长江源区高寒草原和高寒草甸土壤粒径分布特征

为探究长江源区主要下垫面土壤空间异质性与粒径分布(PSD)非均匀性,运用分形理论描述高寒草原和高寒草甸2种下垫面土壤粒径分布特征,分析了2种下垫面土壤的分形维数特征差异及其与土壤颗粒组成的关系。结果表明: 研究区土壤颗粒粒径主要分布于100～800 μm,高寒草原土壤单重分形维数(D_V)为2.429～2.508,高寒草甸土壤D_V为2.697～2.743,高寒草原土壤质地偏粗,高寒草甸土壤质地偏细。土壤在20～30 cm深度质地最细,在0～10 cm层质地最粗糙;多重分形维数(容量维数D₀、信息熵维数D₁、关联维数D₂)均以高寒草原(0.896～0.961、0.828～0.887、0.725～0.819)高于高寒草甸(0.890～0.914、0.693～0.744、0.540～0.603),与高寒草甸相比,高寒草原土壤粒径分布范围更宽,土壤整体构造更复杂,土壤整体非均匀性更高。D_V与土壤黏粒、粉粒含量呈显著正相关,与砂粒含量呈显著负相关;D₁、D₂与黏粒、粉粒含量呈显著负相关,与砂粒含量呈显著正相关。土壤砂粒含量是土壤PSD非均匀分布及分形维数大小变化的主要因素。     

氮源对C.vulgaris油脂积累的影响

实验室条件下,考察了在发酵过程中不同氮源对小球藻的生物量和油脂积累的影响,确定了小球藻的最佳氮源;并对比分析了含氮培养与缺氮培养的生物量、油脂含量、氮消耗量、生物量氮消耗比率和油脂氮消耗比率的不同。结果表明:小球藻在1.6 g/L Na NO3时获得最大生物量,为562.2 mg/L,在0.8 g/L Na NO3时获得最大相对油脂含量为12.01%;以油脂含量为考察指标时,培养小球藻的最佳氮源为0.8 g/L Na NO3;缺氮培养时,最大油脂含量为13.49%,比含氮培养高约15%;含氮培养时,最高生物量为626.3 mg/L,比缺氮培养高约1.9倍。氮源对生物量,相对油脂含量,生物量氮消耗比率和油脂氮消耗比率具有明显的影响。藉此,提出了通过改变培养方式,达到调控小球藻细胞内生理代谢组分的可行性。     

模拟降雨减少对马尾松人工林凋落物量及其化学性质的短期影响

为研究气候变化背景下降水格局变化对森林生长和碳固持的影响,2012年在我国南亚热带地区选择广泛分布的马尾松(Pinus massoniana)人工林为研究对象,分别设置3块20 m×20 m的模拟降雨减少50%和对照样地,每个样地随机设置5个距地面40 cm的1 m×1 m的凋落物收集框,2016年1—12月每隔1月收集各样地林冠层凋落物,比较研究减水处理对凋落物组分产量和基本化学性质的短期影响。结果表明:马尾松人工林针叶凋落物量及其所占比例显著高于其他凋落物组分(P0.05),减雨处理对马尾松人工林凋落叶和总量无显著影响(P0.05)。与对照相比,减雨处理分别增加凋落针叶含碳量和凋落果含氮量27.4 g/kg和5.1 g/kg,以及凋落针叶的木质素含量、阔叶纤维素含量和皮半纤维素含量3.9%、5.2%和4.0%(P0.05),但显著降低凋落皮碳、纤维素含量和凋落果的碳氮比(P0.05)。凋落物N、P含量具有协同性,含碳量与木质素含量显著正相关(P0.05)。模拟降雨减少处理初期并未显著改变南亚热带马尾松人工林总凋落物量,但增加了凋落针叶的木质素含量和含碳量。本研究预示短期穿透雨减少可能降低南亚热带马尾松人工林凋落物的分解能力,由此降低马尾松人工林土壤中凋落物源性碳的输入量。     

