不同林龄橡胶(Hevea brasiliensis)林土壤微生物群落和磷组分的变化

橡胶林是我国热带地区重要的经济林,而土壤磷是热带地区植物生长的重要限制因子之一,理解土壤磷转化机理对于生态系统的磷管理和可持续发展具有重要意义。因此,以热带地区海南儋州不同林龄(4、15、31a)橡胶人工林为研究对象,采用Hedley连续浸提法研究了土壤磷组分,磷脂脂肪酸法(Phospholipid fatty acids,PLFAs)分析了土壤微生物群落。结果表明,在橡胶林内各磷组分的相对含量大小顺序为:闭蓄态磷中等活性态磷活性态磷团聚体内磷钙磷。随着林龄的增加,橡胶林土壤中的磷组分发生显著变化。4、15、31a橡胶林的闭蓄态磷分别占总提取磷的52.61%、47.17%和34.91%,而活性态磷分别占总提取磷的6.67%、11.32%、13.68%。土壤总微生物、细菌、革兰氏阴性菌(G~-)、革兰氏阳性菌(G~+)的PLFAs含量均表现为15a4a31a,而31a橡胶林放线菌、真菌(F)和丛枝菌根真菌(AMF)的PLFAs含量均低于4a和15a。冗余分析(RDA)显示,全氮、有机碳、p H、F、AMF、G~-、G~+是引起不同林龄橡胶林土壤磷组分变化的重要贡献因子。研究表明,在橡胶林发育过程中,土壤理化性质和微生物群落发生了明显的变化,进而影响到土壤磷的转化过程。     

Impact of microorganisms,humidity, and temperature on the enantioselective degradation of imazethapyr in two soils

Imazethapyr (IM) is a chiral herbicide composed of an (−)‐R‐enantiomer and an (+)‐S‐enantiomer with differential herbicidal activity. In this study, the effects of microbial organisms, humidity, and temperature on the selective degradation of the (−)‐R‐ and (+)‐S‐enantiomers of IM were determined in silty loam (SL) and clay loam (CL) soil with different pH values. The (−)‐R‐enantiomer of IM was preferentially degraded in two soils under different microorganism, humidity, and temperature conditions. The average half‐lives of R‐IM ranged from 43 to 66.1 days and were significantly shorter (P <  0.05) than those of S‐IM, which ranged from 51.4 to 79.8 days. The enantiomer fraction (EF = (+)‐S‐enantiomer/((−)‐R‐enantiomer + (+)‐S‐enantiomer)) values were used to describe the enantioselectivity of degradation of IM were >0.5 (P <  0.05) in two unsterilized soils under different humidity and temperature conditions. The highest EF values were observed at unsterilized CL soil samples under 50% maximum water‐holding capacity (MWHC) and 25 °C environmental conditions. The EF values of the IM enantiomers were significantly higher (P <  0.05) in CL soils (higher pH = 5.81) and were 0.581 (unsterilized) and 0.575 (50% MWHC; 25 °C) compared with those recorded in SL soil (lower pH = 4.85). In addition, this study revealed that microbial organisms preferentially utilized the more herbicidal active IM enantiomer.     

An improved procedure of mapping a quantitative trait locus via the EM algorithm using posterior probabilities

Mapping a locus controlling a quantitative genetic trait (e.g. blood pressure) to a specific genomic region is of considerable contemporary interest. Data on the quantitative trait under consideration and several codominant genetic markers with known genomic locations are collected from members of families and statistically analysed to estimate the recombination fraction, θ, between the putative quantitative trait locus and a genetic marker. One of the major complications in estimating θ for a quantitative trait in humans is the lack of haplotype information on members of families. We have devised a computationally simple two-stage method of estimation of θ in the absence of haplotypic information using the expectation-maximization (EM) algorithm. In the first stage, parameters of the quantitative trait locus (QTL) are estimated on the basis of data of a sample of unrelated individuals and a Bayes’s rule is used to classify each parent into a QTL genotypic class. In the second stage, we have proposed an EM algorithm for obtaining the maximum-likelihood estimate of θ based on data of informative families (which are identified upon inferring parental QTL genotypes performed in the first stage). The purpose of this paper is to investigate whether, instead of using genotypically ‘classified’ data of parents, the use of posterior probabilities of QT genotypes of parents at the second stage yields better estimators. We show, using simulated data, that the proposed procedure using posterior probabilities is statistically more efficient than our earlier classification procedure, although it is computationally heavier.     

