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化石带
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  fossil zone
     The paper pre-sents a discussion of the assembly features and date of Fusulinida fauna,establishes an assemblage ofPolydiexodina-Neomisellina-Codonofusiella as the highest fusulinid fossil zone for late stage of Early Permi-an,and discribes in detail the Neomisellina wupingensis sp.nov.
     类化石带。 文章详细描述和讨论了Neomisellina wupingensis sp.nov.
短句来源
     it is proposed that maximum flooding surface is the best choice of boundary stratotype in continental facies stratum, namely boundary stratotype point should be established on the bottom of widespread distributed fossil zone above the maximum flooding surface.
     在陆相地层中,作者提出,界线层型剖面点建立在最大洪泛面上是最好的选择,即应将陆相地层的界线层型剖面点建立在最大海泛面上第一个广泛分布的化石带之底。
短句来源
  fossil zones
     The Ordovician strata has been divided resonably and revised in epoches inn this paper, therefore, 11 fossil zones or biological assemblages of Ordovician are set up in the area.
     确证该区寒武系与奥陶系为连续沉积,对奥陶系进行了合理划分和时代厘定,初步建立了11个化石带或生物组合。 该区是华北地台西缘奥陶系发育最好、生物地层研究最清楚的地区。
短句来源
     Through the study on the bio-stratigraphy, sequence and chemo-stratigraphy from the Or-dovician/Silurian boundary section in Wangjiawan, Huanghuachang, Fengxiang of Yichang County and the newly founded one in Goujiaya of Yuan 'an County, the fossil zones of the upper-most Ordovician and the lowermost Silurian are securely re-established in ascending order; Nankinolithus zone, Dicellograptus complexus zone, Paraorthograptus pacificus zone, Nor-malograptus bohemicus-N.
     根据对湖北宜昌王家湾、黄花场、分乡以及新近发现的远安苟家垭奥陶系与志留系界线剖面生物地层、层序地层和化学地层的综合研究将该区最晚奥陶纪到最早志留纪的化石带自下而上重新厘定为Nankinolithus带,Dicellograptus complexus带,Paraorthograptus pacificus带,Nor-malograptus bohemicus-N.
短句来源
     Four genera and five species of Liaoning and Hebei fossil lizards were named, and at least two new genera and species are being studied. Four lizard fossil zones are recognized in ascending order: Middle Jurassic Yabeinosaurus youngi Zone, early Early Cretaceous Dalinghosaurus longidigitus-Yabeinosaurus ten-uis Assemblage Zone, early Early Cretaceous Yabeinosaurus tenuis Zone, and late Early Cretaceous Teil-hardosaurus canbonarius Zone.
     这些化石自下而上可划分4个蜥蜴类化石带:中侏罗世杨氏矢部龙带(Yabeinosaurus youngi Zone)、早白垩世早期长趾大凌河蜥-细小矢部龙组合带(Dalinghosaurus longidigitus-Yabeinosaurus tenuis Assemblage Zone)、早白垩世早期细小矢部龙带(Yabeinosaurus tenuis Zone)及早白垩世晚期炭德氏蜥带(Teilhardosaurus canbonarius Zone)。
短句来源
     Conodonts discovered from Xiaoshigai section at the boundary between the Cambrian- Ordovician systems of Xiaoshan Region,Zhejiang Province are used to establish 4 con-odont fossil zones.
     本文根据在浙江省萧山县小石盖剖面中所发现的寒武──奥陶系界线地层的牙形刺化石,建立4个牙形刺化石带
短句来源
     The Cambrian of North China type in Henan province may be divided into three series, nine formations and 26 fossil zones.
     河南省华北型寒武系可划分为3统9组26个化石带
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  “化石带”译为未确定词的双语例句