油茶蒲提取物抑制前列腺增生活性化合物的分离与鉴定

为了探究油茶蒲提取物中对前列腺增生具有抑制作用的天然活性化合物,本研究采用高效制备液相(preparative HPLC)从油茶蒲聚酰胺组分中分离得到抑制前列腺增生(benign prostatic hyperplasia,BPH)的活性化合物。运用质谱(Mass Spectrometer,MS)和核磁共振技术(Nuclear magnetic resonance,NMR)对其化学结构进行鉴定,并采用MTT法检测各化合物对人前列腺增生细胞BPH-1增殖的抑制作用。结果表明:纯化组分F1、F2和F3对BPH-1细胞增殖均具有较强抑制作用,低剂量(50μg/m L)时抑制率分别为30.31%、43.26%和29.00%,抑制效果均优于阳性对照非那雄胺(26.50%)。经化学结构鉴定确定F1、F2和F3分别为橡椀酸双内酯、3-O-没食子酰基-4,6-[(S)-六羟基联苯二酰基]-(α/β)-D-吡喃葡萄糖和3,4,6-三-O-没食子酰基-(α/β)-D-葡萄糖。本研究可为开发改善前列腺疾病的天然产物提供理论参考与物质基础。     

植物的叶表蜡层与昆虫的行为

在高等植物的叶表角质膜外覆盖着一层蜡质薄层。这一薄层由表皮细胞的分泌物沉积而成,被称为上表皮蜡层(epicuticular wax)或蜡被(waxcoating)。叶表蜡层是多种化合物的混合物,其组分复杂多样,有种的差异。但是脂肪族的蜡质成分却广泛地存在于植物界。蜡层的含量也因种属的不同有很大的差异。许多草本植物(如莴苣,菠菜、甜菜)的叶表蜡层仅为5～10μg/cm~2,而有些果类作物(如桃、梨、苹果)的叶表蜡层可达60～300μg/cm~2。叶表蜡层在维持植物体内水平衡、减少机械损伤、抵御霉菌病     

川西高海拔增温和加氮对红杉凋落物有机组分释放的影响

对川西高山树线红杉新鲜凋落物中有机组分于11月进行自然条件(对照)、加氮(2 g N·m^-2)、增温(顶开式培养室)、加氮+增温4个处理的原位培养,并监测凋落物中有机组分的分解动态.结果表明: 在试验开始后4个月内,增温、加氮以及加氮+增温处理比对照显著促进了红杉凋落物中水溶性糖、水溶性酚和多酚的分解,但随着培养时间的延长,累积分解量的差异逐渐缩小.与对照相比,增温、加氮和增温+加氮处理均抑制红杉凋落物中CH₂Cl₂提取组分、酸溶碳水化合物、酸溶木质素和非酸溶木质素分解,其中增温处理抑制作用最强,加氮处理抑制效果最弱,增温+加氮处理介于二者之间;增温处理对非酸溶木质素和CH₂Cl₂提取组分的半分解周期延长1倍以上,热水溶组分的半分解周期延长50%以上.在原位培养条件下,红杉新鲜凋落物中水溶性糖、水溶性酚、多酚、酸溶碳水化合物、酸溶木质素是较容易分解的有机组分,半分解周期分别为182、159、127、154和190 d;热水溶组分、CH₂Cl₂提取组分和非酸溶木质素是较难分解的有机组分,半分解周期分别是209、302和318 d;尽管低温季节(11月至次年3月)极其寒冷,气温均低于0 ℃,常被认为是微生物活性最弱、有机物分解最慢的时期,但结果显示低温季节期间红杉凋落物各有机组分却分解最快.因此,氮沉降和升温将迟滞该区域高寒红杉林凋落物的分解.这将有利于高寒森林生态系统的土壤碳固持.     

北山羊角化学成分解析

本文以北山羊角为主要研究对象,利用傅里叶变换红外光谱仪、气相色谱仪和全自动氨基酸分析仪检测分析其红外光谱、脂肪酸和氨基酸成分。结果表明:北山羊角红外光谱主要体现角蛋白组分的特征峰,其中1 540 cm~(-1)、1 653 cm~(-1)、3 061cm~(-1)归属于角蛋白分子中酰胺类成分;1 454 cm~(-1)、2 875 cm~(-1)、2 963 cm~(-1)归属于角蛋白分子中脂类成分;北山羊角共检测出10种脂肪酸组分,主要成分包括棕榈酸、油酸、山俞酸,它们占脂肪酸总量的53.9%;17种氨基酸组分,总量为976.62 mg/g。     

