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.     

Patterns of above- and belowground biomass allocation in China’s grasslands: Evidence from individual-level observations

Above- and belowground biomass allocation not only influences growth of individual plants, but also influences vegetation structures and functions, and consequently impacts soil carbon input as well as terrestrial ecosystem carbon cycling. However, due to sampling difficulties, a considerable amount of uncertainty remains about the root: shoot ratio (R/S), a key parameter for models of terrestrial ecosystem carbon cycling. We investigated biomass allocation patterns across a broad spatial scale. We collected data on individual plant biomass and systematically sampled along a transect across the temperate grasslands in Inner Mongolia as well as in the alpine grasslands on the Tibetan Plateau. Our results indicated that the median of R/S for herbaceous species was 0.78 in China’s grasslands as a whole. R/S was significantly higher in temperate grasslands than in alpine grasslands (0.84 vs. 0.65). The slope of the allometric relationship between above- and belowground biomass was steeper for temperate grasslands than for alpine. Our results did not support the hypothesis that aboveground biomass scales isometrically with belowground biomass. The R/S in China’s grasslands was not significantly correlated with mean annual temperature (MAT) or mean annual precipitation (MAP). Moreover, comparisons of our results with previous findings indicated a large difference between R/S data from individual plants and communities. This might be mainly caused by the underestimation of R/S at the individual level as a result of an inevitable loss of fine roots and the overestimation of R/S in community-level surveys due to grazing and difficulties in identifying dead roots. Our findings suggest that root biomass in grasslands tended to have been overestimated in previous reports of R/S.     

Survival of Rio Grande Wild Turkeys on the Edwards Plateau of Texas

Abstract: The southeastern portion of the Edwards Plateau of Texas, historically a stronghold of Rio Grande wild turkeys (Meleagris gallopavo intermedia), has seen a decline in turkey numbers since the 1970s. Because adult and juvenile survival are key parameters affecting turkey population dynamics, we used radiotagged individuals to compare Rio Grande wild turkey survival in areas of suspected decline versus stable portions of the Edwards Plateau during 2001–2003. Reproductive period (breeding or nonbreeding) had an impact on survival, but differences in age, sex, or region did not influence survival. Model averaged estimates of monthly survival were 0.97 (SE = 0.005) for nonbreeding periods and 0.96 (SE = 0.007) for breeding periods. Our results indicate juvenile and adult survival in the declining areas was similar to survival in the stable areas of the Edwards Plateau. This suggests causes of the decline might be associated with differences during other life-history stages, such as nest success or poult survival, although we cannot rule out the possibility juvenile or adult survival contributed to the decline in the past. This situation demonstrates why wildlife managers should be cognizant of the implications of initiating long-term monitoring programs after changes in population status occur, rather than initiating them in expectation of such changes.     

鄂尔多斯高原蒙古族食用野生植物传统知识的研究

运用民族植物学＂5W＋1H＂提问法,结合访谈方法和野外调查进行编目,研究了鄂尔多斯高原蒙古族食用野生植物的传统知识。结果：1）鄂尔多斯蒙古族传统食用植物22科32属50种,其中野生粮用植物14种、野生蔬菜13种、野果植物18种、野果酒植物3种、野生调味植物5种、野生薰净植物2种、催化乳制品植物1种。2）鄂尔多斯蒙古族野生食用植物传统知识包括7个方面,其中用植物薰净和消毒奶食器具的传统知识、用冷蒿催化加速油脂成分从奶子中分离的传统知识是蒙古族植物饮食文化的创新。具有鲜明的民族特色、简单、快捷的＂果实＋奶食＂酿果酒文化,能够说明蒙古族祖先在生产实践中掌握了开发和利用植物资源的更高水平的技术和文化。食用芨芨草颖果、选用中间锦鸡儿韧皮部和白沙蒿的果实做面食粘合剂的传统知识是区域特色的文化。3）因生态环境条件的不同,山区、沙区、盐渍区和丘陵区蒙古族牧民的传统食用植物知识表现出多样性,反映了生态环境条件的多样性。4）鄂尔多斯蒙古族野生食用植物传统知识丰富了蒙古族饮食文化,对蒙古族文化的发展做出了贡献。开展搜集、研究、保护和科学分析鄂尔多斯蒙古族植物传统知识的工作,将对社会经济的可持续发展产生十分积极的直接影响。     

