2001—2020年川西北高原归一化植被指数演变特征及其对极端气候的响应

川西北高原是典型的生态气候敏感区,其植被状况与气候变化密切相关。本研究基于2001—2020年MODIS-NDVI数据集和气象数据,采用最大值合成、地理探测器模型、线性趋势分析、相关分析等方法,研究川西北高原生长季归一化植被指数(NDVI)的变化趋势及其对气候因子的响应机制。结果表明: 研究期间,川西北高原植被覆盖度整体状况良好,86.8%的区域植被稳定,12.6%的区域NDVI呈弱持续性上升趋势,0.6%的区域NDVI呈下降趋势,全区生态环境呈稳中向好的发展趋势。研究区植被覆盖度空间差异大,总体呈由西南向东北上升的趋势,并有显著的立体变化。海拔1350 m以下,NDVI随海拔升高而上升;海拔1350～3650 m,NDVI无显著变化;海拔3650～5900 m,NDVI随海拔升高而下降,在4750～5900 m快速下降;海拔5900 m以上,几乎无植被。川西北高原的NDVI受多种自然因子交互作用影响,热量因子(月最高气温极大值、月最低气温极小值、植物生长期、年均温、生长期均温)是主导气候因子,除月最高气温极大值外,其余温度因子对NDVI均以正贡献为主。NDVI对气温指数的响应高于降水指数。在气候变暖背景下,极端气温暖指数对川西北高原植被生长尤其是高海拔地区植被生长及改善以促进作用为主。     

中国西藏发现类三角蚌类祖先闯入非海相领域的证据（英文）北大核心CSCD

新发现的双壳类化石命名为Baxoitrigonia baxoiensis gen. et sp. nov.,产地为藏东八宿林卡家东,化石产于景星动物群之下的拉贡塘组下段,同层位有菊石和其他海相双壳类,时代为晚侏罗世Tithonian期;化石的外部特征很接近于三角蛤类Iotrigonia属,但前闭肌痕特征又相似于类三角蚌类,被认为是三角蛤类闯入非海相领域后演变成类三角蚌类的产物。此发现提供了生物和地层两方面的直接证据,证明非海相类三角蚌类(Trigonioidoidea超科)起源于海相三角蛤类(Trigoniida目),而不是起源于珠蚌类(Unionida目)。海相三角蛤类闯入边缘隔绝的洛隆-八宿地区并演变为非海相类三角蚌类,是一次典型的边域成种事件。     

黄土高原马栏林区不同森林类型的土壤肥力研究

用灰色关联分析法对黄土高原马栏林区主要森林类型优势层生长状况与土壤养分因子的关联性进行分析,并对土壤肥力进行评价。结果表明腐殖质层和有机质是影响森林乔木层生长的主导土壤因子,其次是全氮和碱解氮,然后依次为速效钾、速效磷、全磷、pH值。土壤肥力的综合评价排序总体结果显示,辽东栎占优势的林型肥力最高,油松林、山杨占优势的混交林居中,辽东栎+白桦混交林较差,而白桦占优势的混交林最差。人工油松林对土壤有一定的改良作用;而多数混交林的土壤肥力高于以其中某一树种占优势的林型,但以辽东栎为优势种的林型比辽东栎混交林土壤肥力高,且辽东栎的重要值百分数越大,其土壤肥力越高。     

藏北申扎地区下石炭统永珠组下部孢子组合的特征及意义

报道藏北申扎永珠区德日昂玛—下拉剖面的永珠组孢子组合,发现孢子43属,70余种(包括未定种)。组合特征如下:1)缺乏欧美植物地理区早石炭世典型的石松类植物的小孢子Lycospora属及早石炭世晚期(维宪期)重要孢子属;2)出现较多早石炭世早期(杜内期),甚至泥盆纪晚期分子。呈现出新老化石的混合现象;3)北半球和南半球孢子的混合组合,同时也是冷、暖微古植物群混合,既有相当于中国早石炭世晚期大塘期以及西欧维宪期典型属种,又有南半球澳大利亚(包括巴西和非洲大陆)的维宪期的典型种。从孢子化石混合现象看,永珠组应为近岸浅水或滨海条件下的沉积,下伏地层的孢子化石再沉积现象说明当时有一次很大的海平面下降,在邻近地区出现了大面积的剥蚀区。说明杜内期末期—维宪期初期,申扎地区出现一次由冈瓦纳大陆冰川发育造成海平面相对下降。形成区域上不整合界面———洛工组或“巴日阿朗寨段”底部的不整合界面。混合孢子组合中的寒冷气候条件下的孢子化石的发现,印证了杨式溥、范影年和林宝玉推断的冈瓦纳冰川自早石炭世维宪期(大塘期)开始就影响到西藏申扎的推论。     

