喜马拉雅中部甘达基河流域尼泊尔国鸟(棕尾虹雉)生境分布变化

甘达基河流域(Gandaki River Basin,GRB)是喜马拉雅中部地区的一部分,该地区栖息着许多珍稀的野生动物。由于气候和人类活动的影响,许多珍稀保护物种的生境处于危险之中。本研究基于最大熵(MaxEnt)模型,运用生物气候、土地覆被和DEM数据,分析各环境要素对棕尾虹雉(Lophophorusimpejanus)的生境适宜性的影响,评估棕尾虹雉现在状况和未来栖息地分布的变化。研究表明,目前棕尾虹雉的高度适宜栖息地面积约为749 km^2,主要分布在流域北部、东部和西部,尤其是郎塘国家公园、马纳斯卢峰自然保护区和安纳布尔纳峰自然保护区等保护区内。到2050年,棕尾虹雉的高度适宜栖息地面积将减少至561 km^2,主要在流域北部和西北部(即Chhyo,Tatopani,Humde和Chame地区)。未来环境变化的模拟表明,由于适宜栖息地面积的减少,棕尾虹雉面临的生存风险将增加。     

粤港澳大湾区海洋经济创新发展研究

海洋经济创新发展对粤港澳大湾区创新驱动、打造具有国际竞争力的科技创新中心具有重要意义。文章介绍粤港澳大湾区当前的海洋经济创新发展情况及其优势和不足,从构建大湾区海洋创新发展产业链、驱动陆海科技创新一体化、完善科技创新驱动体制机制和推动科技金融服务蓝色经济发展等方面,提出粤港澳大湾区海洋经济创新发展的突破要点和路径。     

鳜鱼(Siniperca chuatsi)脂肪酸去饱和酶和延长酶基因全长cDNA序列的克隆与分析

利用RT-PCR和RACE方法克隆得到鳜鱼肝脏中控制高不饱和脂肪酸合成的脂肪酸去饱和酶(fatty acid desaturase,FAD)和脂肪酸延长酶(fatty acid elongase,ELO)基因的全长cDNA序列。FAD基因的全长cDNA序列1882bp,编码445个氨基酸,该蛋白序列含有FAD全部的特征结构区,包括3个组氨酸簇、2个跨膜区和1个细胞色素b5结构域,与其它鱼类FAD氨基酸序列的同源性为66.5%-90.1%,系统树分析显示其与欧洲鲈鱼和金头鲷等海水鱼类的亲缘关系最近。获得的ELO基因全长cDNA序列1401bp,编码294个氨基酸,该蛋白序列含有单一的氧化还原中心组氨酸簇、内质网停留信号和多个跨膜区等ELO特征结构,与其它几种鱼类ELO氨基酸序列的同源性为71.8%-86.7%,系统进化分析显示其与南方蓝鳍金枪鱼和金头鲷的亲缘关系较近。鳜鱼FAD和ELO基因全长cDNA序列的获得可为进一步研究其HUFA合成能力及调控机理奠定基础。     

Miocene facies associations and sedimentary evolution of the Southern Transylvanian Basin (Romania): Implications for hydrocarbon exploration

The Transylvanian Basin is a mature hydrocarbon province of Romania characterized by two petroleum systems: Mesozoic (thermogenic) and Miocene (biogenic). An extensive outcrop-based sedimentological and micropaleontological study correlated to seismic and well data discusses the elements of the Miocene petroleum system. The facies associations are indicative of alluvial, fandelta, shallow- and deep-marine settings. These are grouped into four different depositional systems (evaporite, mud-carbonate, sand-mud and sand-gravel). Their evolution in time and space shows large differences between various parts of the basin that have important consequences for exploration.     

中国沿海10 种方蟹16S rRNA 基因序列分析及系统发育研究

中国沿海10种方蟹线粒体16S rRNA基因部分片段的序列长度为517 bp～533 bp。它们的核苷酸序列A、T、G、C的含量相似,A+T的含量(69.8%～76.0%)明显高于G+C的含量;10种方蟹的16S rRNA基因序列比对获得541 bp的同源序列(含插入/缺失位点),除插入/缺失位点外共检测到146个变异位点,其中81个为简约信息位点。4种厚蟹与2种近方蟹的遗传距离(0.054～0.085)都显著小于与其他方蟹之间的遗传距离,甚至明显小于与4种厚蟹原本属于同一相手蟹科的2种相手蟹之间的遗传距离(0.105～0.155);而基于16S rRNA基因片段序列采用NJ法构建的系统进化树的拓扑结构也显示,原本属于相手蟹科的侧足厚蟹、天津厚蟹、日本仿厚蟹和伍氏仿厚蟹没有与2种相手蟹聚为一支,而是最终与属于弓蟹科的2种近方蟹聚为一大支,且有高达99%的支持率。结果表明,4种厚蟹与2种近方蟹的亲缘关系相对较近,而与2种相手蟹等其他方蟹的亲缘关系则相对较远。因此,研究结果支持将4种厚蟹从相手蟹科移到弓蟹科。此外,属于相手蟹科的2种相手蟹聚为一支,属于方蟹科的白纹方蟹和属于斜纹蟹科的瘤突斜纹蟹又各自成为一支;表明16S rRNA基因的分子数据支持其形态学分类结果的正确性,提示上述4科蟹类可能分别为单系。     

