Loading...

Archive

    30 June 2020, Volume 32 Issue 2 Previous Issue    Next Issue

    For Selected: Toggle Thumbnails
    Current status and perspectives on genome mining of polar microorganisms
    Liao Li, Chen Bo
    2020, 32 (2):  133-139.  DOI: 10.13679/j.jdyj.20190034
    Abstract ( 810 )   PDF (1228KB) ( 1117 )  
    The rapid development of sequencing technology has greatly advanced research on microbial genomics. Although the initiation of polar microorganism genome sequencing was relatively late, it has become an important research area in the field of polar microbiology. The genetic resources of polar microorganisms hold strategic significance and social benefits. However, in-depth investigations of polar microbial genomes and genetic resources are quite limited, and the real power of genome sequencing has not been fully utilized. In this review, we summarize the current progress and research directions of polar microbial genomics, and analyze the shortcomings of current research and potential of genome mining. Accordingly, we propose key research directions requiring particular attention and breakthroughs. Overall, enhancing the mining of genetic resources from polar microorganisms provides more possibilities for future biotechnology.
    References | Related Articles | Metrics
    Tectonic control on the evolution of Arctic sedimentary basins
    Wang Zhe, Li Xuejie, Wang Jun, Yang Chupeng, Yao Yongjian, Ju Dong
    2020, 32 (2):  140-150.  DOI: 10.13679/j.jdyj.20190031
    Abstract ( 742 )   PDF (8724KB) ( 446 )  
    The evolution of sedimentary basins in the Arctic is controlled by complex tectonic processes over geological time. Using gravity and magnetic data from the Circum-Arctic Mapping Project, the tectonic framework of the Arctic basement was identified and overlapped with the distribution of sedimentary basins. Three types of regional tectonic factors that play a dominant role in the evolution of Arctic sedimentary basins were selected: (1) post-orogenic extensional collapse; (2) terrane accretion and foreland contraction; (3) rifting and opening of ocean basins. The tectonic events after these three types of regional tectonism have limited abilities to reshape basins; therefore, the characteristics of the basins basically remained constant. From the Neoproterozoic to the Phanerozoic, the Laurentia, Baltic and Siberia paleocontinents collided one after another to form the Tieman, Caledonian, Ellesmere and Ural orogenic belts. During the post-collision period, they extended and collapsed to form the base of large sedimentary basins in the Barents, Kara, Canadian Arctic seas and other regions. The Cenozoic evolution of the North Pacific margin terrane in northeastern Siberia and northwestern North America led to the development of foreland basins in the north. The rifting and opening of the Amerasia Basin and the North Atlantic-Eurasian Basin controlled the evolution of the Mackenzie Delta, Baffin Bay and the Laptev Rift Basin.
    References | Related Articles | Metrics
    Main characteristics and influence factors of the Pacific inflow in the region of Bering Strait: a review
    Zhang Yu, Deng Yongfei, Chen Changsheng
    2020, 32 (2):  151-163.  DOI: 10.13679/j.jdyj.20190045
    Abstract ( 923 )   PDF (3190KB) ( 1159 )  
    As one of the important sources of Arctic marine elements, the Pacific inflow in the region of Bering Strait plays a significant role in the process of surface ocean circulation and material and energy transport in the Arctic Ocean, and has a profound influence on regional and global climate and ecosystem. However, the current studies on the new change of the Pacific inflow and how the Pacific inflow participates in the ocean-atmosphere process of the Arctic Ocean are not enough. This paper reviews the current research progress on the main characteristics of the Pacific inflow including transport, circulation and water mass, summarizes the variation and driving mechanisms of transport, pathways and influence factors of circulation, and the water masses related to the Pacific Ocean water. Based on the previous studies, the prospects for future research are shown.
    References | Related Articles | Metrics
    Extraction of seasonal surface ablation zones in the Dalk Glacier (Antarctica) based on Landsat-8 images
    Qu Yutong, Cheng Xiao, Liu Yan
    2020, 32 (2):  164-176.  DOI: 10.13679/j.jdyj.20190029
    Abstract ( 763 )   PDF (17251KB) ( 433 )  

