Tibetan land use and change near khawa karpo, Eastern Himalayas

Collaborating Authors: Bee Gunn, Wayne Law, George Yatskievych, Wu Sugong, Fang Zhendong, Ma Jian, Wang Yuhua, Andrew Willson, Peng Shengjing, Zhang Chuanling, Sun Hongyan, Meng Zhengui, Liu Lin, Senam Dorji, Ana, Liqing Wangcuo, Sila Cili, Adu, Naji, Amu, Sila Cimu, Sila Lamu, Lurong Pingding, Zhima Yongzong, Loangbao, Bianma Cimu, Gerong Cili, Wang Kai, Sila Pingchu, Axima, and Benjamin Staver.TIBETAN LAND USE AND CHANGE NEAR KHAWA KARPO, EASTERN HIMALAYAS. Economic Botany 59(4):312-325, 2005. Tibetan land use near Khawa Karpo, Northwest Yunnan, China, incorporates indigenous forest management, gathering, pastoralism, and agriculture. With field-based GIS, repeat photography, and Participatory Rural Appraisal we quantitatively compare land use between higher and lower villages, and between villages with and without roads. Households in higher elevation (> 3,000 meters) villages cultivate more farmland (z = -5.387, P ≤ 0.001), a greater diversity of major crops (z = -5.760, P < 0.001), a higher percentage of traditional crops, and fewer cash crops (z = -2.430, P = 0.015) than those in lower elevation villages (< 2,500 meters). Villages with roads grow significantly more cash crops (z = -6.794, P ≤ 0.001). Both lower villages and villages with roads travel farther to access common property resources. Historical analyses indicate agricultural intensification in valleys, an increase in houses, new crop introduction, hillside aforestation, cessation of hunting, glacial retreat, and timberline advance within the past century. We suggest that Tibetan land use reveals trade-offs between high, remote villages and lower villages near roads. Higher villages offer abundant land and access to natural resources but short growing seasons and little market access; in contrast, lower villages have road and market access, an extended growing season, and modern technology, but limited access to land and many other natural resources.     

利用遥感信息研究西藏地区主要植被年内和年际变化规律

利用1982～2000年NOAA-AVHRR月合成NDVI遥感资料和相关气象台站数据对我国西藏地区的稀疏草地、浓密草地和Tebit森林等主要植被的变化进行了初探。利用月合成NDVI的多年平均值分析了植被指数年内季节性变化规律及其与气候因子的关系,利用多年月合成NDVI的标准差描述了NDVI年际间波动情况。结果表明,在西藏地区,浓密草地和Tebit森林的NDVI植被指数年内变化规律呈明显的季节性,而稀疏草地则不明显;在年际变化方面,浓密草地月合成NDVI值波动幅度最大,Tebit森林次之,稀疏草地最小,且波动幅度较大的月份集中在NDVI值较高的植被生长季节6～10月份。     

西藏南部定日、聂拉木地区早-中侏罗世有孔虫

记述早、中侏罗世有孔虫13属17种,标本采自西藏南部定日县的卧龙剖面及聂拉木县中尼公路5264km路标处剖面。早侏罗世普普嘎组以产大有孔虫为特征,在卧龙剖面仅有下侏罗统的中、上部,缺失下部地层;中侏罗世聂聂雄拉组以产小有孔虫为特征,基本没有大有孔虫。     

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。     

F1代西藏小型猪早期生长发育特点

目的研究西藏小型猪早期生长发育的规律。方法对本基地F1代西藏小型猪的体重、体长、胸围、体高、体温、呼吸频率、心率及血液生理生化指标进行了测定。结果西藏小型猪体型小,生长性能稳定,生长速度与原产地西藏小型猪基本一致;西藏小型猪的体温、呼吸次数和心率与原产地西藏小型猪相近,且雌雄之间差异不显著(P>0.05);F1代雌雄间除嗜碱性粒细胞、单核细胞数和尿素氮外其他指标也基本一致,大部分指标与人接近。结论由于西藏小型猪体型小、生长性能稳定,血液生理生化值与人类相近,因而是理想的医学研究用实验动物。     