粤港澳大湾区知识网络空间结构演化特征与影响机制

以2000—2018年国内外期刊数据库合作论文数据为基础,借助社会网络分析和空间结构指数法分析了粤港澳大湾区知识空间网络结构演化特征与影响因素,结果发现：1）知识网络格局由广州的“一家独大”逐渐演变为广州、深圳、香港“齐头并进”的发展态势。香港虽然处于知识网络的核心位置,但受行政壁垒的影响,主要与广州、深圳高等级的城市建立紧密的知识合作联系。2）粤港澳大湾区知识联系网络呈现“核心—边缘”结构,西部地区知识联系远低于东部地区,虽然研究期内湾区的知识网络的极化特征得到一定的缓解,但不均衡性仍然显著。3）湾区知识活动主体的自身需求是促进城市间知识合作的内在驱动力,知识环境和知识联系通道是区域知识合作网络外在推动力,在内生作用和外生作用的共同影响下,知识合作产出得以实现,粤港澳大湾区知识网络得以发展。     

从珠三角到大珠三角再到粤港澳大湾区：改革开放以来中国的国家尺度重组

尺度重组是解释当前国家、城市等地域组织参与全球化竞争的工具媒介。文章以中国华南地区改革开放以来广东、香港、澳门三地跨界合作为例,借鉴行动者网络理论的研究方法深入剖析珠三角、大珠三角及粤港澳大湾区3个“新国家空间”的尺度重组过程,揭示中国尺度重组的政治经济逻辑。研究发现,行动者拥有的资源决定了其在尺度网络中的地位,而中国的“新国家空间”形成主要依托中央政府推动,其发展目标的设定具有决定性作用,港澳特区政府、广东省地方政府、乡镇企业和外资企业等其他行动者在协同合作中将自身的发展目标与之融合形成了“强制通过点”。纵观三阶段的演变过程,制度因素的重要性越来越得到凸显。     

笛鲷属(Lutjanus)鱼类线粒体16S rRNA基因序列比较及系统学分析

对笛鲷属9种鱼的线粒体DNA16S rRNA基因片段进行了PCR扩增,扩增产物经纯化后测序,得到了长度为561bp的分析序列。结合GenBank中的另外9种笛鲷的16S rRNA同源序列计算得出A、T、G、C的含量平均为28.5%、22.1%、23.6%和25.8%,AT含量稍高于GC含量,18种笛鲷碱基组成差异不大。利用MEGA3.1软件对所得序列进行比对后检测到72个变异位点,其中包括简约信息位点44个,在变异位点中75.61%的碱基替换是由于发生了转换,转换/颠换平均为3.1︰1。计算了种间的遗传距离,结果表明,序列差异在0.0193-0.0680之间,其中勒氏笛鲷和金焰笛鲷、勒氏笛鲷和金带笛鲷的序列差异最小,而红鳍笛鲷和金焰笛鲷、红鳍笛鲷和画眉笛鲷的序列差异最大。选用高体四长棘鲷(Argyrops spinifer)为外群,利用NJ法构建了分子系统树,结果表明:本研究中的9种南海笛鲷与其它9种笛鲷进化关系较远;并且南海9种笛鲷相互之间仍然保持着着相对较远的遗传距离,遗传多样性较好。     

Distribution of diagenetic alterations within depositional facies and sequence stratigraphic framework of fluvial sandstones: Evidence from the Petrohan Terrigenous Group,Lower Triassic,NW Bulgaria

Sequence stratigraphy of fluvial deposits is a controversial topic because changes in relative sea level will eventually have indirect impact on the spatial and temporal distribution of depositional facies. Changes in the relative sea level may influence the accommodation space in fluvial plains, and hence have impact on types of fluvial system, frequency of avulsion, and style of vertical and lateral accretion. This study aims to investigate whether depositional facies and changes in the fluvial system of the Lower Triassic Petrohan Terrigenous Group sandstones (NW Bulgaria) in response to changes in the relative sea level have an impact on the spatial and temporal distribution of diagenetic alterations.     

The cordierite‐bearing anatectic rocks of the higher Himalayan crystallines (eastern Nepal): low‐pressure anatexis,melt productivity,melt loss and the preservation of cordierite

Cordierite‐bearing anatectic rocks inform our understanding of low‐pressure anatectic processes in the continental crust. This article focuses on cordierite‐bearing lithologies occurring at the upper structural levels of the Higher Himalayan Crystallines (eastern Nepal Himalaya). Three cordierite‐bearing gneisses from different geological transects (from Mt Everest to Kangchenjunga) have been studied, in which cordierite is spectacularly well preserved. The three samples differ in terms of bulk composition likely reflecting different sedimentary protoliths, although they all consist of quartz, alkali feldspar, plagioclase, biotite, cordierite and sillimanite in different modal percentages. Analysis of the microstructures related to melt production and/or melt consumption allows the distinction to be made between peritectic and cotectic cordierite. The melt productivity of different prograde assemblages (from two‐mica metapelite/metagreywacke to biotite‐metapelite) has been investigated at low‐pressure conditions, evaluating the effects of muscovite v. biotite dehydration melting on both mineral assemblages and microstructures. The results of the thermodynamic modelling suggest that the mode and type of the micaceous minerals in the prograde assemblage is a very important parameter controlling the melt productivity at low‐pressure conditions, the two‐mica protoliths being significantly more fertile at any given temperature than biotite gneisses over the same temperature interval. Furthermore, the cordierite preservation is promoted by melt crystallization at a dry solidus and by exhumation along P‐T paths with a peculiar dP/dT slope of about 15–18 bar °C^?1. Overall, our results provide a key for the interpretation of cordierite petrogenesis in migmatites from any low‐P regional anatectic terrane. The cordierite‐bearing migmatites may well represent the source rocks for the Miocene andalusite‐bearing leucogranites occurring at the upper structural levels of the Himalayan belt, and low‐P isobaric heating rather than decompression melting may be the triggering process of this peculiar peraluminous magmatism.