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| 1 | The Genome of Dendrobium officinale Illuminates the Biology of the Important Traditional Chinese Orchid Herb显示文摘 | Liang Yan Xiao Wang Hui Liu Yang Tian Jinmin Lian Ruijuan Yang ShumeiHao Xuanjun Wang Shengchao Yang Qiye Li Shuai Qi Ling Kui Moses Okpekum Xiao Ma Jiajin Zhang Zhaoli Ding Guojie Zhang Wen Wang Yang Dong Jun Sheng | 2015 | Molecular Plant2015，8，6： | 64 |
| 2 | Cadmium transport mediated by soil colloid and dissolved organic matter:A field study显示文摘This study investigated the potential role of soil colloids and dissolved organic matter (DOM) in transporting Cd through in situ undisturbed paddy soil monoliths. Brilliant Blue was used as a tracer to assess the effect of preferential flow on Cd down migration. Experimental results showed that deep penetration of Cd and Brilliant Blue into the soil profile took place due to the preferential flow through macropores, mainly earthworm channels, with much of chemicals thus bypassing the soil matrix. Dye tracer and Cd distribution within the soil matrix was fairly restricted to several centimeters. Colloid restrained the migration of both dye and Cd in the matrix and preferential flow area. DOM facilitated the transport of Cd and Brilliant Blue in matrix and macropores by about 10 cm over that of the control. Pearson's is correlation analysis revealed strong associations between Brilliant Blue concentrations, exchangeable Cd and total Cd concentrations in three studied plots indicating that they had taken the same preferential flow pathway. | Zhaoli Li, Lixiang Zhou College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, China. | 2010 | Journal of Environmental Sciences2010，22，1： | 24 |
| 3 | Biostratigraphy and geography of the Ordovician-Silurian Lungmachi black shales in South China显示文摘Based on the new material of seven Ordovician-Silurian boundary sections investigated recently, together with previously published data, we analyze the temporal and spatial distributions of the Lungmachi black shales, a key petroleum source bed widely distributed in South China. The Lungmachi black shales range in age from the Normalograptus persculptus Biozone of the uppermost Ordovician to the Spirograptus guerichi Biozone of the lower Telychian, and ten graptolite biozones can be recognized within this unit. The basal and upper contacts of the Lungmachi black shales are diachronous. The basal contact ranges from the N. persculptus to the C. cyphus biozones, a span of five graptolite biozones over two stages. The upper contact ranges from the D. pectinatus-M. argenteus Biozone to the Spirograptus guerichi Biozone, which spans four graptolite biozones over two stages. The Yichang Uplift resulted in the formation of the Hunan-Hubei Submarine High in the border area of Hubei, Hunan, and Chongqing. This is supported by a break in sedimentation in this area spanning all or part of the Hirnantian, and in many areas extending into the underlying Katian and overlying Rhuddanian. Comparison of the distribution of the Katian to Rhuddanian strata in this area indicates a growth and subsequent reduction in area of the Hunan-Hubei Submarine High particularly in the Hirnantian to early Rhuddanian. This may partly represent the influence of the process of formation and melting of ice sheet in Ordovician South Pole and consequent sea level change. | FAN JunXuan Michael J MELCHIN CHEN Xu WANG Yi ZHANG YuanDong CHEN Qing CHI ZhaoLi CHEN Feng | 2011 | Science China Earth Sciences2011，54，12： | 24 |