西藏小型猪线粒体D-loop区及微卫星多态性的遗传学分析

目的通过分析西藏小型猪线粒体控制区(D-loop区)及微卫星位点的遗传多态性,检测西藏小型猪的遗传背景,从而为其作为实验动物提供分子生物学方面的可靠依据。方法利用特异性引物对西藏小型猪的线粒体D-loop区及10个具有多态性的微卫星位点进行扩增,割胶纯化并对线粒体D-loop区进行测序,另外采用聚丙烯酰胺凝胶电泳的方法分离微卫星位点的等位基因。结果西藏小型猪线粒体D-loop区全序列没有多态性,微卫星位点则具有高度的遗传多态性和杂合度,分别为0.584和0.573。结论西藏小型猪线粒体基因组无多态性,证明其在母系进化和遗传上与其他猪种较为一致,本实验所用的西藏小型猪生长于一个封闭的环境,导致其微卫星位点遗传多态性的中低度水平。     

Middle Pleistocene ecology and Neanderthal subsistence: Insights from stable isotope analyses in Payre (Ardèche,southeastern France)

The Middle Palaeolithic site of Payre in southeastern France yields abundant archaeological material associated with fossil hominid remains. With its long sequence of Middle Pleistocene deposits, Payre is a key site to study the Middle Palaeolithic chronology of this region. This study is the first to investigate carbon and oxygen isotope contents of Neanderthal tooth enamel bioapatite, together with a wide range of herbivorous and carnivorous species. The aim is to contribute to the understanding of hunting behaviour, resource partitioning, diet and habitat use of animals and Neanderthals through a palaeoecological reconstruction.     

西藏高原云南松生物量模型及碳储量

云南松林是西藏高原亮针叶林生态系统的重要组成部分,准确估算其生态系统碳储量不但有助于弄清西藏森林生态系统固碳现状,而且可为准确估算青藏高原乃至全国森林生态系统的固碳潜力和固碳速率提供基础数据.本研究以云南松为研究对象,采用实地调查与建模相结合的方法,建立了各器官(叶、枝、干、根)与株高、胸径的生物量回归方程,并以此为基础计算了云南松幼龄林、中龄林、近熟林和成熟林生态系统的生物量和碳储量.结果表明:(1)用胸径和树高估测单株林木器官生物量的较优模型为指数模型,所建立的生物量回归方程相关性较好(R2＞0.90),估计精度较高.(2)在云南松幼龄林、中龄林、近熟林和成熟林生态系统中植被总生物量分别为(63.80±9.21)、(134.76+12.69)、(142.91±13.02)、(316.72+42.57)t·hm-2,其中乔木层生物量分别为(49.48±10.32)、(120.57±9.37)、(124.70±12.92)、(304.76±32.47)t·hm-2,灌草层生物量为(13.09±3.02)、(12.81±2.54)、(11.88±3.12)、(3.47±0.98)t·hm-2,凋落物生物量为(1.23±0.24)、(1.38±0.31)、(0.72±0.11)、(1.13±0.39)t·hm-2.(3)各龄级云南松林生态系统植被碳储量分别为(30.67±7.13)、(67.63±19.06)、(71.00±4.15)、(159.32±39.95)t·hm-2,碳储量随林龄增加的变化规律明显,碳汇潜力巨大.     

The Himalayas: Barrier and conduit for gene flow

The Himalayan mountain range is strategically located at the crossroads of the major cultural centers in Asia, the Middle East and Europe. Although previous Y‐chromosome studies indicate that the Himalayas served as a natural barrier for gene flow from the south to the Tibetan plateau, this region is believed to have played an important role as a corridor for human migrations between East and West Eurasia along the ancient Silk Road. To evaluate the effects of the Himalayan mountain range in shaping the maternal lineages of populations residing on either side of the cordillera, we analyzed mitochondrial DNA variation in 344 samples from three Nepalese collections (Newar, Kathmandu and Tamang) and a general population of Tibet. Our results revealed a predominantly East Asian‐specific component in Tibet and Tamang, whereas Newar and Kathmandu are both characterized by a combination of East and South Central Asian lineages. Interestingly, Newar and Kathmandu harbor several deep‐rooted Indian lineages, including M2, R5, and U2, whose coalescent times from this study (U2, >40 kya) and previous reports (M2 and R5, >50 kya) suggest that Nepal was inhabited during the initial peopling of South Central Asia. Comparisons with our previous Y‐chromosome data indicate sex‐biased migrations in Tamang and a founder effect and/or genetic drift in Tamang and Newar. Altogether, our results confirm that while the Himalayas acted as a geographic barrier for human movement from the Indian subcontinent to the Tibetan highland, it also served as a conduit for gene flow between Central and East Asia. Am J Phys Anthropol 151:169–182, 2013. © 2013 Wiley Periodicals, Inc.