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Genetic diversity and geographic variation innatural populations of the endemic Castanea species in China 植物学报, 1999,null

刘占林%李珊%阎桂琴%宋颐%赵桂仿华山新麦草自然居群的遗传结构和种内遗传多态性研究遗传学报, 2001,08

The resultsshow that the Pliocene paleoclimate of Tuantian Basin is characterized by the mean annualtemperature 21.3-25.1℃, mean temperature of the warmest month21.3-25.1℃, mean temperature of the coldest month 10.8-14.6℃, difference intemperature between the coldest and warmest month 11.3-16.3℃, mean annualprecipitation 1225.7-1638.3 mm, and relative humidity 75-82%.

通过共存因子分析法,取团田植物群37个化石种的最近亲缘种的气候因子的共存区间,定量重建了团田晚上新世的古气候特征:年均温为16.4-19.8℃,最热月平均气温21.3-25.1℃,最冷月平均气温10.8-14.6℃,气温年较差11.3-16.3℃,年均降水量1225.7-1638.3 mm,年均相对湿度75-82%。

Neotropical flora and fauna.

新热带植物群和动物群

According to the characters of the palynofloras, the Early Cretaceous palaeoecologic, palaeoclimatic, sedimentary environment as well as palaeogeographic significance have been discussed.

根据孢粉植物群的特征,探讨了该区早白垩世古生态、古气候、沉积环境及古地理意义。

According to the characters of the palynoflora, the Late Triassic palaeoecological, palaeoclimatic and palaeogeographic characters as well as the sedimentary environments in the region were discussed.

根据孢粉植物群的特征探讨了该区晚三叠世古生态、古气候、古地理和沉积环境。

Myrsine and Rapanea have traditionally been regarded as separate genera, especially in regional and local floras.

Myrsine和Rapanea已经传统上被认为是单独的属,特别是地区和本地植物群

We report the study of the similarity of 18 representative floras of the Lower and Middle Jurassic from China by use of clustering analysis.

选取属级分类单元作为统计变量, Dice系数作为统计公式,对中国早中侏罗世较具代表性的18个植物群进行了相似性的聚类分析。

The macro-biota of the early Doushantuoan from Southeast Zhongqing can compare with the Longfenshania Flora in the middle-late Qingbaikouian in North China, but differs from the late Doushantuoan biotas. It indicates that the macroscopic organisms were able to go through and had gone through the Snowball Event.

渝东南陡山沱期早期宏体生物群可与华北地区青白口期中-晚期Longfenshania植物群可进行比较,而与陡山沱期晚期宏体生物群有较大的区别,它表明了早期的宏体生物能够穿越过&雪球事件&。

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。

And control processes of Far Eastern Branch of Russian Academy of Science ...

27, 中国东北和俄罗斯远东早第三纪植物群的对比研究及其对环境变化的响应。。。

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