:0007)MINT-7710432: FKBP52 (uniprotkb:Q02790) physically interacts (MI:0915) with S100A2 (uniprotkb:P29034) by competition binding (MI:0405)MINT-7710488: FKBP52 (uniprotkb:Q02790) physically interacts (MI:0914) with S100A6 (uniprotkb:P06703) and Hsp90 (uniprotkb:P07900) by anti tag coimmunoprecipitation (MI:0007)MINT-7710329: S100A6 (uniprotkb:P14069) physically interacts (MI:0914) with FKBP52 (uniprotkb:P30416) and Cyp40 (uniprotkb:Q08752) by anti bait coimmunoprecipitation (MI:0006)MINT-7710295: Cyp40 (uniprotkb:P26882) physically interacts (MI:0914) with Hsp90 (uniprotkb:P07900) and S100A1 (uniprotkb:P35467) by anti tag coimmunoprecipitation (MI:0007)     

Physiological changes in androgen plasma levels with elapsing of time from castration in adult male rats

In the present study we investigated in adult male rats the effects of castration on Dehydroepiandrosterone (DHEA), Androstenedione (delta 4), Testosterone (T) and Dihydrotestosterone (DHT) plasma levels: five days (group II), seven weeks (group III) and eleven weeks (group IV) after orchiectomy. The same hormone assays were performed in rats approximately 60 days of age which underwent a sham-operation for orchiectomy (group I). Our data show that five days following orchiectomy (group II) delta 4, T and DHT were decreased with respect to sham-operated rats. (Group I: delta 4: 83.3 +/- 14.9 (SEM) ng/dl (n = 12); T: 435.32 +/- 51.45 (n = 12); DHT: 51.47 +/- 6.54 (n = 12); Group II: delta 4: 44.81 +/- 6.09 (n = 12) P = 0.05; T: 25.54 +/- 2.88 (n = 12) P less than 0.01; DHT: 12.9 +/- 2.51 (n = 12) P less than 0.01). Seven weeks afterwards T and DHT remained significantly lower (group III: T: 54.37 +/- 12.21, n = 16) (P less than 0.01; DHT: 33.22 +/- 4.49 (n = 16) P less than 0.01) while eleven weeks after all steroids were significantly decreased with respect to the values observed in sham-operated rats. (Group IV) delta 4: 32.01 +/- 5.7 (n = 10) P less than 0.01: T: 27.29 +/- 7.05 (n = 10) P less than 0.01; DHT: 29.03: 5.34 (n = 10) P less than 0.01).(ABSTRACT TRUNCATED AT 250 WORDS)     

Persistence of Escherichia coli O157:H7 in barley silage: effect of a bacterial inoculant

AIMS: The effect of a lactic acid producing bacterial (LAB) inoculant on the elimination of Escherichia coli O157:H7 from barley forage was assessed. METHODS AND RESULTS: Triplicate mini-silos were prepared for four treatments and six sampling times (1, 3, 7, 15, 30 and 42 d post-ensiling). The treatments were (i) 10(5) cfu g(-1) Pediococcus pentosaceus and Propionibacterium jenzenii (P2); (ii) 10(5) cfu g(-1) E. coli O157:H7 strain 3081 and 10(5) cfu g(-1) E. coli Biotype 1 strains 719IE10, 719IE14 and 614ME49 (EC); (iii) P2 + EC; and (iv) the control (sterile distilled water). Triplicate mini-silos were opened at each sampling time for pH, volatile fatty acid (VFA) and lactate determinations and E. coli, E. coli O157:H7 and LAB were enumerated. On d 3 and 7, numbers of E. coli O157:H7 in P2 + EC were significantly lower than in EC (P < 0;05). Escherichia coli O157:H7 was not detected in P2 + EC and EC at 7 and 15 d post-ensiling, respectively. On d 15 through 42, E. coli Biotype 1 was not detected in P2 + EC or EC. Populations of LAB were higher in P2 and P2 + EC than in the control and EC on d 3 and 7 (P < 0.05). After 3 d of ensiling, lactate levels were higher (P < 0.05) and pH was lower (P < 0.05) in P2 and P2 + EC as compared to the control and EC. Bacteriocins of P2 were not found to be inhibitory to E. coli O157:H7 using the agar-spot procedure. Escherichia coli O157:H7 inoculated into the control silage at a level of 10(3) cfu g(-1) and exposed to aerobic conditions at 22 degrees C was not detected after 1 d and remained undetectable for the 28 d exposure period. CONCLUSIONS: Silage inoculant P2 increased lactate levels and decreased pH more rapidly during ensiling, which appeared to hasten the elimination of E. coli O157:H7 from the silage. SIGNIFICANCE AND IMPACT OF THE STUDY: Results emphasize the importance of adequate ensiling since E. coli O157:H7 may be maintained and spread among cattle through feed.     