     The Walongshan Formation was established then and it is featured by abundant fusulinid. Six fusulinid zones were established as follows:(1)Eostaffella mosquensis zone,(2)Millerella-Eostaffella zone,(3)Pseudostaffella-Eostaffella zone,(4)Profusuliena zone,(5)Fusulina-Fusulinella zone,(6)Protriticites-Triticites zone.
     经研究,自下而上建立6个■类化石带:(1)Eosta ffella mosquensis带,(2)Millerella-Eostaf fella带,(3)Pseudostaf fella-Eostaf fella带,(4)Pro-fusuliena带,(5)Fusulina-Fusulinella带,(6)Protriticites-Triticites带。
短句来源
     The present paper introduces the strata of the Carboniferous Chuanshan Formation in Shaxian, Fujian. According to the distribution of fusulinid fossils in the strata, the fusulinids may be distingushed into 5 zones in descending order as follows: 5) Eoparafusulina pararegularis Zone, 4) Sphaeroschwagerina sphaerica Zone, 3) Zellia chengkungensis Zone, 2) Pseudoschwagerina miharanaensis Zone and 1) Triticites shikhanensis compactus Zone.
     根据地层中类化石的分布规律 ,福建沙县船山组地层自上而下可划分为 5个化石带 :5 ) Eoparafusulinapararegularis带 ,4 ) Sphaeroschwagerina sphaerica带 ,3) Zellia chengkungensis带 ,2 ) Pseudoschwagerina miha-ranaensis带和 1) Triticites shikhanensis compactus带。
短句来源
     Here described in detail are totally 11 genera and 28 species of upper Permian-Lower Triassic conodonts collected from Boreholes 11-l,11-2,79-8,etc. near Zhenjiang,with the establishment of 6 conodont zones(including 1 upper Permian zone and 5 Lower Triassic zones),based on which correlations are made between corresponding zones both at home and abroad.
     详细描述了采自镇江附近11-1,11-2,79-8号等钻孔的上二叠统—下三叠统的牙形刺化石共11属28种,建立了6个牙形刺化石带,其中上二叠统1个、下三叠统5个,并以牙形刺带为基础,进行了国内外对比。
短句来源
     hughesi and Stichocorys delmontensis, etc, we establish respectivelythree radiolarian fossi1 zones of the Late Miocene in the southern South China Sea,inclu-ding RN6,RN7 and RN8, and discuss their stratlgraphic age.
     hughesi和Stichocorys delmontensis等的分布特征,分别建立了南海南部晚中新世的 RN6,RN7和RN8等3个放射虫化石带,并讨论了其地层年龄。
短句来源
     The Chihsia limestone in eastern CHINA, as our present knowledge goes, comprises 4 fusulinid zones, namely, (1) zone of Schwagerina Tschernyschewi, (2) zone of Misellina claudiae, (3) zone of Nankinella orbicularis-Mufushanella mufushanensis, (4) zone of Sohwagerina chihsiaensis-Parafusulina multiseptata in ascending order. The first zone comprises Schwaqerina tshornyschewi; the second zone contains mainly Misellina claudiao with some Schwagerina tschernyschewi;
     本文初步提出华东地区棲霞灰岩中四个(虫竹廷)类化石带,即(1)Shwagerina tschernyschewi带,(2)Misellina claudiae带,(3)Nankinella orbicularis Mufushanella mufus hanensis带,(4)Schwagerina chihsiaensis-Parafnsulina multiseptata带。
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  fossil zones
According to the distribution of mollusk fossil assemblages in the loess section, 11 mollusk fossil zones have been recognized, representing different climatic and ecological conditions.
      