    Ice sheet surface ablation is a sensitive indicator of climate change and global warming. The melting of ice and snow will reduce the surface albedo and affect the global energy balance. Surface melt water will increase the propagation of cracks, reduce the stability of the ice shelf and affect the material balance of the ice sheet. At present, the lack of high-temporal resolution data on the distribution of ablation zones limits the in-depth exploration of the mechanism and spatial-temporal characteristics of Antarctic ice sheet ablation. Focusing on the research of the extraction of the large-scale ablation zone(blue ice, wet snow and melt water) of the Antarctic ice sheet, an automatic ablation zone extraction method based on the MNDWIice (Modified Normalized Difference Water Index Adapted for Ice,) is proposed. Using Landsat-8 data with a resolution of 30 m at 18 scenes from September 2016 to April 2017, the MNDWIice threshold automatically extracted from the ablation zone was obtained, and the seasonal ablation information extraction and analysis with high spatial resolution were realized by taking the Dalk Glacier in the east Antarctic as an example. The results show that: Under the condition of less cloud and terrain shadow interference, the MNDWIice calculated based on the Landsat-8 reflectance data uses a single threshold (0.136) to extract the ablation zone with an accuracy of 67.7% —94.2%, and the average accuracy is 81.5 %; The ablation area of Dalk Glacier and the mean value of MNDWIice in the ablation zone show obvious seasonal spatiotemporal changes; Ablation occurred no later than the earlier time of Landsat-8 data observation (September 7); Ablation first appeared and mainly occurred at the eastern ground line where the terrain dropped sharply.

    References | Related Articles | Metrics
    Numerical simulations of deck structure icing on polar offshore platforms based on Fluent and FENSAP-ICE
    Shen Jie, Bai Xu
    2020, 32 (2):  177-183.  DOI: 10.13679/j.jdyj.20190033
    Abstract ( 716 )   PDF (440KB) ( 1286 )  

    The polar region is rich in natural resources, but the climate is harsh. The deck surface of offshore platforms in this region is prone to icing, which is dangerous. To investigate factors affecting the icing of deck structures on polar marine platforms, a combination of the software programs Fluent and FENSAP-ICE was used to analyze the influence of sea surface height and structure length on deck icing under conditions of supercooled fog and rain. The results showed that when Characteristic wind speeds were 5 m·s–1, 6 m·s–1 and 7 m·s–1, average ice thickness on the structure surface increased gradually with height from 2 m to 20 m and the relative growth rate of ice on the structure surface decreased gradually. Additionally, when Characteristic wind speed was 5 m·s–1 at altitudes of 20 m and 80 m above sea level, the length of the structure increased from 1 m to 30 m, and average ice thickness on the structure surface and degree of reduction decreased.

    References | Related Articles | Metrics
    Design and implementation of a multi-energy complementary microgrid system at Taishan Station, Antarctica
    Lü Dongxiang, Li Chuan, Wang Zhechao, Yao Xu, Wei Fuhai, Li Zhao, Han Anjun, Bian Jiantao
    2020, 32 (2):  184-194.  DOI: 10.13679/j.jdyj.20190036
    Abstract ( 799 )   PDF (1650KB) ( 1293 )  
    A highly reliable and weatherproof microgrid system was designed under extreme climate conditions, including extremely cold, high winds and thin oxygen, at Taishan Station in Antarctica. The essential operating parameters and installation strategy of the multi-energy complementary microgrid system were studied and simulated using the environment of Taishan Station. The development of this system provides a breakthrough for key technologies, such as solar and wind power generation, capacity and design, under extreme climate conditions. Advances in design and operation, including snow protection and control system designs for a multi-energy complementary microgrid and an intelligent control platform that can operate autonomously, were first studied and applied. Through the use of two control modes (grid-connected and off-grid operation modes), an efficient, stable and complementary system, including wind, solar, fuel and storage, was constructed. The system was installed, debugged and tested at Taishan Station; the results showed that the system met the design requirements and calculation results and can be used as a reliable power supply for Antarctic research stations.
    References | Related Articles | Metrics
    Accurate matching of in-situ geothermal gradients from a Ewing-type heat flow meter with deck thermal conductivity
    Xu Mingzhu, Zhang Tao,Shen Zhongyan,Yang Chunguo,Guan Qingsheng,Gao Jinyao
    2020, 32 (2):  195-201.  DOI: 10.13679/j.jdyj.20190056
    Abstract ( 665 )   PDF (2498KB) ( 623 )  