Long-term patterns of mass loss during the decomposition of leaf and fine root litter: an intersite comparison

Decomposition is a critical process in global carbon cycling. During decomposition, leaf and fine root litter may undergo a later, relatively slow phase; past long-term experiments indicate this phase occurs, but whether it is a general phenomenon has not been examined. Data from Long-term Intersite Decomposition Experiment Team, representing 27 sites and nine litter types (for a total of 234 cases) was used to test the frequency of this later, slow phase of decomposition. Litter mass remaining after up to 10 years of decomposition was fit to models that included (dual exponential and asymptotic) or excluded (single exponential) a slow phase. The resultant regression equations were evaluated for goodness of fit as well as biological realism. Regression analysis indicated that while the dual exponential and asymptotic models statistically and biologically fit more of the litter type–site combinations than the single exponential model, the latter was biologically reasonable for 27–65% of the cases depending on the test used. This implies that a slow phase is common, but not universal. Moreover, estimates of the decomposition rate of the slowly decomposing component averaged 0.139–0.221 year⁻¹ (depending on method), higher than generally observed for mineral soil organic matter, but one-third of the faster phase of litter decomposition. Thus, this material may be slower than the earlier phases of litter decomposition, but not as slow as mineral soil organic matter. Comparison of the long-term integrated decomposition rate (which included all phases of decomposition) to that for the first year of decomposition indicated the former was on average 75% that of the latter, consistent with the presence of a slow phase of decomposition. These results indicate that the global store of litter estimated using short-term decomposition rates would be underestimated by at least one-third.     

Comparative analysis of the secretory proteome of human adipose stromal vascular fraction cells during adipogenesis

Adipogenesis is a complex process that is accompanied by a number of molecular events. In this study, a proteomic approach was adopted to identify secretory factors associated with adipogenesis. A label‐free shotgun proteomic strategy was implemented to analyze proteins secreted by human adipose stromal vascular fraction cells and differentiated adipocytes. A total of 474 proteins were finally identified and classified according to quantitative changes and statistical significances. Briefly, 177 proteins were significantly upregulated during adipogenesis (Class I), whereas 60 proteins were significantly downregulated (Class II). Changes in the expressions of several proteins were confirmed by quantitative RT‐PCR and immunoblotting. One obvious finding based on proteomic data was that the amounts of several extracellular modulators of Wnt and transforming growth factor‐β (TGF‐β) signaling changed during adipogenesis. The expressions of secreted frizzled‐related proteins, dickkopf‐related proteins, and latent TGF‐β‐binding proteins were found to be altered during adipogenesis, which suggests that they participate in the fine regulation of Wnt and TGF‐β signaling. This study provides useful tools and important clues regarding the roles of secretory factors during adipogenic differentiation, and provides information related to obesity and obesity‐related metabolic diseases.     

Maximum yields of microsomal-type membranes from small amounts of plant material without requiring ultracentrifugation

Isolation of a microsomal membrane fraction is a common procedure in studies involving membrane proteins. By conventional definition, microsomal membranes are collected by centrifugation of a postmitochondrial fraction at 100,000g in an ultracentrifuge, a method originally developed for large amounts of mammalian tissue. We present a method for isolating microsomal-type membranes from small amounts of Arabidopsis thaliana plant material that does not rely on ultracentrifugation but instead uses the lower relative centrifugal force (21,000g) of a microcentrifuge. We show that the 21,000g pellet is equivalent to that obtained at 100,000g and that it contains all of the membrane fractions expected in a conventional microsomal fraction. Our method incorporates specific manipulation of sample density throughout the procedure, with minimal preclearance, minimal volumes of extraction buffer, and minimal sedimentation pathlength. These features allow maximal membrane yields, enabling membrane isolation from limited amounts of material. We further demonstrate that conventional ultracentrifuge-based protocols give submaximal yields due to losses during early stages of the procedure; that is, extensive amounts of microsomal-type membranes can sediment prematurely during the typical preclearance steps. Our protocol avoids such losses, thereby ensuring maximal yield and a representative total membrane fraction. The principles of our method can be adapted for nonplant material.     

油菜秸秆还田对水稻根系、分蘖和产量的影响

采用田间试验与栽培模拟试验相结合的方法,分析了油菜秸秆还田对水稻根系、分蘖和产量的影响.结果表明: 水稻移栽后0～36 d,与秸秆不还田处理相比,油菜秸秆还田处理下水稻分蘖减少1～2个,根系单株伤流量降低1.0～8.6 mg,根系谷氨酰胺合成酶(GS)、谷丙转氨酶(GPT)和谷草转氨酶(GOT) 活性分别降低0.10～6.11、0.06～0.31和0.52～0.84 μmol·g^-1·h^-1. 水稻移栽后56 d,与秸秆不还田处理相比,油菜秸秆翻埋还田处理下水稻根系单株伤流量增加3.4～11.7 mg,根系GS、GPT和GOT活性分别增加0.34～0.78、0.13～0.45和0.18～0.20 μmol·g^-1·h^-1;油菜秸秆覆盖还田处理下水稻根系单株伤流量降低19～25 mg,根系GS、GPT和GOT活性分别增加0.16～0.34、0.08～0.21和0.06～0.32 μmol·g^-1·h^-1.油菜秸秆还田处理中,全量还田处理下的水稻产量最高,其中,与全量覆盖还田相比,全量翻埋还田处理下的水稻产量增加0.13～0.48 t·hm^-2.可见,油菜秸秆还田会导致水稻生长前期根系活力下降、氮代谢酶活性降低,从而使水稻根系生长缓慢、返青延迟,但在中后期,随着根系活力和氮代谢酶活性的增强,秸秆还田会促进水稻根系生长;油菜秸秆还田对水稻产量的影响是多因素综合作用的结果,全量翻埋还田更适宜于四川油稻两熟轮作系统.     

