Loading...

Table of Content

    24 June 2017, Volume 39 Issue 3
    Invited Special Paper
    Recent discoveries and research progress on pterosaur eggs and embryos
    ZHANG Xinjun, JIANG Shunxing, WANG Xiaolin
    2017, 39(3):  157-165.  doi:10.3969/j.issn.0253-9608.2017.03.001
    Asbtract ( 456 )   PDF (8612KB) ( 371 )  
    Related Articles | Metrics

    Pterosaur researchers speculated that pterosaurs were oviparous for a long time, and they confirmed it based on the three pterosaur eggs and embryos from the Early Cretaceous reported in 2004. Then, a wukongopterid pterosaur associated with two similar-sized eggs, one outside body near the pelvis and the other inside, was discovered in the Yanliao Biota from the Late Jurassic. It indicated that the pterosaur had two functional oviducts, which differed from mostly modern birds. Five three-dimensionallypreserved pterosaur eggs were first reported from the Early Cretaceous in Hami, Xinjiang, China. The eggshell of one egg, observed under scanning electron microscopy, comprises a thin calcareous external hard shell followed by a thick membrane, which is similar to that of the snake Elaphe. It is hopeful to discover some three-dimensional pterosaur eggs with embryos in Hami, which will make a great progress in pterosaur embryology in the future.

    Review Article
    New recognition of water storages and physicochemical property of the lakes on the Tibetan Plateau
    2017, 39(3):  166-172.  doi:10.3969/j.issn.0253-9608.2017.03.002
    Asbtract ( 594 )   PDF (1981KB) ( 503 )  
    Related Articles | Metrics

    There are a large number of lakes distributed on the Tibetan Plateau (TP), which are sensitivic to climatic change. Lakes, as one of the important components of underlying surface on the TP, not only affect the regional climate by land-atmosphere water and energy exchanges, but also record the information of climatic change through sediments. Lake water storage and water physicochemical property are basic factors affecting water and energy exchanges between lake and atmosphere, and lake sedimentary processes. The basic investigation of lake water storage and water physicochemical property on the TP is one of the key issues for deep understanding the responses and influence of TP in the climatic change. Based upon the basic investigations of the lakes on the TP during past 5 years, we have clarified some fuzzy recognition and renewed the basic data of some important lakes. The lake area and water storage of the TP and their changes with climatic change, as well as the spatio-temporal difference, have been elucidated. Further, a new method is introduced to study water physicochemical properties and their changes within the ranges of long time and wide area based upon water color derived from remote sensing images.

    Greening of the Tibetan Plateau and its drivers since 2000
    ZHANG Yili, LI Lanhui, DING Mingjun, ZHENG Du
    2017, 39(3):  173-178.  doi:10.3969/j.issn.0253-9608.2017.03.003
    Asbtract ( 832 )   PDF (2506KB) ( 343 )  
    Related Articles | Metrics

    The Tibetan Plateau (TP), known as an important carrier of ecological shelter in China, even in Asia, has attracted a great of attentions because its ecosystem was very sensitive to global changes. Based on the results of previous studies and the analysis of relevant data, this study aimed to identify the temporal-spatial pattern of the alpine vegetation change and its drivers based on the perspective of climate change and human activities on the TP from 2000 to 2013. The results showed that the coverage of alpine vegetation has slightly increased by 3%-5% on TP since 2000. The vegetation coverage of about 98.34×104 km2 increased, with a significant increase in 16.85×104 km2, distributed mainly on the central and eastern part of the TP. The vegetation coverage of about 5.73×104 km2 decreased, with a significant decrease in 0.18×104 km2, mainly on the central and western part of the Tibet Autonomous Region. Climate warming and moistening and ecological construction are the main factors for the greening of alpine vegetation. However, the role of the increase of human activity intensity and climate warming and drying on vegetation degradation in local area should not be neglected.

    Are treelines advancing in response to climate warming on the Tibetan Plateau?
    WANG Yafeng, LIANG Eryuan, LU Xiaoming, ZHU Haifeng, PIAO Shilong, ZHU Liping
    2017, 39(3):  179-183.  doi:10.3969/j.issn.0253-9608.2017.03.004
    Asbtract ( 592 )   PDF (1807KB) ( 351 )  
    Related Articles | Metrics

    Tree growth at treelines is generally limited by low temperature so that warming tends to shift treeline upward. However, a global meta-analysis showed that treelines shifted upward at around 50% during the last century among the investigated treelines, and others kept static. Such evidence suggested that non-climate factors (such as interspecific competition) apart from climatic factors controlled treeline shift. The Tibetan Plateau hosts the highest treeline in the Northern Hemisphere, being a good locale for investigating climatic and biotic factors influencing treeline changes. As showed by our research, short and sparse shrub and grass acted as“tree nurseries”for recruitment, and benefitted treeline upward shift. Dense shrubs just above treeline inhibited tree establishment, and slowed upward movement of treelines. Climatic warming tended to promote the upward shift of alpine treelines at local and regional scales. However, upslope migration rates were controlled largely by interspecific interactions. Warming may not cause the upward shift of treelines if dense shrub dominate the above treelines.