    Ewing-type heat flow meters are widely used for heat flow measurements in harsh environments because of their safety and convenience. When using a Ewing-type heat flow meter, the geothermal gradient of seafloor sediments is obtained by in situ measurements while the thermal conductivity of sediment samples is measured in the laboratory. Due to the stake effect, the insertion depth of the sampler in situ is not always consistent with the length of a recovered sample, so it can be difficult to accurately match the measurement positions for thermal conductivity and geothermal gradients, leading to errors up to 3.5 mW·m–2. Based on the principle that heat flow values of the same station at different depths are relatively consistent, a minimum standard deviation method was designed in this study to determine the optimal deviation of Ewing heat flow meter operations. According to an analysis of data collected from 12 stations during China's ninth scientific Arctic expedition, the standard deviation of heat flow values at each depth of the same station decreased from 8.4 mW·m–2 to 3.8 mW·m–2 after the minimum standard deviation method was applied, which is a variation amplitude of about 9% of the average heat flow value.

    References | Related Articles | Metrics
    Surface roughness of the west of Marie Byrd Land(Antarctica) based on airborne elevation data
    Dong Hongwei, Yang Shuhu, Xu Jiaxin, Zhang Yun, Han Yanling, Hong Zhonghua
    2020, 32 (2):  202-211.  DOI: 10.13679/j.jdyj.20190044
    Abstract ( 703 )   PDF (8345KB) ( 359 )  
    Surface roughness of the west of Marie Byrd Land(Antarctica) was studied using airborne elevation data from the National Snow and Ice Data Center obtained by the Support Office for Aerogeophysical Research (SOAR) during flight surveys from December 1998 to January 1999. By analyzing and considering surface changes in the vertical and horizontal directions, surface roughness was accurately represented by effective slope. For 98% of the research area, the surface effective slope was less than 10° with a minimum value of 0.0126°. The effective slope above 10° was mainly distributed near the coast. The effective slopes of Edward VII Peninsula and some areas near the Shellis Coast were over 30° with a maximum of 39.9736°. The relationship between effective slope and topography on the Ross Ice Shelf, Ford Ranges and Edward VII Peninsula are discussed.
    References | Related Articles | Metrics
    Features and formation of fusion crusts on an ordinary chondrite(GRV 090196) from Antarctica
    Sun Yunlong, Miao Bingkui, Huang Lilin, Zhang Chuantong, Xia Zhipeng
    2020, 32 (2):  212-225.  DOI: 10.13679/j.jdyj.20190027
    Abstract ( 808 )   PDF (34862KB) ( 391 )  
    Meteorite fusion crusts are formed during atmospheric entry and show different textural characteristics based on differences in entry velocity and structural changes in the atmosphere. Therefore, fusion crust study is important to understand atmospheric entry processes and atmospheric structure at that time. Many Antarctic meteorites have retained their original or complete fusion crust because of the region’s unique geographical and climatic conditions, so they are ideal samples for fusion crust research. An ordinary H5 chondrite (GRV 090196) from the Grove Mountains region (Antarctica) was investigated in this study. It has a complete molten fusion crust with some flow lines showing its flying direction. Thin sections showed two intact fusion crusts with thicknesses of 1.3 mm and 0.4 mm. Petrology and mineralogy showed that the first fusion crust (Ⅰ) could be divided into four structural layers (outside to inside). Layers 1 and 2 were melted completely and recrystallized to form porphyritic structures in a glassy matrix, but the morphology and chemical composition of olivine phenocrysts in these layers were very different. This indicates it experienced different atmospheric layers of various densities. In layer 3, partial melting was obvious and mineral residues were observed; crystals were rounded with some bubbles. Thermal metamorphism occurred in layer 4, appearing opaque and black under plane polarized light, with a darkening phenomenon that may be from fine iron precipitation. Its texture was similar to those inside the meteorite. The second fusion crust (Ⅱ) was divided into three layers (outside to inside). Silicates in layer 1 were partially melted and rich in metallic grains. Layers 2 and 3 were similar to layers 3 and 4 in fusion crustⅠ. We suggest that fusion crusts were caused by accumulation and can be used to judge the landing direction of a meteorite. The two glassy layers and olivine phenocrysts in fusion crustⅠas well as the recrystallized olivine phenocrysts indicate that fusion crust melt was moved along the meteorite body by air. The fusion crusts experienced two relatively denser atmosphere layers that formed two glassy layers, and fusion crustⅡwas located in the side of the front. Only a small amount of the molten material remained and formed a very thin glassy fusion crust.
    References | Related Articles | Metrics
    Otolith morphological feature of bald notothen (Pagothenia borchgrevinki) and its prediction for change in fish lengt
    Wei Xiaoying, Duan Mi, Zhu Guoping
    2020, 32 (2):  226-235.  DOI: 10.13679/j.jdyj.20190042
    Abstract ( 770 )   PDF (2370KB) ( 864 )  