氮添加对川西高寒灌丛凋落枝化学计量特征及养分归还的影响

氮(N)是陆地生态系统初级生产力的重要限制因子,大气N沉降的增加将会对植物的化学元素含量和生物量产生重要影响,进而影响凋落物的化学计量特征及其养分归还。高寒灌丛是陆地生态系统的重要组成部分,但有关N沉降对高寒灌丛凋落物尤其是凋落枝的化学元素和生物量的研究还较为缺乏,难以深入揭示N沉降对高寒灌丛土壤碳(C)和养分循环的影响机理。基于此,以青藏高原东部地区的优势高寒灌丛类型—窄叶鲜卑花(Sibiraea angustata(Rehd.) Hand.-Mazz.)灌丛为研究对象,连续4年人工模拟N沉降,分析了凋落枝C、N、磷(P)、木质素和纤维素化学计量特征及其归还量对不同N添加浓度(0、20、50、100 kg hm^-2 a^-1)的响应趋势。结果表明：(1)N添加对凋落枝C、N含量无显著性影响(P>0.05),而对P、木质素和纤维素含量有显著性影响(P<0.05),但不同年份间的影响趋势不一致;(2)4年的N添加并未改变凋落枝的C/N、N/P,但显著降低了凋落枝的木质素/N(第3年)、C/P(第1年和第4年)和C/N/P(第1年);(...     

施磷对川西北高寒草地土壤磷形态及有效性的影响

以川西北高寒草地为研究对象,采用随机区组设计,设置0、10、20、30、40、50、60 g/m²的过磷酸钙(P₂O₅,16%)施肥试验,分析土壤不同形态磷含量和有效磷(Olsen-P)含量变化特征,探究施磷对川西北高寒草地土壤磷形态及有效磷的影响。结果表明：(1)随施磷量增加,土壤总磷(TP)含量先增加后趋于平稳而Olsen-P含量减少。高水平(50、60 g/m²)施磷下氢氧化钠有机磷(NaOH-Po)及残留磷(Residual-P)是高寒草地主要的磷素累积形态,其含量显著高于不施磷处理;(2)树脂交换态磷(Resin-Pi)、碳酸氢钠无机磷(NaHCO₃-Pi)、碳酸氢钠有机磷(NaHCO₃-Po)和氢氧化钠无机磷(NaOH-Pi)含量随施磷量增加整体呈先增加后降低趋势,表层土壤30 g/m²磷肥用量下其值均为最高,分别为21.54、22.94、65.86、64.48 mg/kg。酸溶性无机磷(HCl-Pi)随施磷量增加整体呈下...     

一株南海红树林底泥抗真菌放线菌(No.H74-18)的化学成分研究

对我国南海红树林底泥中分离的一株放线菌(No.H74-18)的发酵菌丝体采用95%乙醇提取,并对具有抗真菌活性的乙酸乙酯部位进行研究,通过硅胶开放柱色谱分离得到了一个结晶样品。通过制备型反相高效液相色谱分离,从此结晶样品中分离纯化出3个化合物,经NMR、MS等光谱学方法分别鉴定为抗霉素A1(1)、抗霉素A2a(2)、抗霉素A3(3),这些化合物都是抗霉素类化合物。采用LC-MS联用技术分析了此结晶样品中存在的抗霉素类的可能组份。     

Mechanical resistance by an ectorganic soil layer on root development of seedling Pinus sylvestris

We investigated early root development of Pinus sylvestris seedlings in relation to bulk density and natural particle layering in an ectorganic soil layer from a bracken (Pteridium aquilinum) stand. Responses in root development to two levels of bulk density (0.07 and 0.15 g/cm³) in mixed bracken substrate were compared with effects in peat of similar bulk densities, and in sand of three different bulk densities (0.37, 0.52, and 0.67 g/cm³). The effect on root growth of the natural horizontal layering of the organic particles was examined by comparing intact with mixed ectorganic bracken soil profiles of similar bulk densities (resp. 0.09 and 0.07 g/cm³).Root length growth was significantly reduced in the organic and sandy substrates of high bulk density. Root diameter was not affected by bulk density in the organic substrate, but increased with higher bulk density in sand. Preservation of horizontal layering in the intact ectorganic profile significantly reduced root length compared with mixed substrate of similar bulk density.Roots growing in high bulk density, and intact, organic substrate showed increased twisting, which resulted in a smaller depth reached by the root relative to total root length produced. In sand, root twisting did not change with increased bulk density. It is suggested that roots growing through organic substrate follow a path of least resistance. This implies that organic particle size and orientation are more important in determining root development than bulk density.This study points out that the natural layering of organic particles presents another constraint on the establishment of plant species in sites with a well-developed ectorganic soil layer. Disturbance of this layer may therefore enhance establishment of seedlings by reducing the mechanical resistance of the ectorganic soil profile to developing seedling roots.     

