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   广盐性生物 在 地质学 分类中 的翻译结果: 查询用时:0.937秒
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广盐性生物
相关语句
  euryhaline organisms
    All kinds of organisms belonged to euryhaline organisms.
    所有生物都属于广盐性生物.
短句来源
  “广盐性生物”译为未确定词的双语例句
    It was observed that they can reproduce and grow in the salinity range of 2-50‰, but the more suitable range was 10-30%) and the optiomum range was 15—25‰.
    此种轮虫为广盐性生物,能在2—50‰的盐度范围内生长繁殖,但其适宜的繁殖盐度为10—30‰,而尤以15—25‰为最适宜。
短句来源
    (5)The degree of saline-alkali water effect from high to low is shrimp,fish,shellfish and alga.
    (5)咸水水质对广盐性生物影响程度依次为虾、鱼、贝、藻。
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  euryhaline organism
The results of this study indicate that the Manila clam, a euryhaline organism, cannot maintain a normal metabolic activity at a salinity lower than 15‰.
      
The species has the adaptability to the environment, namely, the species is eurythermal and euryhaline organism.
      
  euryhaline organisms
Metahaline marine elements also inhabit the saline lagoons with salinities up to 60 to 80‰ In open lagoons, beyond these values, a hyperhaline community of marine euryhaline organisms has established itself.
      
Kyung-Soo Park Marine ecotoxicological approaches using euryhaline organisms in Korea ET-3.
      


The integration of geochemistry,palaeontology,sedimentary facies and palaeogeography,regional geology and global sea level fluctuations shows that seawater encroachments did not occur in the oil bearing basins in eastern China during Tertiary time.The presence of the “marine” Dinophyceae,foraminifera and calcareous ultramicrofossils are attributed to the salinized lakes and abundant nutrients.Dinophyceae is a kind of euryhaline organisms,and thus ubiquitous in ponds,lakes,rivers and seas,especially in brackish...

The integration of geochemistry,palaeontology,sedimentary facies and palaeogeography,regional geology and global sea level fluctuations shows that seawater encroachments did not occur in the oil bearing basins in eastern China during Tertiary time.The presence of the “marine” Dinophyceae,foraminifera and calcareous ultramicrofossils are attributed to the salinized lakes and abundant nutrients.Dinophyceae is a kind of euryhaline organisms,and thus ubiquitous in ponds,lakes,rivers and seas,especially in brackish environments.This implies that caution should be exercised in the application of Dinophyceae as a facies fossil.

本文以沟鞭藻生态为基础,结合我国东部第三纪盆地的地球化学、古生物、岩相古地理、区域地质和全球海平面变化,论证东部含油气盆地在第三纪时不存在海水侵进。出现有“海相”沟鞭藻、有孔虫和钙质超微化石是由于当时湖泊咸化及富养料造成的。同时认为沟鞭藻是广盐性生物,其最适应于半咸水环境。

The fossils of algae,ostracoda,foraminifera,gastropod and polychaeta were found in the Tertiary carbonate beds in the west of Chaidamu Basin.The quantity of various kinds of fossils was few,except the algae.The organisms were characterized by small size,simple structures of shells and low diversity.All kinds of organisms belonged to euryhaline organisms.It indicated that these organisms were developed in the environments of brackish lakes or salt water lakes and were not developed in the environments of marine...

The fossils of algae,ostracoda,foraminifera,gastropod and polychaeta were found in the Tertiary carbonate beds in the west of Chaidamu Basin.The quantity of various kinds of fossils was few,except the algae.The organisms were characterized by small size,simple structures of shells and low diversity.All kinds of organisms belonged to euryhaline organisms.It indicated that these organisms were developed in the environments of brackish lakes or salt water lakes and were not developed in the environments of marine facies or the transitional facies between the marine and land,according to the analysis of the paleontological characteristics in this area and the comparison with the paleocoenosis developed in other areas.11refs.

柴达木盆地西部第三系的碳酸盐岩层中发现有藻类、介形虫、有孔虫、腹足类、多毛类等化石.除藻类外各种生物的数量都比较少.生物具有个体小,壳体构造简单,多样性低等特点.所有生物都属于广盐性生物.根据该区古生物特征分析和与其它地区的对比,认为当时该区生物生长于内陆半咸化湖至咸化湖环境,而不是海相或海陆过渡相环境.参11.

 
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