| 4 | Zircon SHRIMP U-Pb dating of granites from Dulan and the chronological framework of the North Qaidam UHP belt, NW China显示文摘Zircon SHRIMP dating of granites from Dulan,east segment of North Qaidam UHP belt shows that they are 406.6±3.5 Ma for Yematan-E,407.3±4.3 and 397±6 Ma for Balijiehatan-W,404.5±4.0 and 397.0±3.7 Ma for Shuiwenzhan-N,380.5±5.0 Ma for Shuiwenzhan-S,382.5±3.6 and 372.5±2.8 Ma for Chachagongma.These granites from Dulan represent the products of the third and fourth periods of Paleozoic magmatism in North Qaidam.Geochemically,the granitoids with metalumious to weak peratuminous are quartz diorite,granodiorite,and granite in composition and mainly belong to calc-alkaline series,a few samples to calc or alkali-calc series.The third period of granites is a rock association of granodiorite+granite,with initial 87Sr/86Sr ratios from 0.7082 to 0.7110 and T2DM model ages from 1.41–1.90 Ga;and the fourth period of granites is a rock association of quartz diorite+granodiorite+granite,with initial 87Sr/86Sr ratios from 0.7072 to 0.7091 and T2DM model ages from 1.07–1.38 Ga.Therefore,the third period of granites has higher initial 87Sr/86Sr ratios and T2DM model ages.On the contrary,the fourth period of granites has Nd(t)values from 0.6 to-3.0,higher than that of the third granite with Nd(t)values-3.2 to-9.3.Thus,the data comparison indicates that the third granites may derive from Paleo-proterzoic continental crust with mantle material whereas the fourth granites may derive from the Meso-proterzoic basalt crust with continental material.Combined with regional geology,we thought that the third granites were formed relative to plate exhumation and the fourth granites to delamination of the lithospheric mantle. | WU CaiLai GAO YuanHong LI ZhaoLi LEI Min QIN HaiPeng LI MinZe LIU ChunHua Ronald B FROST Paul T ROBINSON Joseph L WOODEN | 2014 | Science China Earth Sciences2014，57，12： | 21 |
| 5 | Characteristics of rare-earth elements (REE),strontium and neodymium isotopes in hydrothermal fluorites from the Bailashui tin deposit in the Furong ore field,southern Hunan Province,China显示文摘In this paper the authors present the REE concentrations and Sr and Nd isotopic compositions of fluorites from the Bailashui tin deposit of the Furong ore field,southern Hunan Province. The results showed that the total amount of REE in fluorites is usually low,ranging from 0.705 to 8.785 μg/g with the chondrite-normalized REE dis-tribution patterns similar to those of the Qitianling granites in the study area,characterized by LREE-enrichment patterns with pronounced negative Eu anomalies. The fluorites vary in Sr isotopic composition within the range of 0.7083-0.7091,the values are lower than those of the granites and higher than those of the host carbonate rocks in this area. The εNd(t) values of fluorites vary between -9.4 and +10.3,revealing that both the crust-and mantle-source materials were involved in the ore-forming hydrothermal fluids. Combined with previous studies on this ore deposit,the Bailashui tin deposit is temporally and spatially closely related with granitic magmatism in this area. The hydro-thermal fluorites are the product of fluid/rock interactions between granitic magmatic hydrothermal fluid and marine carbonate rocks. The REE and F in the ore-forming fluid were derived from the granites,whereas Sr in the ore-forming fluid came mainly from the granitic magmatic hydrothermal fluid and marine carbonate rocks,although variations in Sr isotopic composition cannot be explained by a simple mixture of these two end-members. Evidence demonstrated that the ore-forming fluids are of crustal-mantle mixing origin,but that the fluids were probably in-completely homogenized and this may be caused by inhomogeneous mixing of the fluids of different sources. | YUAN Shunda PENG Jiantang HU Ruizhong BI Xianwu QI Liang LI Zhaoli LI Xiaomin SHUANG Yan | 2008 | Chinese Journal Of Geochemistry2008，27，4： | 16 |
| 6 | Immunohistochemical prognostic markers of esophageal squamous cell carcinoma:a systematic review显示文摘Background: Esophageal squamous cell carcinoma(ESCC) is an aggressive malignancy, with a high incidence and poor prognosis. In the past several decades, hundreds of proteins have been reported to be associated with the prognosis of ESCC, but none has been widely accepted to guide clinical care. This study aimed to identify proteins with great potential for predicting prognosis of ESCC.Methods: We conducted a systematic review on immunohistochemical(IHC) prognostic markers of ESCC according to the 2009 Preferred Reporting Items for Systematic Reviews and Meta-Analyses(PRISMA) Guidelines. Literature related to IHC prognostic markers of ESCC were searched from PubMed, Embase, Web of