An analysis of the bovine genome by Cs2SO4-Ag density gradient centrifugation

Calf DNA preparations having molecular weights of 5 to 7 × 10⁶ have been fractionated by preparative Cs₂SO₄—Ag⁺ density gradient centrifugation into a number of components. These may be divided into three groups: (1) the main DNA component (1.697 g/cm³; all densities quoted are those determined in CsCl density gradients), the 1.704 and 1.709 g/cm³ components form about 50, 25 and 10% of the genome, respectively; they are characterized by having symmetrical CsCl bands and melting curves, both of which have standard deviations close to those of bacterial DNAs of comparable molecular weight, and by their G + C contents being equal to 39, 48 and 54%, respectively; after heat-denaturation and reannealing, their buoyant densities in CsCl are greater than native DNA by 12, 10 and 3 mg/cm³, respectively. (2) The 1.705, 1.710, 1.714 and 1.723 g/cm³ components represent 4, 1.5, 7 and 1.5% of the DNA, respectively, and exhibit the properties of “satellite” DNAs; their CsCl bands and melting curves have standard deviations lower than those of bacterial DNAs; after heat-denaturation and reannealing, their buoyant densities are identical to native DNA, except for the 1.705 g/cm³ component, which remains heavier by 5 mg/cm³; in alkaline CsCl, only the 1.714 g/cm³ component shows a strand separation. (3) A number of minor components, forming 1% of the DNA, have been recognized, but they have not been investigated in detail; two of them (1.719 and 1.699 g/cm³) might correspond to ribosomal cistrons and mitochondrial DNA, respectively.     

黄河源园区高寒草地碳储量估算及其影响因素

高寒草地碳储量及其影响因素研究是认识青藏高原草地生态系统乃至陆地生态系统碳循环和气候变化的关键之一。利用2021年8月上旬地面调查数据与同期高分6号遥感数据建立回归关系,在反演研究区植被地上、地下生物量碳密度和0—40cm土壤层有机碳密度基础上,估算了黄河源园区高寒草地有机碳储量,并通过路径分析探讨了土壤理化性质对碳密度的影响驱动机制。结果表明：(1)2021年黄河源园区地上生物量、地下生物量、0—40cm土壤层碳密度分别为37.65g/m²、1305.28g/m²、4769.11g/m²;总碳储量为100.44Tg(1Tg=10¹²g),植被层和土壤层碳储量分别分为22.06Tg、78.38Tg,占总碳密度的21.96%、78.04%。(2)黄河源园区高寒草甸和高寒草原两种草地类型地上生物量碳密度分别为41.27g/m²、30.76g/m²;地下生物量碳密度分别为1661.41g/m²、618.74g/m²;0...     

Buoyant Densities and Dry-Matter Contents of Microorganisms: Conversion of a Measured Biovolume into Biomass

Several isolates of bacteria and fungi from soil, together with cells released directly from soil, were studied with respect to buoyant density and dry weight. The specific volume (cubic centimeters per gram) of wet cells as measured in density gradients of colloidal silica was correlated with the percent dry weight of the cells and found to be in general agreement with calculations based on the partial specific volume of major cell components. The buoyant density of pure bacterial cultures ranged from 1.035 to 1.093 g/cm³, and their dry-matter content ranged from 12 to 33% (wt/wt). Average values proposed for the conversion of bacterial biovolume into biomass dry weight are 1.09 g/cm³ and 30% dry matter. Fungal hyphae had buoyant densities ranging from 1.08 to 1.11 g/cm³, and their dry-matter content ranged from 18 to 25% (wt/wt). Average values proposed for the conversion of hyphal biovolume into biomass dry weight are 1.09 g/cm³ and 21% dry matter. Three of the bacterial isolates were found to have cell capsules. The calculated buoyant density and percent dry weight of these capsules varied from 1.029 g/cm³ and 7% dry weight to 1.084 g/cm³ and 44% dry weight. The majority of the fungi were found to produce large amounts of extracellular material when grown in liquid cultures. This material was not produced when the fungi were grown on either sterile spruce needles or membrane filters on an agar surface. Fungal hyphae in litter were shown to be free from extracellular materials.     

