Genetic sex determination in <Emphasis Type="Italic">Astatotilapia calliptera</Emphasis>, a prototype species for the Lake Malawi cichlid radiation

East African cichlids display extensive variation in sex determination systems. The species Astatotilapia calliptera is one of the few cichlids that reside both in Lake Malawi and in surrounding waterways. A. calliptera is of interest in evolutionary studies as a putative immediate outgroup species for the Lake Malawi species flock and possibly as a prototype ancestor-like species for the radiation. Here, we use linkage mapping to test association of sex in A. calliptera with loci that have been previously associated with genetic sex determination in East African cichlid species. We identify a male heterogametic XY system segregating at linkage group (LG) 7 in an A. calliptera line that originated from Lake Malawi, at a locus previously shown to act as an XY sex determination system in multiple species of Lake Malawi cichlids. Significant association of genetic markers and sex produce a broad genetic interval of approximately 26 megabases (Mb) using the Nile tilapia genome to orient markers; however, we note that the marker with the strongest association with sex is near a gene that acts as a master sex determiner in other fish species. We demonstrate that alleles of the marker are perfectly associated with sex in Metriaclima mbenjii, a species from the rock-dwelling clade of Lake Malawi. While we do not rule out the possibility of other sex determination loci in A. calliptera, this study provides a foundation for fine mapping of the cichlid sex determination gene on LG7 and evolutionary context regarding the origin and persistence of the LG7 XY across diverse, rapidly evolving lineages.     

Impacts of Mauritia flexuosa degradation on the carbon stocks of freshwater peatlands in the Pastaza-Marañón river basin of the Peruvian Amazon

Tropical peat swamp forests (PSF) are characterized by high quantities of carbon (C) stored as organic soil deposits due to waterlogged conditions which slows down decomposition. Globally, Peru has one of the largest expanse of tropical peatlands, located primarily within the Pastaza-Marañón river basin in the Northwestern Peru. Peatland forests in Peru are dominated by a palm species—Mauritia flexuosa, and M. flexuosa-dominated forests cover ~?80% of total peatland area and store ~?2.3 Pg C. However, hydrologic alterations, land cover change, and anthropogenic disturbances could lead to PSF’s degradation and loss of valuable ecosystem services. Therefore, evaluation of degradation impacts on PSF’s structure, biomass, and overall C stocks could provide an estimate of potential C losses into the atmosphere as greenhouse gases (GHG) emissions. This study was carried out in three regions within Pastaza-Marañón river basin to quantify PSF’s floristic composition and degradation status and total ecosystem C stocks. There was a tremendous range in C stocks (Mg C ha^?1) in various ecosystem pools—vegetation (45.6–122.5), down woody debris (2.1–23.1), litter (2.3–7.8), and soil (top 1 m; 109–594). Mean ecosystem C stocks accounting for the top 1 m soil were 400, 570, and 330 Mg C ha^?1 in Itaya, Tigre, and Samiria river basins, respectively. Considering the entire soil depth, mean ecosystem C stocks were 670, 1160, and 330 Mg C ha^?1 in Itaya, Tigre, and Samiria river basins, respectively. Floristic composition and calcium to Magnesium (Ca/Mg) ratio of soil profile offered evidence of a site undergoing vegetational succession and transitioning from minerotrophic to ombrotrophic system. Degradation ranged from low to high levels of disturbance with no significant difference between regions. Increased degradation tended to decrease vegetation and forest floor C stocks and was significantly correlated to reduced M. flexuosa biomass C stocks. Long-term studies are needed to understand the linkages between M. flexuosa harvest and palm swamp forest C stocks; however, river dynamics are important natural drivers influencing forest succession and transition in this landscape.

     