Science, and Cochrane Library until January 30 th, 2017. The risk of bias of these original studies was evaluated using the Quality in Prognosis Studies(QUIPS) tool.Results: We identified 11 emerging IHC markers with reproducible results, including eight markers [epidermal growth factor receptor(EGFR), Cyclin D1, vascular endothelial growth factor(VEGF), Survivin, Podoplanin, Fascin,phosphorylated mammalian target of rapamycin(p-mTOR), and pyruvate kinase M2(PKM2)] indicating unfavorable prognosis and 3 markers(P27, P16, and E-cadherin) indicating favorable prognosis of ESCC.Conclusion: Strong evidence supports that these 11 emerging IHC markers or their combinations may be useful in predicting prognosis and aiding personalized therapy decision-making for ESCC patients. | Chunni Wang Jingnan Wang Zhaoli Chen Yibo Gao Jie He | 2017 | Chinese Journal of Cancer2017，36，11： | 16 |
| 7 | Peaked abundance of Calanus sinicus earlier shifted in the Changjiang River (Yangtze River) Estuary:a comparable study between 1959,2002 and 2005显示文摘The sea surface temperature (SST) of the East China Sea (ECS) increased in the past decades,which may have a great impact on the ecosystem of the ECS,including the changes in plankton-population structure.In this paper,the changes in peaked abundance of Calanus sinicus in the Changjiang River (Yangtze River) Estuary were compared between 1959 and 2002,based on the data collected from the seasonally oceanographic cruises and those performed in spring of 2005.It was much higher in spring compared with that in other seasons both in 1959 and 2002.Furthermore,in spring 2005,the time for occurrence and decrease of the peaked C.sinicus abundance advanced about one month, accompanying the increase in the sea surface water temperature (SST).It peaked in June and decreased in July in 1959,however,in 2005,it peaked in May and attenuated sharply in early June.The earlier decrease of peaked C.sinicus abundance may further deteriorate the ecosystem in the Changjiang River Estuary and north nearshore of the ECS. | XU Zhaoli MA Zengling WU Yumei | 2011 | Acta Oceanologica Sinica2011，30，3： | 11 |
| 8 | Species composition and diversity of Euphausiacea in the East China Sea显示文摘Based on the data of four seasonal oceanographic censuses in the East China Sea (23°30′~33°00′N, 118°30′~128°00′E) in 1997~2000, the species composition and the diversity of Euphausiacea were discussed as well as their relations with environmental variables. Results showed that there were totally 23 different species of Euphausiacea, in which 16 occurred in spring and autumn respectively; 15 were present in summer and only 10 were observed in winter. According to the calculated alternation fraction (R), the species composition showed a clear seasonal alternation with the changes ofseasons. Moreover, the environmental variables had different impacts on the distribution of Euphausiacea in different seasons. The distribution in summer was not significantly related to water temperature and salinity. However, the surface salinity was a major determinant of the distribution in spring. In autumn, both surface and bottom temperatures were influencing factors. The distribution in winter depended on salinity at the surface and 10 m depth as well as the temperature at 10 m depth. Regarding to the seasonal variation of species composition, the variations in spring, summer and autumn were not so significant as those in winter. Except in summer, the species number changed with synchronous water temperature and salinity, as a result of the presence of warm currents in the East China Sea and the habitability of the dominant species. Since Euphausiacea tend to agglomerate, the distribution of different species was uneven, which was the major reason for the low diversity of Euphausiacea in the East China Sea. | XU Zhaoli LI Chunju | 2005 | Acta Oceanologica Sinica2005，24，4： | 10 |
| 9 | Oxygen and Hydrogen Isotopes of Waters in the Ordos Basin,China:Implications for Recharge of Groundwater in the North of Cretaceous Groundwater Basin显示文摘从 1988 年 1 月在 Ordos 盆从气象学的车站收集到 2005 年 12 月的几百件降水样品被用来建立一根本地大气的水线并且计算现代降水的加权的平均同位素的作文。氧和氢同位素,与为 δ