中国土壤容重特征及其对区域碳贮量估算的意义

容重是土壤最重要的物理性质之一,不仅能反映土壤质量和土壤生产力水平,还是区域尺度土壤碳贮量估算的重要参数。由于野外测定土壤容重费时费力、并且操作过程也容易造成较大的误差,因此,土壤容重在国内外大多数清查数据库中均缺失严重。通过收集和整理中国第二次土壤普查数据、中国生态系统研究网络数据和1980—2014年论文内的中国土壤容重数据(共11845条记录),系统地探讨了中国陆地生态系统土壤容重的整体分布特征、垂直分布特征以及不同土壤类型间的差异。分析结果表明:中国陆地生态系统的土壤容重数据整体呈正态分布,平均值为(1.32±0.21)g/cm~3,中值为1.35g/cm~3;土壤容重随土层深度增加而增加,两者间表现为显著的幂函数关系。土壤容重与有机质含量呈显著的正相关关系,与沙粒含量的负相关关系较弱。此外,不同土壤类型间的土壤容重差异较大,高山土平均容重最低(0.93 g/cm~3),而盐碱土平均容重最高(1.41 g/cm~3)。结果全面阐释了中国陆地生态系统土壤容重的基本特征及其变异规律,其结论还将为准确评估区域乃至全国土壤碳贮量提供重要参数。     

青海湖流域矮嵩草草甸土壤有机碳密度分布特征

通过对青海湖流域不同退化程度矮嵩草草甸土壤容重和有机碳含量的测定,确定了其土壤有机碳密度。结果表明:不同退化程度下矮嵩草草甸土壤有机碳含量和变化特征各有不同。从未退化-重度退化,0—100 cm土壤剖面平均有机碳含量分别为(25.17±4.73)g/kg,(17.51±3.06)g/kg,(20.79±1.30)g/kg和(14.53±1.20)g/kg,即未退化中度退化轻度退化重度退化;0—20 cm土壤平均有机碳含量从(64.47±11.70)g/kg减少为(14.52±1.52)g/kg,减少了77.48%。土壤剖面有机碳密度变化趋势与其有机碳含量变化趋势一致。0—100 cm土壤剖面有机碳密度分别为(18.16±4.12)kg/m3,(14.24±3.52)kg/m3,(18.64±2.82)kg/m3和(13.27±2.28)kg/m3,即中度退化未退化轻度退化重度退化;土壤有机碳集中分布在0—40 cm深度,从未退化到严重退化,该深度有机碳密度分别为(32.06±6.41)kg/m3,(25.10±4.20)kg/m3,(22.68±3.17)kg/m3和(17.10±2.77)kg/m3,比整个剖面有机碳密度高出76.53%,76.25%,21.68%和28.88%。不考虑其他因素,以空间尺度代替时间尺度,这一结果说明矮嵩草草甸的退化导致土壤逐渐释放有机碳,其作为储存碳的功能在减弱,必须加强对矮嵩草草甸生态系统的保护,以防止其碳库变为碳源。     

Identification and separation of components of calf thymus DNA using a CsCl-netropsin density gradient

Calf thymus DNA containing satellite components of various densities was used as a model to study the effect of netropsin on the density of DNA in a CsCl gradient. The binding of netropsin resulted in a decrease in density which depended upon the quantity of netropsin added and on the average composition of the DNA. Differences in density of DNA components were higher in CsCl - netropsin gradients than in simple CsCl gradients. By use of netropsin a main band and four satellite bands could be differentiated in calf thymus DNA. Satellite DNA's were isolated using preparative CsCl - netropsin gradient centrifugation and were characterised by density and homogeneity in native and in reassociated state. Two of the satellite components, with densities of 1.722 and 1.714 g/cm³, are probably of homogenous sequence, the other two components of densities 1.709 and 1.705 g/cm³ appear to be heterogeneous.     

