15N natural abundance in forest and pasture soils of the Brazilian Amazon Basin

The natural abundance of ¹⁵N was examined in soil profiles from forests and pastures of the Brazilian Amazon Basin to compare tropical forests on a variety of soil types and to investigate changes in the sources of nitrogen to soils following deforestation for cattle ranching. Six sites in the state of Rondônia, two sites in Pará and one in Amazonas were studied. All sites except one were chronosequences and contained native forest and one or more pastures ranging from 2 to 27 years old. Forest soil ¹⁵N values to a depth of 1 m ranged from 8 to 23 and were higher than values typically found in temperate forests. A general pattern of increasing ¹⁵N values with depth near the soil surface was broadly similar to patterns in other forests but a decrease in ¹⁵N values in many forest profiles between 20 and 40 cm suggests that illuviation of ¹⁵N-depleted nitrate may influence total soil ¹⁵N values in deeper soil where total N concentrations are low. In four chronosequences in Rondônia, the ¹⁵N values of surface soil from pastures were lower than in the original forest and ¹⁵N values were increasingly depleted in older pastures. Inputs of atmospheric N by dinitrogen fixation could be an important N source in these pastures. Other pastures in Amazonas and Pará and Rondônia showed no consistent change from forest values. The extent of fractionation that leads to ¹⁵N enrichment in soils was broadly similar over a wide range of soil textures and indicated that similar processes control N fractionation and loss under tropical forest over a broad geographic region. Forest ¹⁵N profiles were consistent with conceptual models that explain enrichment of soil ¹⁵N values by selective loss of ¹⁴N during nitrification and denitrification.     

Changes in the origin and quality of soil organic matter after pasture introduction in Rondônia (Brazil)

We examined the effects of the conversion of tropical forest to pasture on soil organic matter (SOM) origin and quality along a chronosequence of sites, including a primary forest and six pastures. Bulk soil samples received a physical size-fractionation treatment to assess the contribution of each compartment to total SOM pool. Besides a general increase in total C and N stocks along the chronosequence, we observed a reduction of the relative contribution of the coarser fractions to total soil C content, and an increased concentration in the finer fractions. The origin of the C in each size fraction was established from measurements of¹³C abundance. After 80 years about 93% of the C in the least humified fraction of the top 10 cm of soil was of pasture origin, while in the most humified it was 82%. Chemical analyses indicated that the fine silt and coarse clay fractions contained the most refractory carbon.     

Sterols from three Lactarius species

The sterol composition of three fungi was determined. Ergosterol is the major sterol, accompanied by other closely related sterols.     

Chemical constituents of some Tricholomataceae

Sterols, fatty acids and free amino acids of four species of Tricholomataceae were investigated. They contained ergosterol in high amount and the related sterols, fucosterol, sitosterol, cholesterol and brassicasterol. Linoleic and palmitic are the main unsaturated and saturated fatty acids respectively. The most abundant free amino acids were alanine, valine and proline.     

广西扶绥南山洞新发现的人类化石和蒙古野驴化石——末次冰期华南气候变化的哺乳动物化石新证据

广西扶绥县南山洞发现人类化石及哺乳动物化石。人类化石包括2枚智人牙齿化石,分别是左下第三臼齿和右下第二臼齿,其形态特征与广西其他山洞发现的智人化石相似,归入晚期智人。哺乳动物化石多为华南大熊猫———剑齿象动物群成员,时代属更新世晚期。该地点新发现的蒙古野驴化石属华南晚更新世动物群的首次发现。南山洞所有化石发现于洞内浅褐色砂质粘土中,堆积物第二层钙板层的铀系年龄为30—40ka。蒙古野驴的出现暗示中国南方大陆可能在末次冰期出现过干冷的气候环境。     

水电开发对鱼类种群分布及生态类型变化的影响——以溪洛渡至向家坝河段为例

梯级水库修建后自然河流形成了河相段和湖相段,而河流生境的改变对鱼类种群空间分布和生态类型变化产生了重要影响。为探究金沙江梯级水电开发对鱼类资源的影响,结合2018年5月渔获物和文献记载水库修建前后的渔获物数据,分析了鱼类群落组成及变化,优势物种及群落多样性特点,以及鱼类在河相、湖相段生态类型的变化。结果表明,梯级水库建设后溪洛渡至向家坝鱼类的种类数减少,随着水库的运行该减少趋势放缓,而大型鱼的种类数占比呈增长趋势。受生境变化的影响,鱼类优势物种发生变化,水库河相段和湖相段生态类型差异较大。生态类型组成上以缓流型、生活于水流中下层、产卵初始水温高于18℃等生态类型占优。研究表明,高坝大库的运行会造成鱼类种群以生态需求为目标,形成明显的空间分布和群落结构特征,而梯级水库建设导致的水动力条件差异是鱼类群落生态类型差异的内在驱动力。     