Mitochondrial and chloroplast phylogeography of Picea crassifolia Kom. (Pinaceae) in the Qinghai-Tibetan Plateau and adjacent highlands

The disjunct distribution of forests in the Qinghai-Tibetan Plateau (QTP) and adjacent Helan Shan and Daqing Shan highlands provides an excellent model to examine vegetation shifts, glacial refugia and gene flow of key species in this complex landscape region in response to past climatic oscillations and human disturbance. In this study, we examined maternally inherited mitochondrial DNA (nad1 intron b/c and nad5 intron 1) and paternally inherited chloroplast DNA (trnC-trnD) sequence variation within a dominant forest species, Picea crassifolia Kom. We recovered nine mitotypes and two chlorotypes in a survey of 442 individuals from 32 populations sampled throughout the species' range. Significant mitochondrial DNA population subdivision was detected (G(ST) = 0.512; N(ST) = 0.679), suggesting low levels of recurrent gene flow through seeds among populations and significant phylogeographical structure (N(ST) > GST, P < 0.05). Plateau haplotypes differed in sequence from those in the adjacent highlands, suggesting a long period of allopatric fragmentation between the species in the two regions and the presence of independent refugia in each region during Quaternary glaciations. On the QTP platform, all but one of the disjunct populations surveyed were fixed for the same mitotype, while most populations at the plateau edge contained more than one haplotype with the mitotype that was fixed in plateau platform populations always present at high frequency. This distribution pattern suggests that present-day disjunct populations on the QTP platform experienced a common recolonization history. The same phylogeographical pattern, however, was not detected for paternally inherited chloroplast DNA haplotypes. Two chlorotypes were distributed throughout the range of the species with little geographical population differentiation (G(ST) = N(ST) = 0.093). This provides evidence for highly efficient pollen-mediated gene flow among isolated forest patches, both within and between the QTP and adjacent highland populations. A lack of isolation to pollen-mediated gene flow between forests on the QTP and adjacent highlands is surprising given that the Tengger Desert has been a geographical barrier between these two regions for approximately the last 1.8 million years.     

Factors influencing the distribution of Subantarctic deep-sea benthic foraminifera,Campbell and Bounty Plateaux,New Zealand

We investigate the combination of environmental factors that influence the distribution patterns of benthic foraminiferal tests (> 63 μm) in a topographically varied region crossed by both the Subtropical and Subantarctic Fronts, south-east of New Zealand. Seafloor sample sites, extending from outer shelf (50 m) to abyssal (5000 m) depths, are bathed by five different water masses, and receive phytodetritus from Subtropical, Subantarctic and Circumpolar surface water masses. Eight mappable associations are recognised by Q-mode cluster analysis of the benthic foraminiferal census data. Similar associations are identified using cluster analysis based solely on the presence or absence of species. Canonical correspondence analysis and a correlation coefficient matrix were used to relate the faunal data to a set of environmental proxies. These show that factors related to water depth (especially decreasing food supply with increasing depth) are the most significant in determining the overall foraminiferal distribution. Other contributing factors include surface water productivity and its seasonality; bottom water ventilation; energetic state of the benthic boundary layer and resulting substrate texture; and bottom water carbonate corrosiveness. Three shallow-water associations (50–700 m), dominated by Cassidulina carinata, Trifarina angulosa, Globocassidulina canalisuturata, Gavelinopsis praegeri, and Bolivina robusta, occur in coarse substrates on the continental shelf, and on the crests and upper slopes of four seamounts under well-oxygenated, high energy regimes, and high food input. Three mid bathyal to upper abyssal associations (500–3300 m), dominated by Alabaminella weddellensis, C. carinata, and Epistominella exigua, occur in biopelagic sandy mud, beneath a region of strongly seasonal food supply, with their composition influenced by total food flux, ventilation (Oxygen Minimum Zone), and bottom current strength. An unusual lower bathyal association (1200–2100 m), dominated by T. angulosa and Ehrenbergina glabra, occurs in a belt of coarser sandy substrate that runs along the crest of the submarine plateaux slopes beneath the strongly-flowing Subantarctic Front-related currents. A deep abyssal association (3500–5000 m), dominated by Nuttallides umbonifer and Globocassidulina subglobosa, occurs on the abyssal plain beneath oligotrophic lower Circumpolar Water south-east of the Subantarctic Front and is strongly influenced by the cold, carbonate-corrosive conditions.     