青藏高原丽蝇科昆虫物种多样性初探

本文从种数、特有物种和区系构成等角度分析了青藏高原丽蝇科昆虫的物种多样性。青藏高原已知丽蝇5亚科35属120种,占中国已知种数的44.28%,其中特有种55种,占该地区总种数的45.83%;区系构成以特有种、古北界 东洋界共同种及典型的东洋界种和古北界种为主,但澳洲界、新北界、非洲界和新热带界共同种也占一定比例。文中讨论了该地区特有种丰富的原因及地质历史环境对其的影响,分析了区系构成中各种区系成分的比例及形成原因。     

Migration patterns of Gentiana crassicaulis,an alpine gentian endemic to the Himalaya–Hengduan Mountains

The Himalaya–Hengduan Mountain region is one of the hotspots of biodiversity research. The uplift of the Qinghai–Tibetan Plateau (QTP) and the Quaternary glaciation caused great environmental changes in this region, and the responses of many species in the QTP to the Quaternary climate are still largely unknown. The genetic structure and phylogeographical history of Gentiana crassicaulis Duthie ex Burk, an endemic Chinese alpine species in this area, were investigated based on four chloroplast fragments and internal transcribed spacer region of the nuclear ribosomal DNA (nrITS) sequences of 11 populations. The populations with highly diverse chloroplast haplotypes were mainly found at the edge of the QTP. There were two main haplotypes of nrITS clones, one shared by the Yunnan and Guizhou populations, and the other by the remaining populations. The population with the highest diversity was the Gansu population, located at the edge of the plateau. Based on molecular dating, the diversification of G. crassicaulis at the edge of the plateau occurred before the Last Glacial Maximum (LGM), and the species may have completed its expansion from the edge to the platform. Ecological niche models were conducted to predict the distributional ranges of G. crassicaulis at present, during the LGM, and during the last interglacial (LIG) period. The results demonstrated that G. crassicaulis survived on the QTP platform and at the edge during the LGM but afterward retreated from the platform to the southern edge, followed by expansion to the platform.     

高原鼠兔冷驯化和脱冷驯化中的产热变化

本文探讨了冷驯化和脱冷驯化对高原鼠兔代谢产热的影响。在冷驯化中，鼠兔的静止代谢率逐渐增加，血清Ｔ３‘／Ｔ４比率上升，肝线粒体状态３呼吸明显增加，线粒体细胞色素Ｃ氧化酶激活，而肝脏线粒体蛋白含量没有明显变化。     

黄土高原植被恢复的水分生态环境研究

水分是制约黄土高原地区植被恢复与生态环境重建的决定性因子,在分析现有关于该区植被建设中的水分生态环境的各项研究的基础上,从水资源,土壤水分背景,土壤水分动态,土壤干层,土壤水分的林草生产力,水分性质分区,林草对策等7个方面,对黄土高原的土壤水分环境进行了阐述,针对该问题的研究现状,指出其中存在的问题,并对今后的研究进展了展望。     

Contrasting responses to Pleistocene climate changes: a case study of two sister species Allium cyathophorum and A. spicata (Amaryllidaceae) distributed in the eastern and western Qinghai–Tibet Plateau

It has been hypothesized that species occurring in the eastern and the western Qinghai–Tibet Plateau (QTP) responded differently to climate changes during the Pleistocene. Here, we test this hypothesis by phylogeographic analysis of two sister species, Allium cyathophorum and A. spicata. We sequenced two chloroplast DNA (cpDNA) fragments (accD‐psaI and the rpl16 intron) of 150 individuals, and the nuclear (ITS) region of 114 individuals, from 19 populations throughout the distributional ranges of these species. The divergence between the two species was dated at 779 ‐ 714 thousand years before the present and was likely initiated by the most major glaciation in the QTP. Analysis of chlorotype diversity showed that A. spicata, the species occurring in the western QTP, contains much lower genetic diversity (0.25) than A. cyathophorum (0.93), which is distributed in the eastern QTP. Moreover, multiple independent tests suggested that the A. spicata population had expanded recently, while no such expansion was detected in A. cyathophorum, indicating a contrasting pattern of responses to Pleistocene climate changes. These findings highlight the importance of geographical topography in determining how species responded to the climate changes that took place in the QTP during the Pleistocene.