Variations in leaf and root stoichiometry of Nitraria tangutorum along aridity gradients in the Hexi Corridor,northwest China

Nitrogen (N) and phosphorus (P) concentrations and N: P ratios between leaves and roots of Nitraria tangutorum along aridity gradients were studied. N. tangutorum was relatively limited by N in April (mean leaf N: P ratio = 11.13) and by P in August (mean leaf N: P ratio = 38.78). N and P in both leaves and roots were highly correlated across sampling sites. In April both leaf and root N and P concentrations increased along aridity gradients. Mean leaf N: P ratios changed slightly, but mean root N: P ratios increased with increasing aridity gradients. We suggest that leaf N: P ratios can indicate nutrient status at different plant growth stages, and root N: P ratios can signify if the amount of soil nutrients is insufficient.     

Changes of the relationships between soil and microbes in carbon,nitrogen and phosphorus stoichiometry during ecosystem succession

AimsThe carbon (C), nitrogen (N) and phosphorus (P) stoichiometry (C:N:P) of soil profoundly influences the growth, community structure, biomass C:N:P stoichiometry, and metabolism in microbes. However, the relationships between soil and microbes in the C:N:P stoichiometry and their temporal dynamics during ecosystem succession are poorly understood. The aim of this study was to determine the temporal patterns of soil and microbial C:N:P stoichiometry and their relationships during ecosystem succession.MethodsAn extensive literature search was conducted and data were compiled for 19 age sequences of successional ecosystems, including 13 forest ecosystems and 6 grassland ecosystems, from 18 studies published up to May 2016. Meta-analyses were performed to examine the sequential changes in 18 variables that were associated with soil and microbial C, N and P contents and the stoichiometry. Important findings (1) There was no consistent temporal pattern in soil C:N along the successional stages, whereas the soil C:P and N:P increased with succession; the slopes of the linear relationships between soil C:N:P stoichiometry and successional age were negatively correlated with the initial content of the soil organic C within given chronosequence. (2) There was no consistent temporal pattern in microbial C:N:P stoichiometry along the successional stages. (3) The fraction of microbial biomass C in soil organic C (qMBC), the fraction of microbial biomass N in soil total N, and the fraction of microbial biomass P in soil total P all increased significantly with succession, in consistency with the theory of succession that ecosystem biomass per unit resource increases with succession. (4) The qMBC decreased with increases in the values of soil C:N, C:P, or N:P, as well as the stoichiometric imbalances in C:N, C:P, and N:P between soil and microbes (i.e., ratios of soil C:N, C:P, and N:P to microbial biomass C:N, C:P, and N:P, respectively). The C:N, C:P, and N:P stoichiometric imbalances explained 37%-57% variations in the qMBC, about 7-17 times more than that explainable by the successional age, illustrating the importance of soil-microbial C:N:P stoichiometry in shaping the successional dynamics in qMBC. In summary, our study highlights the importance of the theories of ecosystem succession and stoichiometry in soil microbial studies, and suggests that appropriately applying macro-ecological theories in microbial studies may improve our understanding on microbial ecological processes.     

Intestinal enterobacteria of the hibernating Apis mellifera mellifera L. bees

Dynamics of enterobacteria of normal intestinal microflora was studied in Apis mellifera mellifera L. bees hibernating under snow in the Western Urals. The cell numbers (N) of the predominant species Klebsiella oxytoca increased from 10-10(6) CFU/bee in November 2004 to 10(4)-10(7) CFU/bee in March 2005; its frequency of occurrence (P) increased from 92 to 100%. Increase of Providencia rettgeri (11.2004: N up to 10(6), P 25%; 03.2005: N 10(2)-10(6), P 80%) was accompanied by the substitution of Morganella morganii (11.2004: N up to 10(6), P 25%) with Proteus vulgaris (03.2005: N up to 10(5), P 8%). By spring, Hafnia alvei and Citrobacter sp., which are pathogenic to bees, disappeared (11.2004: N up to 10(5), P 13 and 10%, respectively). Endophytic species Pantoea agglomerans, Leclecria sp., and other representatives of the "Enterobacter agglomerans" group were present in November and after the first emergence in spring (N up to 10(5); November: P 15%; April: P 23%). In April, the number of enterobacteria decreased to 10(5), and P. rettgeri became the predominant species (P 54%) instead of K. oxytoca (P 43%).