18 分别地, O 和 δD 在春天在冬季和富人被弄空,并且逐渐地在夏天和秋天减少,说明季节的效果是可观的。他们也证明南方部分和 Ordos 盆的北方部分之间的同位素的差别不是明显的,并且在中间的部分的同位素通常被弄空。32 件样品的同位素作文从浅地下水收集了(不到 150 m 的深度) 在到有为 δ
18 O 并且从 85 ‰到有为 δD 的 63 ‰的一般水准的 46 ‰。他们中的大多数与现代降水是相同的。22 中间、深的地下水的同位素作文(比 275 m 的深度大) 为 δ
18 O 并且从 89 ‰到有为 δD 的 76 ‰的一般水准的 63 ‰。一般水准珍视,说明是显著地不到那些现代降水中间、深的地下水在比较地更低的空气温度被再装。14 C 证明中间、深的地下水的 recharge 在迟了的更新世开始了。从八个湖收集的 13 件湖水样品的同位素定义一个本地蒸发趋势,与 3.77 的一个相对扁平的斜坡,并且证明湖水被现代降水和浅地下水主要喂。 | YANG Yuncheng SHEN Zhaoli WENG Dongguang HOU Guangcai ZHAO Zhenhong WANG Dong PANG Zhonghe | 2009 | Acta Geologica Sinica(English Edition)2009，83，1： | 10 |
| 10 | Effect of global warming on the distribution of Lucifer intermedius and L.hanseni(Decapoda) in the Changjiang estuary显示文摘We conducted an oceanographic censusin 1959,2002,and 2005 to evaluate changes in the temporo-spatial distribution and abundance of Lucifer intermedius and L.hanseni in the Changjiang estuary.In general,the abundance and frequency of occurrence(OF) for these two species were highest during the summer.We measured a significant change in the abundance and OF between years.The abundance and OF of L.intermedius increased from 3.7 individuals m 3 and 66.67%,respectively,in 1959,to 8.93 individuals m 3 and 85.19%,in 2002.In 1959,L.hanseni was only found during the summer(abundance:0.01 individuals m 3,OF:3.70%).However,in 2002,this species was collected during all seasons except the winter.Furthermore,abundance(0.47 individuals m 3) and OF(25.93%) were higher in 2002 than in 1959.Further increases in abundance and OF were measured during cruises during the spring of 2005.We hypothesize that global warmingis responsible for theincrease inabundanceofL.intermediusand L.hanseniand thenorthward expansionofL.hanseniinthe Changjiang estuary.Given our results,monitoring of both species may be useful to evaluate the effects of climate change. | Zengling Ma Zhaoli Xu Jin Zhou | 2009 | Progress in Natural Science:Materials International2009，19，10： | 9 |
| 11 | Seasonal distribution of Calanus sinicus (Copepoda,Crustacea) in the East China Sea显示文摘根据在 23 ° 3 0' ~的四季节的调查 33 ° N and118 ° 3 0' ~从 1997 ~ 2000 的 Easl 中国海的 128 ° E, Calanussinicus 的季节的分发与聚集紧张,回归贡献和另外的统计法被学习。它被推断那 C。sinicu 是从冬季介绍给夏天的 s 优势,特别在春天和夏天,因为它的优势等于 0。62 和 0.29 分别地。它在桡脚类的动物丰富的丰富的百分比在夏天是 76.71% ,比 66 大。60% 在春天,比 19.02% 大在冬季,比 4.02% 大在里面秋天。在冬季和春天的出现频率是 83.08% 和 93。89% ,比那高在夏天和秋天, 76.71% 和 73。87% 。与桡脚类的动物的另外的优势种相比, C。sinicu 对桡脚类的动物丰富的 s 贡献显然比在冬季,夏天和春天的另外的种类的大,但是在秋天更小。C。中国我们趋于有聚集的分布。clumping 索引在夏天达到顶点(50。19 ) ,在春天列在后面(19。60 ) ,在秋天衰退了(13。18 ) 并且在冬季(3.04 ) 是最低的。丰富在不同季节和区域变化了,关于在春天和秋天的温度然而并非咸度,到在夏天的咸度然而并非温度;到在冬季的既不温度也不咸度。在春天和夏天,它的高丰富区域经常位于台湾暖流, Huanghai 海冷水团,沿海的水群众和 Changjiang 形成的混合水团冲淡水。在春天和秋天,它的丰富被暖流影响,以及从大陆河的流量在夏天影响了它。它能被推断那 C。中国我们被使适应宽咸度和温度,,在华东海的 euryhalinous 和 eurythermousspecies。 | XU Zhaoli CHEN Bijuan | 2007 | Acta Oceanologica Sinica2007，26，3： | 9 |
| 12 | Analysis on the indicator species and ecological groups of pelagic ostracods in the East China Sea显示文摘Ecological adaptation and ecological groups of pelagic ostracods were examined in the East China Sea (23°30′~33°00′N, 118°30′~128°00′E), in relation to temperature and salinity. The data were collected in four surveys conducted from 1997 to 2000. The density, yield density, or negative exponent models were used to determine the optimal temperature and salinity of water for the thriving growth of pelagic ostracods. Thereafter,ecological groups and potential distribution patterns of pelagic ostracods were determined based on the predicted parameters such as optimal temperature and salinity, consulting the geographic distribution. The analytical results indicate that, among the numerical dominant pelagic ostracods in the East China Sea (ECS), Euconchoecia aculeata, E. elongata, E. chierchiae, E. maimai, and Cypridina dentata, etc. are offshore subtropical water species. These species are widely distributed in the area, and they can be brought by the warm current to north offshore during spring and winter. The predicated optimal temperature (OT) and optimal salinity (OS) for Paraconchoecia decipiens, P. echinata, P. spinifera, P. oblonga, Conchoecia magna and Porroecia