0.21nm分辨率BO-(L-精氨酸)牛胰岛素晶体结构研究

应用差值Fourier技术,立体化学最小二乘技术和XPLOR程序并辅以电子密度图的人工拟合,以三方二锌猪胰岛素模型为起点,解析了0.21nm分辨率BO-(L-精氨酸)牛胰岛素的晶体结构,最终R因子为18.2%,与标准键长与键角的均方根偏差分别为0.0022nm和 4.3°.从电子密度图与模型的拟合来看,独立区两个分子中B链N端加长的L-精氨酸清晰可见.相对于三方二锌猪胰岛素分子,B链N端晶体学微环境发生了变化.     

Soil Carbon Turnover Measurement by Physical Fractionation at a Forest-to-Pasture Chronosequence in the Brazilian Amazon

The effect of conversion from forest-to-pasture upon soil carbon stocks has been intensively discussed, but few studies focus on how this land-use change affects carbon (C) distribution across soil fractions in the Amazon basin. We investigated this in the 20 cm depth along a chronosequence of sites from native forest to three successively older pastures. We performed a physicochemical fractionation of bulk soil samples to better understand the mechanisms by which soil C is stabilized and evaluate the contribution of each C fraction to total soil C. Additionally, we used a two-pool model to estimate the mean residence time (MRT) for the slow and active pool C in each fraction. Soil C increased with conversion from forest-to-pasture in the particulate organic matter (>250 μm), microaggregate (53–250 μm), and d-clay (<2 μm) fractions. The microaggregate comprised the highest soil C content after the conversion from forest-to-pasture. The C content of the d-silt fraction decreased with time since conversion to pasture. Forest-derived C remained in all fractions with the highest concentration in the finest fractions, with the largest proportion of forest-derived soil C associated with clay minerals. Results from this work indicate that microaggregate formation is sensitive to changes in management and might serve as an indicator for management-induced soil carbon changes, and the soil C changes in the fractions are dependent on soil texture.     

鼎湖山南亚热带常绿阔叶林碳素积累和分配特征

研究了鼎湖山南亚热带常绿阔叶林 40 0多年林龄的锥栗 (Castanopsis chinensis)、黄果厚壳桂 (Crypto-carya concinna)和 50多年林龄的黄果厚壳桂、鼎湖钓樟 (Lindera chunii)两个群落碳素积累和分配特征。结果表明 ,两林分间植物碳素含量在不同器官和不同层中的分配格局均十分相似 ,总平均分别为 41 .980 %(锥栗、黄果厚壳桂群落 )和 40 .377% (黄果厚壳桂、鼎湖钓樟群落 )。锥栗、黄果厚壳桂群落生态系统碳总贮量为 2 4 4 .998t/ hm2 ,其中植被部分为 1 54.2 89t/ hm2 ,土壤为 89.1 2 8t/ hm2 ,地表凋落物层为 1 .581 t/ hm2。黄果厚壳桂、鼎湖钓樟群落植被碳总贮量为 84.1 51 t/ hm2。在两林分植被碳总贮量中 ,乔木层分别占了97.47% (锥栗、黄果厚壳桂群落 )和 98.0 4 % (黄果厚壳桂、鼎湖钓樟群落 ) ,而在乔木层碳总贮量中 ,干器官则分别占 47.93% (锥栗、黄果厚壳桂群落 )和 44.66% (黄果厚壳桂、鼎湖钓樟群落 )。锥栗、黄果厚壳桂群落植被碳年积累量为 3.1 4 9t/ (hm2· a) ,黄果厚壳桂、鼎湖钓樟群落植被碳年积累量则为 3.42 5 t/ (hm2· a)。     

有丝分裂激酶Aurora B的研究进展

真核生物细胞通过有丝分裂将遗传物质均等地分配到两个子细胞中,从而维持基因组的稳定性。有丝分裂的每一环节都需要精准而细致的调控,这依赖于一系列调节机制,尤其需要多个相关激酶的共同协调。Aurora B是一个关键的有丝分裂调控激酶,伴随有丝分裂的进行,其先后在染色体臂、内着丝粒、中央纺锤体、中体上动态分布。与其高度时空动态性相一致的是,Aurora B在有丝分裂的多个环节,如姐妹染色体粘连、动粒微管连接、纺锤体检验点和胞质分裂过程中都发挥着一系列重要功能。本文将概述近年来Aurora B激酶功能与调控方面的研究进展。