    The bald notothen (Pagothenia borchgrevinki) is a typical fish species that preferred to stay at the underside of Antarctic sea ice. The morphology of otolith in bald notothen correlates to the shape of fish. To understand otolith morphology and its ability to predict sizes of individual, using the samples with standard length (SL) 4.50 cm to 17.80 cm and wet weight (WW) 1.31 g to 80.79 g, this study measures and analyzes otolith morphology and then attempts to predict fish length using random forest modeling. The results show ranges of otolith length (OL) and width (OW) are 0.992 – 2.814 mm and 0.744 – 1.797 mm, respectively, and otolith weight is 0.00008 – 0.00448 g. With distinct rostrum and antirostrum, otolith is smooth with no obvious scallop. The size of otolith is increased with increasing SL of fish, but the relative size of otolith decreases gradually, therefore basically the proportion of different morphological structures remain unchanged. The OL, dorsal length (DL), dorsal width (DW), antirostrum length (ARL), rostrum length (RL) and perimeter (P) show a logarithmic relationship to fish SL. The OW and fish SL shows a power relationship, and the otolith area (S) and fish SL show a linear relationship. The relationship between OL, DL, ARL, P and fish WW is logarithmic, and OW, DW, RL, S and fish WW have a power relationship. The OL and OW show a power function relationship, but OL is linearly related to OW. Compared to other otolith morphological parameters, the contribution of OW, DW and S to fish SL is larger. The length of fish can be pre-dicted effectively by otolith morphological parameters using random forest modeling, with a prediction accuracy of 93.91%. This study provides a reference for the morphological study of Antarctic fish otoliths, shows that fish SL can be reconstructed using otolith thich is extracted from the stomach of fish-eating predators, and contributes information for the study of feeding ecology.