porrecta are all greater than 25℃ and 34 separately. These species are mainly distributed in the waters of the Kuroshio, the Taiwan Warm Current, and the Taiwan Strait, and therefore are designated as oceanic tropical water species. On the other hand, Pseudoconchoecia concentrica is considered as offshore subtropical water species based on its geographical distribution although its OT is 19℃. The other species, though their OSs are approximately 34 and with OTs ranging from 20° to 25℃, are considered as offshore subtropical water species because they were found to be widely distributed from the South China Sea to the East China Sea. | XU Zhaoli | 2008 | Acta Oceanologica Sinica2008，27，6： | 9 |
| 13 | 军民深度融合中民企“参军”的路径优化——基于交易费用经济学视阈显示文摘运用交易费用理论优化民企在军民深度融合中的路径。研究提议:构建'四位一体化'的军民融合信用评估体系、搭建标准化的军民'对话'机制、完善准入和退出市场机制,探索'军民一家亲'的关系契约模式,以期降低交易费用,提高交易效率,为'民参军'寻找新制度经济学下的理论建议,同时拓宽新制度经济学的研究范围。 | 谭清美 武翠 Zhaoli SONG | 2019 | 科学管理研究2019，37，3： | 9 |
| 14 | A unified implicit scheme for kinetic model equations. Part I. Memory reduction technique显示文摘A memory reduction technique is proposed for solving stationary kinetic model equations. As implied by an integral solution of the stationary kinetic equation, a velocity distribution function can be reconstructed from given macroscopic variables. Based on this fact, we propose a technique to reconstruct distribution function at discrete level, and employ it to develop an implicit numerical method for kinetic equations. The new implicit method only stores the macroscopic quantities which appear in the collision term, and does not store the distribution functions. As a result, enormous memory requirement for solving kinetic equations is totally relieved. Several boundary conditions, such as, inlet, outlet and isothermal boundaries, are discussed. Some numerical tests demonstrate the validity and efficiency of the technique.The new implicit solver provides nearly identical solution as the explicit kinetic solver, while the memory requirement is on the same order as the Navier–Stokes solver. | Songze Chen Chuang Zhang Lianhua Zhu Zhaoli Guo | 2017 | Science Bulletin2017，62，2： | 7 |
| 15 | Over-expression of small ubiquitin-like modifier proteases 1 predicts chemo-sensitivity and poor survival in non-small cell lung cancer显示文摘 | Mu Juwei Zuo Yong Yang Wenjing Chen Zhaoli Liu Ziyuan Tu Jun Li Yan Yuan Zuyang Cheng Jinke He Jie | 2014 | Chinese Medical Journal2014，，23： | 7 |
| 16 | Rangeland Privatization and Its Impacts on the Zoige Wetlands on the Eastern Tibetan Plateau显示文摘The high Zoige Basin (Ruoergai Plateau) on the eastern Tibetan Plateau is a fault depression formed during intensive uplifting of the Tibetan Plateau. The wetland is globally important in biodiversity and is composed of marshes,bogs,fens,wet meadows and shallow water interspersed with low hills and sub-alpine meadows. Most of the Zoige wetlands have long been one of the most important grazing lands in China. Recent rangeland policy has allowed grazing,and usable wetland areas have been being legally allocated to individuals or groups of households on a long-term lease basis. Privatization of the wetland has impacted the Zoige wetlands in aspects of hydrologic condition,landscape and biodiversity. The uneven spatial distribution of water resources on private lands has led to the practice of extracting ground water,which has decreased the perched water table in Zoige. Fencing off the rangelands and grazing on expanding sand dunes have affected landscapes. Variation in the water table has led to the changes in vegetation diversity,resulting in the changes in wildlife and aquatic diversities and ecosystem processes. Making use all year round of the pasture that was previously grazed only in summer has shrunk the daily activity space of wildlife,and the newly erected fences blocked the movement of wild animals looking for food in the snow to lower and open areas. To maintain the favorable conditions of the Zoige wetland ecosystem,the author suggests that,in addition to biophysical research and implementation of conservation practices,there is an immediate need to initiate an integrated management program,increase public awareness of wetland functions and provide better training for the local conservation staff. | YAN Zhaoli WU Ning | 2005 | Journal of Mountain Science2005，2，2： | 6 |
