西沙永兴岛抗风桐与海岸桐群落凋落叶分解及中型土壤动物的贡献

我国南海诸岛主要是珊瑚岛。植物凋落物分解是生态系统元素循环的关键环节,但目前关于南海珊瑚岛生态系统凋落物分解的研究还是空白。以我国西沙群岛的优势树种抗风桐（Pisonia grandis）和海岸桐（Guettarda speciosa）为研究对象,采用凋落物袋法,分别于分解期间的第3、6、9、13和15个月取样,探究中型土壤动物对两种植物群落中凋落物分解过程中质量损失和养分释放的影响。结果表明：与没有中型土壤动物存在的情况（0.1 mm凋落物袋）相比,分解开始后的6个月内,中型土壤动物存在（2 mm凋落物袋）使抗风桐和海岸桐凋落叶分解速率分别提高了12.3%和4.8%（P<0.05）;分解6-15个月期间,中型土壤动物存在使抗风桐和海岸桐凋落叶分解速率分别提高了33.0%和12.3%（P<0.05）。中型土壤动物排除显著影响了不同分解阶段凋落叶总碳（Total carbon,TC）、总氮（Total nitrogen,TN）、纤维素、木质素和半纤维素的残留率变化。中型土壤动物群落组成受土壤温度显著影响（P<0.05）,它们对凋落叶分解的贡献可能主要受优势类群如真螨目和寄螨目的影响。相较海岸桐,抗风桐凋落叶的分解周期更短,中型土壤动物对其的贡献更大;选用抗风桐作为南海珊瑚岛退化植被恢复或新建的先锋种对促进生态系统元素循环更有利。     

基于Landsat-8影像的沿海城市公园冷岛效应——以厦门为例

城市公园主要由水体和绿色植被等景观构成,其形成的公园冷岛（Park cool island,PCI）已成为减缓城市热岛效应的重要途径之一。采用景感生态学中的景感营造理念规划设计城市公园或优化公园空间结构有助于增强公园冷岛效应,进一步改善局地城市热环境。选择沿海城市——厦门市为研究对象,基于2013年8月的Landsat-8 OLI/TIRS遥感影像和Google Earth高分影像数据,首先提取了研究区15个公园的土地利用信息,采用改进的地表温度单通道算法,获取了城市公园地表温度数据,并采用缓冲区分析、景观格局指数和多元统计等方法定量分析公园内部平均地表温度、城市公园冷岛强度（即降温幅度）、公园冷岛影响距离（即对周边区域的降温范围）三者的主要影响因子,并利用景感生态学原理初步剖析了城市公园景感营造的原则。结果显示：（1）公园面积和公园建设用地面积是影响公园平均温度的关键因子（R²=0.915）,这两个因子与公园平均温度均呈显著非线性相关;公园面积存在阈值55 hm²左右;（2）公园冷岛PCI强度由公园绿地面积、公园建筑面积和面积-周长形状指数（P/A）三个因子决定（R²=0.911）;公园冷岛PCI强度与公园绿地面积呈显著非线性正相关,与公园建筑面积呈显著非线性负相关,与面积-周长形状指数（P/A）呈显著线性负相关;在确保公园绿地面积达到一定阈值时,应该尽量降低公园建筑面积,增加公园形状复杂度,有利于其PCI强度的增加,缓解城市热岛效应;（3）公园冷岛影响距离由公园面积和公园水体面积比例决定（R²=0.719）,公园冷岛影响距离与两者呈显著正相关;绿地公园中提高公园水体的面积比例,有助于增大公园冷岛的影响距离;（4）城市公园的规划与设计,需要运用景感生态学的原理,从缓解城市热岛效应的角度,充分考虑公园大小、形状、土地利用类型组成比例及空间配置等因素。     

Study of the independent gametophytes found on Jeju Island in South Korea and the first record of the obligate independent gametophyte of Antrophyum obovatum Baker

Fern gametophytes have often been neglected in research; however, studies on gametophytes are crucial for a better understanding of the evolution of ferns. During their life cycle, some gametophytes produce large and long‐lived populations without producing sporophytes and reproduce independently through asexual means, such as through the formation of gemmae. In this study, we investigated independent gametophytes on the Jeju Island of Korea, which was located on the land bridge between East China and Japan during the glacial periods. Fourteen gametophyte populations were collected from seven sites, of which 13 populations were clearly identified as belonging to four fern species known to occur in Jeju Island with BLAST searches using rbcL and trnL‐F sequences. Surprisingly, the last remaining population constituted undescribed taxa in Korea. We presented the first report of the independent gametophytes of Antrophyum obovatum Baker which has not been previously recorded in Korea. It has been supposed that many ferns sought suitable habitat throughout the land bridge between China and Japan. However, Jeju Island might be unsuitable for vittarioid ferns that prefer a tropical or subtropical environment. Consequently, only two species of vittariod ferns (A. obovatum and Haplopteris flexuosa (Fée) E.H. Crane) in the form of a gametophyte and sporophyte, respectively, exist on Jeju Island. Therefore, this gametophyte population must be protected and managed from a conservation perspective. In the case of the independent gametophyte of Hymenophyllum wrightii Bosch, haplotype analysis was conducted based on the rbcL sequences and the result supported that the North American populations were migrated from Japan through land bridge during the glacial periods and Jeju populations were recently established by long‐distance dispersal of the Japanese populations.     

