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biota相关的网络例句

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与 biota 相关的网络例句 [注:此内容来源于网络,仅供参考]

The Wenghui biota, which is found in the Ediacaran Doushantuo Formation in Northeast Guizhou, is composed mainly of macroalgae (18 species of 15 genera, one unnamed macroalgae, and macroalgal holdfast forms described herein), and contains macroscopic metazoan, putative metazoan and trace fossils. This biota not only contains some elements of the Miaohe biota from West Hubei, the Lantian flora from South Anhui, the Ediacara fauna in Australia, and the White Sea biota in Russia, but also has its own characters to distinguish other Ediacaran biota.

产自于黔东北伊迪卡拉系陡山沱组的瓮会生物群生活环境应在贫氧的、透光性良好的浅海低能环境,以宏体藻类为主,共描述15属18种(其中包括3个新属、5个新种、2个修定属和4个修定种)和1个未命名藻以及不明藻类固着器,另包含有宏体后生动物,可能的后生动物以及遗迹化石。

The biomarkers such as the n-Alkanes, the isoprenoids, the terpane, and cholestane were detected through GC-MS analysis. Based on the study of the biomarkers, the biological evolution during Permian and Triassic can be divided as three stages, namely, the mixing source stage of low biota such as thallose and advanced plant in late Permian (below bed 63), the stage of low biota such as thallose in the boundary transitional layer (bed 63-69) and the mixing source stage of advanced plant and low biota such as thallose in early Triassic (above bed 69). What's more, the second stage near the boundary transitional layer can be subdivided into 4 stages. The stages of biota evolution is close related with sedimentary environment changing and the boundary transitional layer.

利用GC—MS分析技术,在陆相地层中检测出正构烷烃、类异戊二烯烷烃、萜烷和甾烷类生物标志化合物并根据生物标志化合物和特征值研究,将二叠系—三叠系生物演化划分为三个大的阶段,即晚二叠世的菌藻类低等生物与高等植物混源阶段(63层以下),界线异常层的菌藻类低等生物阶段(63-69层)和早三叠世高等植物与菌藻类低等生物混源阶段(69层以上),界线附近异常层的第二阶段又进一步细分为4个次一级阶段,生物演化阶段与沉积环境变化及界线异常层具有非常密切关系。

On the section, the Wenghui Biota can be redivided into Globusphyton,Sectoralga-Longifuniculum,Cucullus,Beltanelliformis,and Baculiphyca- Gesinella Communities, from below to above. The change and evolution of these communities show the relation the biota and microenvironment, and indicates the relationship macro-plants with metazoans.

在时间纵向上可依次分为Globusphyton , Sectoralga-Longifuniculum , Cucullus , Beltanelliformis ,Baculiphyca-Gesinella等5个群落,反映出生物群落与环境的相关性以及宏体后生动物与植物之间的相关性和规律性。

The Miaohe biota in South China and the Ediacaran biota in Australia are doubtlessly contemporaneous. A couple of triradial fossils from the Wenghui lagerst?

翁会化石库中少量出露的三辐射化石与俄罗斯&白海生物群&的典型分子—Albumares和Anfesta可以对比。

Due to the relatively unique macrofossil assemblages in the Sinian strata of South China, its comparison with the Ediacara-type Biota occurring abundantly abroad in the strata postdating the last glacilation of Neopro-terozoic (including the Avalon Biota, the Pound/White Sea Biota and the Nama Biota) remains to be studied in detail in future.

由于华南震旦纪宏体化石具有较为独特的组合面貌,与国外末次冰期后大量出现的伊迪卡拉型生物群(阿瓦隆生物群,庞德/白海生物群和纳马生物群)如何对比,还有待深入的研究。

The authors reinvestigated the im-portant sections and fossil sites and collected macrofossils respectively from "Houjiashan Biota" in Jiangchuan, Yunnan Province, and "Wenghui Biota" in Jiangkou, Guizhou Province. On the basis of the above study and other latest research advancements, the authors integrated and synthesized the macrofossil features and assemblages of the Upper Neoproterozoic strata in South China and brought forward the biostratigraphic successions as well.

本项研究重新考察了部分重要的标准剖面和化石点,重点采集了近年来开始研究的云南&江川生物群&,贵州江口&翁会生物群&的宏体化石,在总结了前人研究成果的基础上,集成了最新的研究进展,综合记录了华南晚新元古代地层中的宏体化石特征,组合面貌,据此提出了华南晚新元古代生物地层序列。

The Wenghui Biota of the late Doushantuoan in Northeast Guizhou not only contains some elements of the Miaohe Biota from West Hubei, the Lantian Flora from South Anhui, the Ediacara Funa from South Australia, and the White Sea Biota from Russia, but also has its own characters to distinguish other Ediacaran biotas.

黔东北陡山沱期晚期瓮会生物群不但含鄂西庙河生物群和皖南蓝田植物群的分子,也有南澳大利亚伊迪卡拉生物群和俄罗斯White Sea生物群的分子,而且有别于其它伊迪卡拉期生物群。

There have been subsequent changes in the composition stromatolite biota through Earth's history. Smaller eubacteria may have greater involvement than cyanobacteria in stromatolite formation in the Precambrian, and cyanobacteria may enter stromatolite building biota until the latest Neoproterozoic.

参与碳酸盐岩叠层石建造的微生物群组成可能随着地质历史的演化发生变化,蓝细菌在显生宙的叠层石建造过程中起主导作用,细胞体积更小的真细菌很可能是参与前寒武纪叠层石建造的主要微生物。

This biota not only contains some elements of the Miaohe biota from West Hubei, the Lantian flora from South Anhui, the Ediacara fauna in Australia, and the White Sea biota in Russia, but also has its own characters to distinguish other Ediacaran biota.

瓮会生物群不但含有鄂西庙河生物群和皖南蓝田植物群的分子,也有南澳大利亚Ediacara生物群和俄罗斯White Sea生物群的分子,而且具有自已的特征而有别于其他伊迪卡拉期的生物群。

As we know, the Jehol Biota was found in this Formation; therefore, the investigation of depositional environment of it is important for the study of the occurrence and development of Jehol biota.

由于义县组地层富含了闻名于世的热河生物群,对其沉积环境的研究对于揭示热河生物群的发生、发展具有重要意义。

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