炭基肥对旱区玉米农田土壤理化性质、酶活性及微生物群落的影响

探讨炭基肥对土壤环境因子和微生物群落的影响,可以解决如何通过炭基肥改善旱区土壤状况和促进农业可持续发展的问题. 以玉米“先玉335”为供试品种,采用随机区组设计,设5个处理：CK（普通化肥450 kg·hm^-2）、T1（炭基肥1 125 kg·hm^-2）、T2（炭基肥1 013 kg·hm^-2）、T3（炭基肥900 kg·hm^-2）和T4（炭基肥788 kg·hm^-2）,采集成熟期玉米农田土壤,分析不同炭基肥处理对土壤理化性质、土壤酶活性和微生物多样性的影响. 结果表明：①与单施化肥相比,施用炭基肥显著降低旱区农田土壤容重,增大土壤间孔隙度与田间持水量,提高土壤养分及酶活性. T1和T2处理的有机碳、全氮和全磷含量分别显著增加13.68%~32.63%、25.00%~26.79%和35.00%~47.50%,脲酶、蔗糖酶和碱性磷酸酶活性分别显著增加49.04%~91.35%、48.88%~58.71%和20.69%~31.03%. ②T3和T4处理降低了微生物的Chao1、Shannon、Simpson、Faith_pd和Pielou_e指数. 各处理优势菌门为变形菌门、放线菌门和酸杆菌门,相对丰度为71.50%~86.66%,T1和T2处理显著增加了变形菌门和放线菌门相对丰度,降低了酸杆菌门相对丰度. 各处理下微生物的氨基酸代谢、碳水化合物代谢、能量代谢、遗传信息处理和新陈代谢功能的相对丰度无显著性差异,均在18.12%~21.34%之间. ③相关性分析显示,除土壤容重外,土壤物理性质、土壤养分与土壤酶之间呈显著正相关,不同优势菌门与土壤环境因子之间的关系存在显著差异,微生物的6个功能通路与土壤养分显著正相关. PLS-SEM分析发现,炭基肥通过调控土壤物理性质、土壤养分以及土壤酶直接或间接影响微生物群落,土壤养分是土壤微生物群落演替的主要驱动参数. 最后,PCA分析显示,土壤综合肥力表现为：T2>T1>T3>CK>T4. 综上,炭基肥改善了旱区土壤的物理、化学和生物特性,从而提高了土壤综合肥力,炭基肥1 013~1 125 kg·hm^-2的施用量适合在旱区玉米种植中推广.     

Type 0092丝状菌污泥微膨胀在短程硝化中的实现

利用Type 0092丝状菌不易引发污泥恶性膨胀的特点,本实验采用实际生活污水,以SBR反应器接种短程硝化污泥,考察了短程硝化状态下启动Type 0092丝状菌污泥微膨胀的特性,研究了系统启动与维持期间的污泥沉降性能、亚硝酸盐积累率(NAR)、污染物去除特性以及污泥菌群结构变化情况.结果表明控制DO为0. 3～0. 8 mg·L~(-1),F/M(以COD/MLSS计)=0. 24 kg·(kg·d)~(-1),按照交替缺氧/好氧模式运行(单周期3次,缺氧∶好氧=20 min∶60 min),能够启动Type 0092丝状菌污泥微膨胀与短程硝化耦合,系统SVI值维持在180 m L·g~(-1)左右,NAR一直维持在99%左右,COD和TN去除率能够分别提高约13%和5%,相较于传统全程硝化非微膨胀状态曝气量能节省约62. 5%.当交替缺氧/好氧模式变为单周期交替6次,缺氧∶好氧=10 min∶30 min,亚硝酸盐氧化菌(NOB)的活性会恢复,使短程硝化被破坏;低溶解氧、交替缺氧/好氧、低负荷是实现Type 0092丝状菌污泥微膨胀的关键因素,当负荷(以COD/MLSS计)大于0. 25 kg·(kg·d)~(-1)时,仅靠低溶解氧和间歇曝气无法维持污泥微膨胀状态.     

厌氧条件下砂壤水稻土N2、N2O、NO、CO2和CH4排放特征

了解厌氧条件土壤反硝化气体(N2、N2O和NO)、CO2和CH4排放特征,是认识反硝化过程机制的基础,并有助于制定合理的温室气体减排措施.定量反硝化产物组成,可为氮转化过程模型研发制定正确的关键过程参数选取方法或参数化方案.本研究选取质地相同(砂壤土)的两个水稻土为研究对象,通过添加KNO3和葡萄糖的混合溶液,将培养土壤的初始NO-3和DOC含量分别调节到50 mg·kg-1和300 mg·kg-1,采用氦环境培养-气体及碳氮底物直接同步测定方法,研究完全厌氧条件下土壤N2、N2O、NO、CO2和CH4的排放特征,并获得反硝化气态产物中各组分的比率.结果表明,在整个培养过程中,两个供试土壤的N2、N2O和NO累积排放量分别为6~8、20和15~18 mg·kg-1,这些气体排放量测定结果可回收土壤NO-3变化量的95%~98%,反硝化气态产物以N2O和NO为主,其中3种组分的比率分别为15%~19%(N2)、47%~49%(N2O)和34%~36%(NO);但反硝化气体产物组成的逐日动态均显现为从以NO为主逐渐过渡到以N2O为主,最后才发展到以N2为主.以上结果说明,反硝化气体产物组成是随反硝化进程而变化的,在以气体产物组成比率作为关键参数计算各种反硝化气体产生率或排放率的模型中,很有必要重视这一点.     

利用玉米浸泡液产电的微生物燃料电池研究

以玉米淀粉生产过程中的浸泡液（玉米浸泡液）作为接种液和基质,利用“三合一”膜电极的单室空气阴极微生物燃料电池进行试验,采用在线监测电压和废水分析方法对产电功率和化学需氧量（COD）、氨氮进行测定,探讨高COD、高氨氮有机废水产电及废水处理的可行性.结果表明,经过94 d（1个周期）的连续运行（固定外电阻为1 000 Ω）,17 d时输出电压达到最大（525.0 mV）,稳定期最大输出功率可达169.6 mW/m²,此时电池相应的电流密度为440.2 mA/m²,内阻约为350 Ω,开路电压619.5 mV;但燃料电池电子利用效率较低（库仑效率为1.6%）;1个周期结束时浸泡液的COD去除率达到51.6%,氨氮去除率25.8%.本试验利用玉米浸泡液成功获得电能,同时对浸泡液有效地进行了处理,为其资源化利用提供新途径.     