奇异变形杆菌中基因岛介导的多重耐药传播研究进展

奇异变形杆菌是导致医院内感染的重要条件致病菌,广泛分布于自然环境及人和动物的肠道中。基因岛是细菌染色体上约10-200 kb独立的DNA片段,能促进宿主细菌适应复杂多变的环境,与细菌适应性进化密切相关。近年来在奇异变形杆菌基因组中发现了多个与多重耐药密切相关的基因岛,包括沙门菌基因岛1及其相关基因岛、SXT/R391整合性接合元件、PmGRI1等,表明基因岛在奇异变形杆菌多重耐药形成和传播中具有重要作用。本文对奇异变形杆菌中与耐药相关基因岛的结构特征、传播机制、流行情况等进行综述,以期为奇异变形杆菌中多重耐药相关基因岛的深入研究提供参考。     

长白山林线过渡带树岛土壤微生物群落结构和生态功能

林线过渡带是指从郁闭森林上限到树种分布上限之间的区域,过渡带内生物多样性丰富,生态系统结构、功能和生态过程在很小的海拔梯度内发生剧烈变化,因此对全球气候变化和人类活动极为敏感。树岛是在林线过渡带内出现的斑块状或条带形不连续分布的树木集群,树岛内生存的树木通常能达到与较低海拔郁闭森林同样的高度和胸径,因此揭示树岛这一特殊生境的生态特征及其形成机制,对于预测未来气候变化下林线动态具有重要意义。以长白山岳桦林线过渡带一大型树岛作为研究对象,测定了土壤理化性质和土壤酶活性,采用宏基因组测序技术分析了微生物群落结构组成和功能基因丰度,通过与同海拔的开阔区生境进行对比,揭示了树岛这一特殊生境的土壤微生物群落结构特征和潜在生态功能,从土壤养分和土壤微生物学角度,阐明树岛形成的可能驱动机制。结果表明,树岛土壤的含水量、总碳、总氮和微生物生物量显著高于同海拔开阔区（P<0.05）,与微生物r-策略相关的生理生化和遗传学指标,包括纤维素酶活性、放线菌相对丰度、与转录、防御、控制细胞周期相关的基因丰度、小分子碳降解基因丰度,均高于开阔区（P<0.05）。相反的,与微生物K-策略相关的指标,包括酸杆菌相对丰度、大分子碳降解基因相对丰度低于开阔区。揭示了树岛土壤微生物学特征,并从土壤微生物组学角度探讨了树岛形成的潜在机制,认为树岛内土壤养分增加并导致微生物群落r-策略倾向,这种变化反过来也可能促进树岛进一步扩大,进而影响林线动态。     

区域气候背景对城市热岛效应的影响规律

城市热岛效应受到区域气候背景的影响而具有显著的时空差异性,尚缺少大尺度对比研究。利用1991-2019年的月均气象数据,量化了我国69个典型城市的大气城市热岛效应强度,从热带、干带、暖温带、冷温带和极地带五个气候带,分析城市热岛效应的时空特征规律。结果表明：（1）区域差异：干带热岛效应明显高于其他气候带,极地带最弱,且表现为较强的冷岛效应,热带、暖温带、冷温带热岛效应较弱,而冷温带的京津冀地区由于城市化程度较高,表现出较强的热岛效应,温暖带中西南地区较为明显;（2）季节性差异：不同季节城市热岛效应的强弱关系在不同气候带有所不同,秋季热岛效应较为稳定,热岛和冷岛效应均主要处于弱强度范围,春、冬热岛效应较为波动,易出现强热岛、强冷岛效应的极端现象,夏季热岛效应发生率最高;（3）时间演变规律：城市热岛效应的多年演变规律在相同气候带较为一致,2010年前后是各气候带各季节城市热岛效应的变化拐点,2010年后,干带、冷温带、暖温带热岛效应均有所下降,热带、极地带有所上升。     