不同海拔高原鼠兔个性特征与SERT基因多态性关联

个性特征是指动物个体间稳定、可遗传的行为差异,与相关基因多态性有关,反映了动物对环境的适应模式,探究个性相关基因变异,将有助于更好地理解动物对环境的适应与进化机制。本文以高原鼠兔 (Ochotona curzoniae) 为对象,研究了5个不同海拔地区高原鼠兔的个性 (探究性、勇敢性和温顺性) 差异特征,并检测了个性相关基因5-羟色胺转运体 (SERT) 的单核苷酸多态性 (SNP) 和mRNA表达。结果发现,高海拔地区高原鼠兔的探究性和勇敢性显著高于低海拔地区,而高海拔地区高原鼠兔SERT基因mRNA表达量显著低于低海拔地区,提示不同海拔高原鼠兔个性特征差异可能与SERT基因mRNA表达有所关联。进一步检测不同海拔地区高原鼠兔SERT基因多态性及其分布差异情况,发现该基因存在6个SNP (其中5个位于外显子3,1个位于外显子5 );不同海拔地区鼠兔基因分布差异分析显示外显子5的c.A1063C 同义突变与海拔之间存在显著相关,高海拔地区该位点CC基因型分布频率显著高于低海拔地区;c.A1063C的基因型虽然与探究性、勇敢性无显著相关,但与温顺性显著相关。综上所述,随着海拔升高,高原鼠兔探究性和勇敢性增加,这有利于动物获取更多的食物资源,进而增加其生存机会。与此同时,SERT基因多态性显示与不同海拔地区的生存环境相适应的特征,且与温顺性有关,暗示不同海拔高原鼠兔个性差异可能与SERT基因SNP的差异有关。本研究从基因表达与突变的角度尝试阐述高原鼠兔适应不同海拔环境的行为差异,显示了不同海拔地区高原鼠兔行为生存策略潜在的分子机制。     

MTNR1a和MTNR1b基因在繁殖期与非繁殖期雄性高原鼢鼠HPG轴上的表达

高原鼢鼠 (Eospalax baileyi) 终年营地下生活,感光受洞道限制,但褪黑素 (Melatonin) 分泌水平仍存有季节差异,为探明褪黑素对高原鼢鼠季节性繁殖的调控作用,研究利用q?PCR技术检测雄性高原鼢鼠繁殖期 (5月) 和非繁殖期 (9月) 下丘脑、垂体及睾丸中褪黑素受体1a (Melatonin receptor 1a, MTNR1a) 和褪黑素受体1b (Melatonin receptor 1b, MTNR1b) 基因mRNA的相对表达量,通过免疫组织化学技术对MTNR1a和MTNR1b在睾丸中定位,并采用Image Pro Plus软件进行免疫组化阳性评价。结果发现,高原鼢鼠繁殖期下丘脑和垂体中MTNR1a基因的相对表达量显著高于非繁殖期的相对表达量 (P < 0.05),MTNR1b基因的相对表达量在不同时期无显著差异 (P > 0.05),但非繁殖期睾丸中MTNR1a和MTNR1b基因的相对表达量均显著高于繁殖期 (P < 0.01);繁殖期除长形精子外的所有类型细胞以及非繁殖期的间质细胞、支持细胞和精原细胞中均观察到MTNR1a的阳性信号,繁殖期除精原细胞和长形精子细胞外的所有类型细胞,以及非繁殖期间质细胞和支持细胞中均观察到MTNR1b的阳性信号,且非繁殖期MTNR1a和MTNR1b的平均光密度值均显著高于繁殖期 (P < 0.01)。MTNR1a和MTNR1b基因在雄性高原鼢鼠HPG轴上的表达模式,提示了褪黑素在其季节性繁殖调控中的潜在作用。