江西定南县离子型稀土尾矿周边水体氮污染状况与分布特征

为探究\"稀土王国\"江西省赣南地区离子型稀土矿对周边水体环境的影响,以离子型稀土矿分布密集区定南县濂江月子河流域和龙迳河龙头流域为研究对象,综合分析研究区特征污染物ρ（NH₄+-N）空间分布特征,采用相关性分析和主成分分析揭示其主要污染来源及影响因素.结果表明:①离子型稀土矿停产整顿半年后,濂江月子河流域和龙迳河龙头流域ρ（NH₄+-N）超过1.00和2.00 mg/L的采样点分别达72%和68%;pH范围为2.95~7.66,平均值分别为6.23和5.53,水体总体上偏酸性;ρ（TN）、ρ（NH₄+-N）、EC与ρ（NO₃--N）变异系数较大,均介于0.80~1.50之间.②相关性分析结果显示,ρ（NH₄+-N）与ρ（TN）、EC均呈极显著正相关（P < 0.01）;ρ（NH₄+-N）与pH呈显著负相关（P < 0.05）.③流经稀土尾矿区的水体中ρ（NH₄+-N）随距离增加呈现明显的空间梯度分布特征,即距稀土矿区边界200 m处水体中ρ（NH₄+-N）最高（12.20~200.00 mg/L）,其次为1.15 km内（3.69~11.80 mg/L）及3.5 km以上水体（0.80~1.51 mg/L）,矿区周边未受到采矿活动影响的水体中ρ（NH₄+-N）最低（0.03~0.15 mg/L）.④PCA结果表明,2条河流的主要环境影响因子为ρ（TN）、ρ（NH₄+-N）、pH和EC,主要受到周边稀土矿山尾矿的强烈影响.研究显示,离子型稀土矿原位浸矿开采停产半年后,重点小流域水体中ρ（NH₄+-N）高概率超标的现状仍然存在,受稀土开采活动影响较大.建议进一步开展重点小流域NH₄+-N剩余\"库容\"精算和矿山周边地表水定期监测.      

Chorionic villi sampling changes maternal serum alpha-fetoprotein

Second trimester amniocentesis has traditionally been utilized for prenatal genetic diagnosis. Chorionic villi sampling (CVS) is presently offered as an alternative. The occurrence of fetomaternal bleed (FMB) during CVS could increase the rate of post sampling abortion and, additionally, be of significance in patients at risk for isoimmunization. Detection and quantitation of FMB can be accomplished by the determination of changes in maternal serum alpha-fetoprotein (MSAFP) before and after CVS.     

CO2倍增和施氮对水稻不同生长期土壤反硝化细菌丰度的影响

随着全球气候变化的不断加剧,大气CO₂浓度呈明显增加趋势,这将间接影响土壤-植物-微生物系统的氮循环过程.为研究典型水稻土壤反硝化细菌对CO₂浓度升高的响应规律和机制,借助水稻密闭培养箱,运用实时荧光定量聚合酶链式反应（Real-Time qPCR）分子技术,设置不施氮（0 mg/kg）和常规施氮（100 mg/kg）2个处理,研究CO₂倍增对水稻不同生长期土壤关键反硝化功能细菌（narG、nirK和nirS型）丰度的影响.结果表明:①在2种施氮水平,CO₂倍增显著促进了水稻分蘖期、孕穗期、扬花期和成熟期水稻根系生长（增幅为2.96%~28.4%）、地上部生物量增加（增幅为7.1%~107.3%）以及成熟期籽粒干质量的增加（增幅为19.5%和38.0%）,具有显著的增产效应.②反硝化细菌丰度对CO₂倍增的响应与生育期及施氮水平有关,CO₂倍增在2个施氮水平均抑制分蘖期反硝化细菌的繁殖,显著增加孕穗期反硝化细菌数量;在水稻扬花期,CO₂倍增促进了施氮处理narG和nirS型反硝化细菌数量的增加,在成熟期抑制未施氮处理下narG、nirK和nirS型反硝化细菌的生长.另外,narG、nirK、nirS型反硝化细菌丰度整体表现为narG > nirS > nirK,且随水稻的生长,其在成熟期的丰度均呈降低趋势.nirK和nirS基因同属亚硝酸还原酶,但nirS基因丰度高于nirK,且对CO₂倍增和施氮的响应有所差异.研究显示,CO₂倍增可显著增加水稻生长和产量,不同施氮水平对稻田土壤反硝化细菌丰度的影响存在差异.