基于增强回归树与区域增温敏感性指数的城市升温效应空间分异

热岛效应已成为城市化进程中备受关注的城市生态环境问题。有关城市热岛效应的研究对区域在地表升温过程中的空间分异关注尚不足。通过设计区域增温敏感性指数,借助增强回归树（boosted regression tree,BRT）机器学习算法,量化城市不同区域在地表升温过程中的敏感性差异。结果表明：（1）上海市各辖区增温敏感性从高至低依次是：黄浦区、杨浦区、虹口区、静安区、普陀区、徐汇区、长宁区、宝山区、闵行区、浦东新区、嘉定区、奉贤区、松江区、青浦区、金山区、崇明区;（2）区域增温敏感性在不同的温度梯度下具有明显差异,在高温梯度下区域间指数值的差异最大;（3）地表覆被的增温敏感性存在明显的区域分异特性;（4）基于BRT的增温敏感性指数具有较好的指示意义和较高的灵敏度。在城市热环境持续恶化背景下,探讨城市异质空间中地表温度变化的敏感性可为城市热环境调控提供科学依据。     

绿色基础设施的生态及社会功能研究进展

随着城市化进程的加快,城市硬化地表不断挤占透水表面,使得绿色基础设施规模不断下降、破碎化程度逐渐加大,严重影响了绿色基础设施服务功能的有效发挥。绿色基础设施的发展经历了早期萌芽、初步形成和快速发展三个阶段,主要在宏观尺度研究区域生态安全,中观尺度促进城市可持续发展,微观尺度解决社区生态环境问题。目前绿色基础设施的研究内容集中在其生态功能和社会功能两个方面,主要关注调蓄降雨径流、消减非点源污染、调节区域微气候、居民健康与福祉和空间布局公平性。而供需结构的合理配置也是决定绿色基础设施服务水平的关键因素。未来的研究应加强与相关学科的交叉融合,完善绿色基础设施功能的测度与评估方法,将绿色基础设施建设与实际规划相结合,以期为区域可持续发展和国家生态文明建设提供支撑与保障。     

Le Paléolithique supérieur dans l’île d’Hokkaïdo

Since the discovery of the first Paleolithic site in Hokkaido, we consider that the time in the half more than centuries already passed, and float today. However, our research is still a way. By today, we have not discovered the trace about a Pithecantropines (Homo erectus) and a Paleanthropic man (Homo sapiens neanderthalensis) at all in this region. We know that a Neanthropic man (Homo sapiens sapiens) dominated all the continents except Antarctica in the final time of the Pleistocene era. And they passed along the dried shoal which appeared to the north in the same time from the Asian Continent to the Island of Hokkaido, and reached it to this place. The first attainment time is an age which exceeds 20,000-years before a little from the present. We are not checking a fact which exceeds it you to be much. However, the habitants of these beginnings left the trace of the activity of them in large numbers, so that he was wonderful to inside of this island. The studies-of-prehistory research in Hokkaido has little proof of the natural science field concerned on age determination or chronology. This has serious restriction. However, the tephra-chronology of volcanic ashes has played the big role uniquely. The eruption of the Eniwa volcano of the Hokkaido central part is especially a very important index. This volcano blows off ash fall (En-a) in large quantities, and covered all large ranges. This deposited volcanic-ashes layer plays a big role to discernment of an old industry and a recent industry on the cultural chronology. The obsidian from this island and nearby hard shale was used for many industries of this Upper Paleolithic cultures as main materials. Although obsidians in the island where the different four outcrops are known well. This rock was mined in large quantities, and was carried in various places. As well as many examples in the world, we divided this rock, and the human beings of the prehistoric age were demanded for it, and it was often utilized. In it, especially the outcrop of Shirataki was located in the northern part of Hokkaido, and was very important. Large quantities of obsidian from Shirataki outcrop is discovered in a large number of Paleolithic sites within a segment 700 km in diameter at least. It covered the territory in Hokkaido and circulated further also except this island. This fact circulated as important trade materials on stone-tool fabrication among the human-beings groups from whom this island's every place differed. In this time, human beings’ activity in Hokkaido is a clear proof, which was not isolated at all. As for the studies of the prehistorians of Hokkaido distinguish, the exception put the technical process of eight different microblade productions. The technical process of some of them was limited only to the specific narrow area. Or it is proved that other technical processes are widely connected with the human-beings group of the Asian Continent on the contrary. At present, our research grasps the whole second-half Paleolithic culture, and has not yet established the year system edited by locally complete. The oldest industry of this area composed the typical stone tool of second-half Paleolithic culture from the beginning, and was accompanied by the manufacturing technique of a braid and microblade. The feature is the example in which the ruins of Kashiwadai-I were most excellent. These ruins correspond at time older than deposition of the Eniwa volcano tephra. It is located at the chill time in the second half of a Würm glacial period. The second continuing step is an industry of succession newer than this volcano tephra. It is raised as an example with Ôsatsu-16 typical ruins etc. The third phase is an industry of the end term of second-half Paleolithic culture. It is simultaneously located in the dawn of Jōmon culture. The feature of this cultural aspect is a transitional cultural stage which earthenware appears and is called what is called “Sub-Neolithic-Culture”. We can check having passed expansively, while the aspect of this last continues within a short period of time relatively.