1) plant fossil
古植物化石
2) microflora
微古植物化石
1.
The dominant genera of the microflora, from the Xicun formation are Leiominuscula, Leiofusa, Asperatopsophosphaera, Germinosphaera and Melanocyillum.
文章论述了安徽歙县浅变质岩系微古植物化石的产出特点(计有27属40种)和它的时代意义,分析研究了西村组和昌溪组的优势属,分别为Leiominuscula,Leiofusa,Asperatopsophos-phaera,Germinosphaera,Melanocyillum和Germinosphaera,Leiominuscula,Leiopsophosphaera,Triangumorpha,Leiofusa等各5属。
3) palaeovegetation
古植被
1.
Palynological assemblages and palaeovegetation and palaeoclimate of the Holocene in eastern Shanghai;
上海东部地区全新世孢粉组合及古植被和古气候
2.
Evolution of Palaeovegetation and Palaeoenvironment of Pleistocene on the Basis of Spore-Pollen Analysis in the Shanghai Region;
从孢粉分析看上海地区更新世时期古植被、古环境演变
3.
Palynological Assemblages of Pleistocence from Shanghai Region and Its Palaeovegetation and Palaeoclimate;
上海地区更新世孢粉组合及其古植被、古气候
4) paleovegetation
古植被
1.
The data of spore-pollen offered the palynological information for stratigraphic division and correlation and for reconstruction of paleovegetation,paleoclimate.
通过对上海地区斜土路 2号孔晚第四纪地层的孢粉研究 ,划分出了晚第四纪 8个孢粉组合带 ,并结合邻近钻孔孢粉研究资料 ,恢复了该区植被演替、气候波动的六个阶段 ,这种气候波动不仅与世界性气候变化一致 ,而且其波动曲线也与海平面变化相吻合 ,从而为本地区进行地层年代划分和对比提供可靠的证据 ,为本地区晚第四纪古植被、古气候、古环境的重建提供了丰富的孢粉学资
2.
According to these data together with the sporopollen assemblage data from the Xining-Minhe basin, Lunpola basin, Namlin basin and Weihe basin, the authors analyzed the evolution of the Late Cenozoic paleovegetations and paleoenvironment on the Qinghai-Tibet Plateau and in its a.
对取自沱沱河盆地、通天河盆地、那曲盆地、东温泉盆地、乌郁盆地的新近纪湖相沉积与取自巴斯错、错鄂、纳木错的晚第四纪湖相沉积,进行孢粉分析;结合西宁—民和盆地、伦坡拉盆地、南木林盆地、渭河盆地的孢粉资料,分析青藏及邻区新生代晚期古植被和古环境的演化过程。
3.
Based on the U-series dating and sporo-pollen analysis, this paper presents a discussion on the paleovegetation and paleoclimate of the Buqu Basin and its adjacent regions during the interval 88.
结合孢粉分析结果 ,本文探讨了青海省西部地区通天河及布曲流域晚更新世早中期的古植被与古气候。
5) ancient vegetation
古植被
1.
A preliminary study of ancient vegetation in Xishui Swan Pool;
习水天鹅池古植被的初步研究
6) Palaeo-vegetation
古植被
1.
In this paper, the vertical evolution characteristics of palaeo-vegetation, palaeoclimate and palaeo-environment in Tuha basin are probed through the study of the Jurassic palynoflora, special lithology, and the distribution law of elements and clay mineral in argillaceous rock.
通过吐哈盆地侏罗系孢粉植物群、特殊岩性、泥质岩中元素、粘土矿物分布规律研究,探讨了古植被、古气候及古环境的纵向演化特点,认为区内侏罗纪古气候为:早侏罗世至中侏罗世早期区内气候为温暖潮湿的亚热带,局部有干旱趋势;中侏罗世中晚期半潮湿、半干旱的温带-亚热带气候;从中侏罗世末期开始转为炎热干旱的亚热带气候。
2.
This paper presents the high-resolution sequence of vegetation change of the last inter-glacial period in Xishan Mountain,Beijing by pollen analysis and thermoluminescent dating technology with reconstruction of the palaeo-vegetation and palaeo-environment of this region.
末次冰期—间冰期气候旋回研究是过去的全球变化(PAGES)研究的三大重点之一,通过孢粉分析和热释光断代建立了北京西山末次间冰期植被的演化序列,研究了该地区古植被与古环境的演化规律。
参考词条
补充资料：盗掘古人类化石、古脊椎动物化石罪
盗掘古人类化石、古脊椎动物化石罪：指盗掘国家保护的具有科学价值的古人类化石和古脊椎动物化石的行为。本罪属选择性罪名，具体包括盗掘古人类化石罪和盗掘古脊椎动物化石罪。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。