| 17 | Distribution pattern of pelagic amphipods and its affecting facors in the East China Sea显示文摘 | XU Zhaoli JIANG Mei | 2006 | Acta Oceanologica Sinica2006，25，5： | 6 |
| 18 | Study on abundance variation of pteropods in the East China Sea显示文摘On the basis of the census in four seasons from 1997 to 2000 in the East China Sea (23°30′￣33°N, 118°30′￣128°E), the horizontal distribution of pteropods, the seasonal variations of their abundance and dynamic mechanisms of these variations were approached with quantitative and qualitative methods. Results showed that the total abundance of pteropods varied clearly with the seasons in an order of decrease of autumn (108×10-2 ind./m3), summer (33×10-2 ind./m3), winter(28×10-2 ind./m3) and spring (10×10-2 ind./m3). Pteropods were not observed in the north nearshore of the East China Sea (29°30′￣33°N, 122°30′￣125°E)in winter and spring. In all seasons, the peteropod abundance was higher in the south than that in the north and higher in the offshore than that in the nearshore. The major species influencing the peteropod abundance were Creseis acicula in spring, Creseis virgula in summer, Desmopterus papilio in autumn and Limacina trochiformis in winter. The variation of pteropod abundance showed a prominent linear correlation with the surface water temperature and 10 m water temperature, but no significant correlation with both the bottom water temperature and salinity. In summer, the high-abundance distribution area of pteropods was located in the place where the Taiwan Warm Current branchedfromtheKuroshio. Inautumn, thedistributionareawithanabundancehigherthan250×10-2ind./m3expanded northward along with the Taiwan Warm Current within the mixing area where the Changjiang freshwater, the Fujian—Zhejiang coastal water and the Huanghai Sea Cold Water met together. Water temperature and warm currents were the most important environmental factors that influenced the changes of pteropod abundance in the East China Sea. | XU Zhaoli LI Chunju | 2006 | Acta Oceanologica Sinica2006，25，1： | 5 |
| 19 | Gastric Epithelial Apoptosis Induced by Helicobacter pylori and its Relationship with Fas Antigen Expression显示文摘 | LiuHai-feng LiuWei-wen FangDian-chun YangShi-ming ZhaoLi | 2000 | 胃肠病学2000，5，B08： | 4 |
| 20 | Species composition,diversity and density of plagic Ostracoda in the East China Sea显示文摘On the basis of seasonal investigations at 23°30'~33°00'N,118°30'~128°00'E of the East China Sea during 1997~2000,dynamics on the density and diversity of Ostracoda was discussed.Results showed that totally 26 species were identified.The Ostracoda diversity was opposite to the change of its density in most seasons which reflected an uneven assignment of Ostracoda density among its different species.The Ostracoda density was 0.70 ind./m3 in spring,1.72 ind./m3 in summer,2.57 ind./m3 in autumn and 0.90 ind./m3 in winter.Euconchoecia chierchiae in spring and winter,Euconchoecia maimai in summer and Cypridina dentata in autumn were main dominant species in each season.The Ostracoda density did not show an obvious linear relationship with the hydrologic factors in summer and autumn,but was related to the surface salinity in spring and the surface temperature in winter.Its high density areas mainly distributed in the north offshore in all the seasons while in the south offshore in winter and in spring,and the south nearshore in summer and autumn,implied the zooplankton was a typical warm water animal,whose high density distribution in autumn were located in a similar position to Todarodes pacificus,Navodon Septentrionalis,Scomber japonicus and other fishes in the sea,so as to be an important indicator for fishing ground.The main species dominating in Ostracoda now are different from the species twenty years ago probably attributes to global warming. | XU Zhaoli GU Xiaolian ZHANG Fengying | 2007 | Acta Oceanologica Sinica2007，26，5： | 4 |
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