    References | Related Articles | Metrics
    Research on sea ice variability and navigation of the Arctic Northwest Passage from remote sensing data
    Wang Chuya, Yang Yuande, Zhang Jian, Tian Biao, Ding Minghu
    2020, 32 (2):  236-249.  DOI: 10.13679/j.jdyj.20190043
    Abstract ( 1036 )   PDF (14182KB) ( 591 )  
    Using daily sea ice concentration data from satellites (AMSR-E and AMSR2), the average sea ice area from July to September (2002–2018) in the Canadian Arctic Archipelago was calculated and the average sea ice variation in September was studied. Based on the ice-breaking capacity of a merchant ship, the threshold of sea ice concentration was determined. Key areas of the Northwest Passage were selected for study with the navigable windows counted and the possibility of actual commercial navigation discussed. We found that sea ice areas of the Canadian Arctic Archipelago in July, August and September showed a downward trend over the past 17 years with clear fluctuations. The interannual variations in September sea ice distribution were complex. In the navigable years for the Northwest Passage, the navigable start date was generally in August and the end date varied from the end of September to the beginning of October; the navigable duration was more than 14 days with the longest reaching 80 days. In general, Northwest Passage navigable years and duration lacked regularity.
    References | Related Articles | Metrics
    Review of research on Quaternary paleoceanography of the Siberian Arctic seas
    Jia Fufu, Sha Longbin, Li Dongling, Liu Yanguang
    2020, 32 (2):  250-263.  DOI: 10.13679/j.jdyj.20190074
    Abstract ( 803 )   PDF (1584KB) ( 1435 )  
    The Arctic is one of the most sensitive areas to global climate change because of its strong influence on global thermohaline circulation and atmospheric circulation. In particular, changes in Arctic sea ice and sea level have affected the opening and closure of the Bering Strait, water mass exchange and ocean circulation, as well as exposure of Arctic continental margins. The Chukchi, East Siberian and Laptev seas are the largest marginal seas in the Arctic Ocean and have undergone significant oceanographic changes during glacial–interglacial cycles. In this review, we present Quaternary oceanographic and climatic changes in the Chukchi, East Siberian and Laptev seas, and then discuss advantages and disadvantages of different paleoceanographic and paleoenvironmental records based on a diverse range of proxies. In the comparatively comprehensive and systematic body of research on Quaternary paleoceanography of the Siberian Arctic seas, we found that paleoceanographic records (i.e. oceanography, sea level, sea surface temperature and salinity, sea ice) were influenced by changes in the Earth’s orbit and the amount of radiant energy reaching the Earth, as well as ice sheet mass balance, sea level changes and Arctic river discharge. We also provide suggestions for future paleoclimate and paleoceanographic research in this region.
    References | Related Articles | Metrics
    A review of novel polar microbial enzymes for industrial applications
    Wang Wei, Yao Congyu, Sun Jingjing, Hao Jianhua
    2020, 32 (2):  264-275.  DOI: 10.13679/j.jdyj.20190039
    Abstract ( 743 )   PDF (376KB) ( 1252 )  
    Special challenges for microorganisms in cold ecosystems include reduced enzymatic reaction rates, limited bioavailability of nutrients, and frequent extremes in pH and salinity. To thrive successfully in low temperature environments, psychrophiles have evolved a complex range of structural and functional adaptations. Psychrophiles produce cold-active enzymes, which can be up to ten times more active at low and moderate temperatures compared with their mesophilic homologues. The enzymes of polar microorganisms are shaped by their adaptations to the permanently low temperatures. In addition, strongly differing environments, such as permafrost, glaciers and sea ice, have contributed to additional functional diversity. Microorganisms that thrive in the polar zones are a vast reservoir of cold-adapted enzymes. These enzymes could be beneficial in many industrial applications. Research using polar microorganisms to find new bioproducts has been mainly focused on enzymes that can be used in a range of industrial processes. The biotechnological value of cold-adapted enzymes stems from their high turnover (kcat) at low to moderate temperatures and their high thermolability at elevated temperatures. In recent years, a large number of new polar microbial enzymes have been continuously discovered, indicating that polar microbes have become an important source of novel enzymes. This review describes the research progress of new microbial enzymes over the past five years, and focuses on the discovery of important industrial enzymes, such as protease, lipase/esterase and carbohydrate-degrading enzymes, with good commercial prospects.
    References | Related Articles | Metrics
    Briefing of 36th Chinese National Antarctic Research Expedition
    He Jianfeng
    2020, 32 (2):  276-278. 
    Abstract ( 630 )   PDF (777KB) ( 1219 )  
    References | Related Articles | Metrics