排水对若尔盖高原泥炭地土壤有机碳储量的影响

泥炭地作为陆地上生态系统一个重要碳汇,存储了全球土壤有机碳储量的25%—43%。泥炭地排水与其他土地利用导致了大量的土壤有机碳损失。然而,有关排水对中国泥炭地土壤有机碳储量的影响研究报道较少,因此,为了获得更多可靠的泥炭地碳储量信息,以便减少它们估算的不确定性。选取了我国若尔盖高原未排水泥炭地和排水泥炭地进行土壤剖面取样,定量评价排水对泥炭地土壤有机碳储量的影响。研究表明:(1)未排水泥炭地土壤有机碳储量平均值为(923.71±107.18)t C/hm~2,为中国陆地和全球陆地土壤有机碳储量的8.1和9.4倍;而排水泥炭地土壤有机碳储量平均值为(574.01±66.86)t C/hm~2,为中国和全球陆地的5.1和5.8倍。(2)泥炭地排水后,导致表层(0—30 cm)土壤有机碳储量增加(59.11±9.31)t C/hm~2,可能源于土壤容重增加。(3)然而,完全考虑泥炭剖面深度后,排水泥炭地土壤有机碳储量较对照样地减少了349.7 t C/hm~2,这可能是由于泥炭地排水后,水位降低,加速了泥炭氧化,降低了泥炭厚度。     

Utilization of enzyme markers to determine the location of plasma membrane from Pisum epicotyls on sucrose gradients

Using linear sucrose gradients, particulates derived from pea (Pisum sativum L. cv. Alaska) epicotyls have been fractionated and examined for marker enzyme activity. The coincidence of three reputed plasma-membrane markers [cellulase (EC 3.2.1.4), K⁺-stimulated Mg²⁺-ATPase, and glucan synthetase] at the same position on sucrose density gradients, in combination with electron microscopic evidence reported by G. Shore and G. Maclachlan (J. Cell Biol. 64, 557–571; 1975), indicates that plasma membrane of pea epicotyl has a buoyant density of about 1.13 g/cm³. This density disagrees with those usually reported for plant plasma membranes and also with recent reports for Pisum. It is, however, shown to be distinct from the equilibrium densities of enzymic markers for particulate components derived from Pisum endoplasmic reticulum (1.10–1.11 g/cm³), Golgi (1.12 g/cm³) and mitochondria (1.18 g/cm³). Furthermore, other recent literature indicates that the 1.13 g/cm³ buoyant density may be characteristic of the plasma membrane of many members of the Leguminosae. Our data indicate that the conditions of differential centrifugation (time, centrifugal force), coupled with the amount of protein utilized, affect the resolution and interpretation of profiles of marker enzymes on sucrose gradients (e.g. glucan synthetase and K⁺-stimulated Mg²⁺-ATPase were sometimes found to be associated not only with particles of 1.13 g/cm³ density, but with particles of higher densities as well). Particulate cellulase was found to be associated only with particles with equilibrium densities of about 1.13 g/cm³. Cellulase thus proved to be the most useful marker for establishing a differential centrifugation regime which would permit examination of the 1.13 g/cm³ particulate components with minimal contamination by particles of higher densities.     

Fractionation of somatic and sperm chromatin during spermatogenesis in fish

A new approach is suggested for studying changes in the interactions of protein with DNA in the cells. Measurements of the buoyant density of chromatin were performed in somatic cells and in cells undergoing meiosis in fish. During the process of spermatogenesis some of the somatic histones on the DNA are replaced by a new class of proteins; consequently, the mature sperm contains a unique type of protein having a low mol. wt and a high proportion of arginine.The chromatin obtained from mature sperm is composed of a single component with a density of 1.48–1.49 g/cm³ as measured by CsCl equilibrium sedimentation. On the other hand, somatic cells contain chromatin with lower densities. Chromatin obtained from erythrocytes contains a single component with a density of 1.41–1.42 g/cm³ while liver chromatin shows two components; a main component with a density of 1.45–1.46 and a more heterogeneous component with a lighter density (1.32–1.35). There is a correlation between the buoyant density of the chromatin, the type of its basic proteins and the level of biosynthetic activity in the cells.