Urea decomposing activity of fractionated brackish phytoplankton in Lake Nakaumi

The influence of brackish phytoplankton cell classes upon the response of urea decomposition was investigated in Lake Nakaumi. The urea decomposition rate was 5 to 350 μmol urea m⁻³ h⁻¹ in the light and 3 to 137 μmol urea m⁻³ h⁻¹ in the dark. The urea decomposition rates in the light were obviously higher than in the dark. An extremely high rate (350 μmol urea m⁻³ h⁻¹) was observed in Yonago Bay. The rate in the smaller fraction (<5 μm) exceeded that in the middle (5–25 μm) and larger fractions (>25 μm). The chlorophyll- and photosynthesis-specific rates for urea decomposition in the light were 0.5 to 3.9 μmol urea mg chl.a ⁻¹ h⁻¹ and 0.3 to 1.3 μmol urea mg photo.C⁻¹. The specific urea decomposing activities were higher in the smaller fraction than in the other two fractions. The present results suggest that in brackish waters urea decomposition occurred with coupling to the standing crop and photosynthetic activity of phytoplankton. Received: May 22, 1999 / Accepted: August 15, 1999     

典型黑土区不同生态系统土壤团聚体有机碳分布特征

基于团聚体分组和闭蓄态微团聚体分离技术,利用典型黑土区27年长期定位试验,研究草地生态系统、农田生态系统和裸地生态系统下土壤团聚体及团聚体内部组分中有机碳的分布,以解析不同生态系统下土壤团聚体和有机碳固持间的关系,揭示黑土有机碳的物理稳定性机制。结果显示:与农田相比,草地土壤有机碳含量显著提高7.6%;裸地土壤有机碳含量显著下降14.1%。草地促进了大团聚体(250μm),尤其2000μm团聚体的形成,提高了土壤团聚体的稳定性;裸地则降低了土壤的团聚化程度及稳定性,大团聚体和微团聚体含量下降,粉粘粒含量相应增加。草地大团聚体中有机碳含量显著高于农田,且内部各组分有机碳含量均有显著提高,其中粗颗粒有机质、闭蓄态微团聚体和粉黏粒有机碳含量增幅分别为600%、54%和65%;裸地增加了粉粘粒结合有机碳含量,降低了大团聚体和微团聚体中有机碳含量,且大团聚体和微团聚体内部各组分有机碳含量均有所下降。3种生态系统类型土壤均以总粉粘粒结合有机碳为主,占土壤总有机碳52%—79%,其作为惰性碳库是黑土有机碳的重要组成部分。黑土有机碳的累积或损失主要表现为活性较强的有机碳库-团聚体中颗粒有机质的增加或减少,与农田相比,草地土壤有机碳的累积主要归因于大团聚体中粗颗粒有机质的增加,为总有机碳增量的3倍;裸地土壤有机碳的损失主要归因于微团聚体中总细颗粒有机质的减少,对总有机碳损失的贡献率为60%。     

Climate warming alters subsoil but not topsoil carbon dynamics in alpine grassland

Subsoil contains more than half of soil organic carbon (SOC) globally and is conventionally assumed to be relatively unresponsive to warming compared to the topsoil. Here, we show substantial changes in carbon allocation and dynamics of the subsoil but not topsoil in the Qinghai‐Tibetan alpine grasslands over 5 years of warming. Specifically, warming enhanced the accumulation of newly synthesized (¹⁴C‐enriched) carbon in the subsoil slow‐cycling pool (silt‐clay fraction) but promoted the decomposition of plant‐derived lignin in the fast‐cycling pool (macroaggregates). These changes mirrored an accumulation of lipids and sugars at the expense of lignin in the warmed bulk subsoil, likely associated with shortened soil freezing period and a deepening root system. As warming is accompanied by deepening roots in a wide range of ecosystems, root‐driven accrual of slow‐cycling pool may represent an important and overlooked mechanism for a potential long‐term carbon sink at depth. Moreover, given the contrasting sensitivity of SOC dynamics at varied depths, warming studies focusing only on surface soils may vastly misrepresent shifts in ecosystem carbon storage under climate change.