    Changes of plant phenophases and their effects on the Qinghai-Tibetan Plateau
    MENG Fandong, TSECHOE Dorji, CUI Shu juan, WANG Qi, LI Bowen,WANG Shiping
    2017, 39(3):  184-190.  doi:10.3969/j.issn.0253-9608.2017.03.005
    Asbtract ( 1098 )   PDF (1666KB) ( 533 )  
    Related Articles | Metrics

    Plant phenology is the recurrence of life history events. Impacts of climate change and human activity on phenology weresignificant in the Qinghai-Tibetan  Plateau, and warming and optimal grazing advanced the timings of green-up and flowering but delayed the end date of senescence. However, fruiting time kept relative stable compared with other phenophases. Warming prolonged the duration of plant activity period which was mainly derived from prolonged flowering duration as well as other reproductive phenophases. These changes mainly attributed to changes of temperature, moisture and grazing. Warming and wet, moderate grazing contributed to advance and lengthen phenophases, whereas warming and drought led to delay and shorten phenophases. Changes of
    phenophases had significant influences on structure and function of populations, community, ecosystem and productions and lives of pastoral and tourism. However, there were few studies on phenology, especially the effects of changes of phenology on structure and function of ecosystem on the Tibetan plateau. Therefore, we suggest that we should pay more attentions to effects of climate change and human activity on alpine plant phenology from physiology-level to ecosystem-level, and to feedbacks of phenology on ecosystems in the future.

    Natural Forum
    Big knowledge in small vesicles: preexistence and this life of exosomes
    BEI Yihua, YU Pujiao, XIAO Junjie
    2017, 39(3):  191-200.  doi:10.3969/j.issn.0253-9608.2017.03.006
    Asbtract ( 747 )   PDF (1943KB) ( 580 )  
    Related Articles | Metrics

    Exosomes are endosomes derived extracellular vesicles of 30~100 nm size range, which carry nucleic acid and protein. Exosomes have powerful biological functions. Here we described the discovery and functions of exosomes. In addition, we also summarized the roles of exosomes in cancer growth, metastasis, immune escape, diagnosis, and treatment. Besides, functions of exosomes in a variety of cardiovascular physiological and pathological processes including atherosclerosis, myocardial infarction, ventricular remodeling, and cardiac regeneration are reported. In summary, a big knowledge is contained in these small vesicles.

    Earth origin and continental growth
    WAN Tianfeng
    2017, 39(3):  201-209.  doi:10.3969/j.issn.0253-9608.2017.03.007
    Asbtract ( 723 )   PDF (3036KB) ( 382 )  
    Related Articles | Metrics

    The Earth in the early period (4.5 billion years before)was produced by the accumulation and accretion of the planetesimals, composed largely of the heavier elements, which had previously condensed from the solar nebula. The meteorite impact caused that the earth surface rocks against and crushed, evoked the supercritical fluid or magma uplift from the mantle, formed the violent volcanic eruption and let the volatile component concentrat on the solid earth surface, then let them gradually evolve to the hydrosphere and atmosphere. The oceanic crust was mainly formed by tholeiitic basalt, which was caused by the violent eruption of iron magnesium silicate rocks. The original continental cores were formed by gneiss domes, which may be also caused by the meteorite impact. The lithosphere plates were developed in 1.8~1.6 billion years ago. The strain rates of subductions between oceanic and continental plates or collision between continent and continent plates are all very low, which could be formed the partial fractures. However, the ductile deformation, metamorphism, magmatism and the injection and cooling caused the continents accretion continually. The Asian continental lithosphere plate was formed by 14 subductions or collisions, caused by 27 bigger ancient blocks and about hundreds small blocks from the 1.8 or 1.6 billion years ago to the recent. As to the continent destroyed, it may be caused by mantle plume uplift or giant meteorite impact.

    History of Natural Science
    Magical yeast, ideal model
    GUO Xiaoqiang, HUANG Weiren
    2017, 39(3):  210-221.  doi:10.3969/j.issn.0253-9608.2017.03.008
    Asbtract ( 887 )   PDF (4673KB) ( 438 )  
    Related Articles | Metrics

    Yeast is a unicellular eukaryote and become an important experimental organism in biochemistry, genetics and cell biology on the basis of its many advantages. In vitro experiment, cell-free yeast system plays an important role in enzyme function, enzyme composition, coenzyme characteristics, tRNA structure, eukaryotic transcription, and so on. As a model organism, yeast also played a fundamental contribution in many great discoveries including cell cycle, vesicular transport, cell autophagy, telomere protection, protein folding, unfolded protein response, DNA damage response, target of rapamycin and histone regulation. Many scientists won the Nobel Prize for these discoveries. In this article, the application and significance of yeast in scientific researches are introduced.

    Science Review
    Three scientific achievements in China
    GUAN Yi
    2017, 39(3):  222-230.  doi:10.3969/j.issn.0253-9608.2017.03.009
    Asbtract ( 442 )   PDF (2069KB) ( 148 )  
    Related Articles | Metrics
    Science Focus
[an error occurred while processing this directive]