南方丝绸之路对大理的影响及当前的对策

大理历史悠久,文化灿烂,风光秀丽,古道纵横。过去南方丝绸之路对大理的经济、政治、交通、文化、宗教等有较大的影响,今天在国家"一带一路"的大战略背景下,大理应该怎么办,大理学院应该怎么办,这是当代学人的新课题。以古代南方丝绸之路为出发点,建议今天大理的"一带一路"定位为交往之路、人情之路。     

西秦岭南带中志留统的岩石学特征与沉积环境

详细研究了西秦岭南带中志留统岩石学特征,对遭受重结晶作用的碳酸盐岩进行了结构成因分类。分析了该区中志留世的沉积环境及变化特征。在该区发现的层孔虫生物礁及其它“浅水”标志,表明志留纪时,为若尔盖微古陆北侧的边缘浅海环境。西部为局限陆棚环境,可分为:局限内陆棚、海湾、礁滩-泻湖-潮坪(孤立台地)等亚环境;东部为开阔陆棚环境,可分为浅海砂滩、内陆棚、外陆棚等亚环境。     

秦岭地区两栖爬行动物区系组成特点及持续发展对策

对秦岭地区内１１个县的两栖爬行动物进行了调查研究。该区共有两栖爬行动物６０种（亚种）,占陕西省总种数的７５．０％。其中两栖动物１９种,隶２目７科１２属;爬行动物４１种,分隶２目８科２６属。该区两栖爬行动物区系组成以东洋界华中区或华中－华南区共有种类为主,也有一定数量的广布种和古北界华北区种类,还有少量东洋界西南区种类,并就秦岭地区的两栖爬行动物资源现状提出了５项可持续发展对策。     

秦岭藓类植物分布新纪录

通过野外采集和室内鉴定，发现了秦岭藓类植物一个新纪录科白发藓科Leucobryaceae和一个新纪录属青毛藓属Dicranodontium，经分析资料表明，包氏白发藓Leucobryum bowringii Mitt．为热带和亚热带的种类，秦岭是迄今发现的该种分布的北部边缘，它在秦岭的发现对秦岭植物区系划分具有特殊意义，同时也为秦岭藓类植物研究提供了资料。     

秦岭水文特征及其对泥石流影响的初步分析

通过对秦岭山地区域水文特征的分析，指出秦岭泥石流的暴发期与该区降雨的年内集中期相一致，其分布与暴雨中心密切相关。其中，暴雨、连阴雨是产生泥石流的激发因素，径流的汇集及河流洪水亦是导致泥石流发生的重要原因之一。     

东秦岭松树沟长英质高压麻粒岩的原岩性质

地球化学特征研究表明,东秦岭松树沟长英质高压麻粒岩的原岩性质主体为杂砂岩或长石砂岩,少量为亚碱性的酸性火山岩或岩浆岩并具慢源成因;其古构造环境类似于活动大陆边缘。     

秦岭北坡森林公园游憩价值测评

根据秦岭北坡森林公园为陕西省森林生态旅游活动的主体，而森林公园游憩价值又是非市场性的，这就需要探索新的方法来进行计量测评．基于意愿支付假设，在广泛调查的基础上，采用旅行费用法(TCM)对秦岭北坡森林公园的游憩价值进行了测评．结果显示，13个森林公园的年游憩价值合计为14140．4万元，这就为秦岭北坡森林公园产业带的生态旅游开发及经济评价提供了参考依据．     

华南黑色岩系铂多金属矿成矿流体地球化学及其矿床成因意义

较系统的流体包裹体观测显示:①华南黑色岩系铂多金属矿中存在两种不同体系的流体包裹体,一为具中低盐度、NaCl-H2O体系者(Ⅰ型);二为具中高盐度、CaCl2-NaCl-H2O体系者(Ⅱ型);其中后者为该类矿床中首次确定;②存在2个不同期次的成矿流体,其中铂多金属矿层和其下伏磷块岩中碳酸盐石英网脉的流体包裹体特征基本一致,可能代表主成矿期流体,其均一温度峰值为170℃左右,而盐度具双峰式特征,峰值分别为27%～31%和4%～6%;矿层之上碳酸盐石英脉中流体包裹体可能代表了晚期成矿流体,其均一温度多为130～170℃左右,盐度峰值在12%～14%;③在早寒武世,接受了巨厚沉积的扬子克拉通南缘加里东冒地槽中的盆地热卤水受挤压而顺层侧向迁移,从地层中汲取Ni、Mo、V和PGE等成矿元素,形成中高盐度的CaCl2-NaCl-H2O体系成矿热液,沿断裂上升并与NaCl-H2O体系海水混合,形成黑色岩系中的铂多金属矿床(点).     

南宋雅词之探

雅俗之辨是中国古代文学史上一个争议颇多的话题。宋词作为一代文学样式，在雅俗的演变上更有其特点。南宋词坛经过自北宋以来的长期探索与辨析，在词的雅化之路上逐渐形成了自己的理论。内容上反对淫艳猥亵，提倡骚雅；风格上“涉谐谑”、“鄙俗”、“侧艳”则去之；在词体源头的探求上，认为诗词同源，推尊词体；语言和音律求雅，反对俚俗。姜夔、张炎、王沂孙等是南宋雅词的代表。通过南宋词学的雅俗之辨，词的创作发生了根本变化，词人的创作规范化、理性化了，人们认可了词这种文学体裁，并使词体定型，渐成为与诗比肩的一种文体。     

Response of the northwestern Pacific upper water δ~(13)C to the last deglacial ventilation of the deep Southern Ocean

The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes.