晚始新世,Late Eocene
1)Late Eocene晚始新世
1.They represent the first records of the Pri- mates in Late Eocene of Nei Mongol.记录了内蒙古晚始新世的3种原始灵长类化石(Eosimias sp。
2.All of them represent the first records of their kinds in Late Eocene of Nei Mongol.上述啮齿类的发现也证明呼尔井组的时代为晚始新世
3.They represent the first cricetids ever found in Late Eocene of Nei Mongol.描述了产自内蒙古晚始新世地层中的3属5种仓鼠化石(Pappocricetodon antiquus,Pap- pocricetodon sp。
英文短句/例句

1.DISCOVERY OF PROTITAN (PERISSODACTYLA, BROTOTHERIIDAE) FROM LATE EOCENE TUKHUM BEDS, NEI MONGOL内蒙古晚始新世土克木层发现之原雷兽
2.LATE EOCENE MAMMALIAN FAUNAS OF HONAN AND SHANSI WITH NOTES ON SOME VERTEBRATE FOSSILS COLLECTED THEREFROM河南、山西晚始新世哺乳类化石地点与化石层位
3.LATE EOCENE MAMMALS FROM PINGCHANGGUAN BASIN, HENAN河南信阳平昌关盆地晚始新世哺乳动物化石
4.THE FIRST DISCOVERY OF LATE EOCENE LOCALITY OF MAMMALIAN FAUNA IN EAST CHINA山东首次发现晚始新世哺乳动物化石地点
5.LATE EOCENE AND OLIGOCENE CHAROPHYTES FROM THE DONGPU AREA, HENAN AND THEIR PALAEOENVIRONMENTAL SIGNIFICANCE河南东濮地区晚始新世至渐新世轮藻植物群及其古环境探讨
6.PLANT FOSSILS OF LATE EOCENE FROM WUCHENG,HENAN AND THEIR SIGNIFICANCE IN BOTANY AND PALEOCLIMATOLOGY河南吴城晚始新世的植物化石及其在植物学、古气候学上的意义
7.IRDIN MANHA UPPER EOCENE AND ITS MAMMALIAN FAUNA AT HUHEBOLHE CLIFF IN CENTRAL INNER MONGOLIA内蒙古呼和勃尔和陡坎晚始新世伊尔丁曼哈层及其哺乳动物群
8.LATE EOCENE QUATERNARY RADIOLARIA FROM THE NORTHEAST OF THE PHILIPPINE SEA AND THEIR SIGNIFICANCE FOR PALEOCEANOGRAPHY菲律宾海盆东北部晚始新世以来放射虫及其古海洋学意义
9.THE DISCOVERIES OF THE LATE EOCENE PLANKTONIC FORAMINIFERA INTHE PEARL RIVER MOUTH BASIN AND THEIR GEOLOGICAL IMPLICATIONS珠江口盆地晚始新世浮游有孔虫的发现及其地质意义
10.A NEW BRONTOTHERE FROM LATE MIDDLE EOCENE OF QUFU, SHANDONG记山东曲阜中始新世晚期─雷兽新属种
11.SOME NEW GENERA OF LATE CRETACEOUS TO EOCENE MICROPHYTOPLANKTON FROM WESTERN TARIM BASIN IN SOUTHERN XINJIANG新疆塔里木盆地西部晚白垩世—始新世微体浮游植物的几个新属
12.Primary Study on Quantitative Reconstruction of Middle-Late Eocene Climate in Jianghan Basin江汉盆地始新世中、晚期古气候定量重建初探
13.BIOTA AND DEPOSITIONAL ENVIRONMENT IN BEIJINGTIANJIN-BAXIAN AREA DURING LATE EOCENE AND EARLY OLIGOCENE京津霸地区始新世晚期至渐新世早期的生物群及其沉积环境
14.PALEOMAGNETIC STUDY OF SANSHUI BASIN IN GUANGDONG FROM LATE CRETACEOUS TO EOCENE AND ITS TECTONIC SIGNIFICANCE广东三水盆地晚自垩世—始新世古地磁研究及构造意义
15.Since the beginning of the upper Triassic epoch, the Indian plate upthrusted to the north over the Tethys oceanic crust and led to the closure of the Tethys in Eocene epoch.晚三迭世开始,印度板块在特提斯洋壳上向北仰冲,并导致特提斯在始新世的关闭。
16.Eocene series始新统始新系始新-中新世
17.A Study of Middle and Late Eocene Palynological Assemblages in Jianghan Basin and Their Environmental Significance江汉盆地始新世中、晚期孢粉组合特征及其环境意义
18.The Baikal rift system was formed due to faulting on the late Cretaceous?Eocene. Epoch planation surface base.在晚白垩世—始新世夷平面基础上,由于断裂作用形成了贝加尔裂谷系。
相关短句/例句

Bartonian[bɑ:'t?uni?n]巴尔頓(晚始新世)
3)late pleistocene晚更新世
1.Characteristics of Palynological Assemblage of Late Stage of Late Pleistocene in Changjiang River Delta Area and Paleoenvironment;长江三角洲地区晚更新世晚期的孢粉特征及古环境
2.The Sporopollen Assemblages and Their Paleoenvironment Significance of the Qianhu Bay,Zhangpu,Fujian since Late Pleistocene;福建漳浦前湖湾晚更新世的孢粉组合及其古环境意义
3.The distribution of elephant fossils and the physiognomy characters of late Pleistocene in Jixian County of Tianjin;天津蓟县晚更新世象化石分布与地貌特征
4)Late Holocene晚全新世
1.Pollen assemblage and palaeo-vegetation of Late Holocene fen in Dunhua of Jilin Province.;吉林省敦化地区晚全新世泥炭沼泽孢粉组合特征及古植被
2.Late Holocene climatic and environmental changes inferred from multi-proxies from Zabuye Saline Lake in Tibet;青藏高原扎布耶盐湖晚全新世气候环境演化
3.Environmental Evolvement and Human Activity Impact in the Late Holocene on the North Slopes of the Tianshan Mountains, China;天山北麓晚全新世环境演变及其人类活动的影响
5)Late Miocene晚中新世
1.Thermal and denudational history of granitoid batholith recorded by apatite fission track in the Dulong River region in northwestern Yunnan,since Late Miocene.;滇西北独龙江岩体晚中新世以来的热史和剥蚀历史的磷灰石裂变径迹记录
2.Late Miocene woods were investigated from the Lühe Basin in Chuxiong Borough, central Yunnan, China.利用光学显微镜和扫描电镜首次对云南省楚雄州晚中新世石灰坝组石鼓村层的钙化木材进行了解剖学研究。
3.New materials of Sinohippus from the Late Miocene"Hipparion Red Clay"of Gansu and Nei Mongol,China,are described and identified as Sinohippus robustus sp.结合甘肃临夏盆地和内蒙古四子王旗发现的新材料及之前发现的材料,辨认出中国晚中新世三趾马地层中的大型中华马与其他安琪马类的显著区别:下门齿前倾,第一对下门齿大而粗壮,第二对比第一对稍小,第三对非常小;前臼齿列及臼齿列的宽度分别向前和向后明显变小;下前脊长,下外谷与齿列长轴近垂直;m~3第三叶退化。
6)The late pleistocene晚更新世
1.Syn-depositional Deformation Structures by Earthquake Related to Volcanic Activity of the Late Pleistocene in Weizhou Island, Beihai City, Guangxi;广西北海涠洲岛晚更新世火山活动引起的地震同沉积变形构造
2.Deposit Characteristic and Developed Law of Debris Flow During the Late Pleistocene in Xiaojiang Valley;晚更新世小江流域泥石流沉积特征及发育规律
3.Based on the sporo-pollen analysis and  ̄(14)C dating from Balikun Lake Core ZK024, the sporo-pollen assemblages array surbey in Balikun Basin since the late Pleistocene is drawn out, and six comprehensive sporo-pollen zones are divided.本文根据巴里坤湖ZK─024孔的孢粉分析结果和~(14)C测年数据研究对比,总结归纳出巴里坤盆地晚更新世以来的孢粉组合序列概貌,并划分为六个孢粉组合带,在大陆性气候控制下的新疆,晚更新世以来干湿冷暖配置状况与东部地区相反。
延伸阅读

秋晚登楼望南江入始兴郡路【诗文】:潦收沙衍出,霜降天宇晶。伏槛一长眺,津途多远情。思来江山外,望尽烟云生。滔滔不自辨,役役且何成。我来飒衰鬓,孰云飘华缨。枥马苦踡跼,笼禽念遐征。岁阴向晼晚,日夕空屏营。物生贵得性,身累由近名。内顾觉今是,追叹何时平。【注释】:【出处】:全唐诗:卷47_17