A sequence-stratigraphic framework of the Dabeigou-Zhangjiagou Fms has been constructed by tracing sequence-bounds, marker-beds and fossil zones.
      
The Middle Ordovician Volginsky and Kirensky fossil zones were sampled in the Krivaya Luka section (Krivolutsky suite) that outcrops along the Lena river in Siberia.
      
Eight fossil zones were identified in the Upper Cretaceous section of the C-15Testhole, which ranges in age from Cenomanian to Maastrichtian.
      


The Chihsia limestone in eastern CHINA, as our present knowledge goes, comprises 4 fusulinid zones, namely, (1) zone of Schwagerina Tschernyschewi, (2) zone of Misellina claudiae, (3) zone of Nankinella orbicularis-Mufushanella mufushanensis, (4) zone of Sohwagerina chihsiaensis-Parafusulina multiseptata in ascending order. The first zone comprises Schwaqerina tshornyschewi; the second zone contains mainly Misellina claudiao with some Schwagerina tschernyschewi; the third zone contains the species of Nankinella,...

The Chihsia limestone in eastern CHINA, as our present knowledge goes, comprises 4 fusulinid zones, namely, (1) zone of Schwagerina Tschernyschewi, (2) zone of Misellina claudiae, (3) zone of Nankinella orbicularis-Mufushanella mufushanensis, (4) zone of Sohwagerina chihsiaensis-Parafusulina multiseptata in ascending order. The first zone comprises Schwaqerina tshornyschewi; the second zone contains mainly Misellina claudiao with some Schwagerina tschernyschewi; the third zone contains the species of Nankinella, Sphaerulina, Pisolina and Mufushanella; the fourth zone is composed of Schwagerina chihsiaensis and Parafusulina multiseptata and other species. Recently, some new fusulinids have been discovered in the middle part of the limestone.In the districts of Nanlin and Chenghsien, southern Anhuei,some Cancellina-like fusulinlds were collected from the middle beds of the Chihsia limestone. They are now named as Praesumatrina anhueiensis Chen and Praesumatrina sp. Some specimens of Misellina claudiao were discovered together with Sohwagerina chihsiaonsis in the upper part of the limestone. This confirms the fact that this species has been found to occur through the whole beds of the Chihsia limestone in southwestern China. Some peculiar and very interesting fusulinid fossils were recently found in the middle part of the Chihsia limestone at Mufushan near Nanking city,Kiangsu. We call this fusulinid Mufushanolla mufushanonsis Chen. This new species is rhombic in axial section; its characteristic features are the presence of foramen in the basal part of the septa in the outer volutions and the absence of parachamata between the foramen. These specimens will be described in the following.

本文初步提出华东地区棲霞灰岩中四个(虫竹廷)类化石带,即(1)Shwagerina tschernyschewi带,(2)Misellina claudiae带,(3)Nankinella orbicularis Mufushanella mufus hanensis带,(4)Schwagerina chihsiaensis-Parafnsulina multiseptata带。並討論前苏門答腊(虫竹廷)与格子(虫竹廷)的不同特征,同时說明前苏門答腊(虫竹廷)在該灰岩中部出現及克郎特米斯(虫竹廷)在其上部发現的意义。最后将新近在該灰岩中发現的新属及新种幕府山(虫竹廷)以及安徽前苏門答腊(虫竹廷),球形南京(虫竹廷)等加以敘述,以供古生物学者討論。

The fusulinids described and illustrated in this paper comprise 52 species or

本文系统描述了贵州西部晚二叠世的(竹蜓)类6属、51种、一亚种和一未定种,其中24新种;建立了两个带和两亚带,自下而上为:1.Codonofusiella 带,2.Palaeofusulina 带,后者包括(1)P.minima-Nankinella guizhouensis 和(2)Palaeofusulina sinensis 两亚带。对Codonofusiella 带的涵意作了进一步阐述,讨论了Palaeofusulina 作为二叠系和三叠系分界标志的重要意义。并扼要介绍了国外晚二叠世含(竹蜓)地层和贵州西部晚二叠世的(竹蜓)类化石带的对比。

Upper Cambrian conodont bearing strata are widely distributed in many provinces of China, Anhui Province being one of them. In this paper, according to the fossil assemblages of trilobites and conodont, three conodont zones are established and may be correlated with the three trilobite zones.(see Table Ⅱ,Ⅲ) Three new genera (Prodentatus, Prodistacodus, Triangulatudus,) ten new species (Hertzina quadrata, Oistodus fungshanensis, Proconodontus anulatus, Proconodontus longiformis, Prodentatudus dentatus, Prooneotodus...

Upper Cambrian conodont bearing strata are widely distributed in many provinces of China, Anhui Province being one of them. In this paper, according to the fossil assemblages of trilobites and conodont, three conodont zones are established and may be correlated with the three trilobite zones.(see Table Ⅱ,Ⅲ) Three new genera (Prodentatus, Prodistacodus, Triangulatudus,) ten new species (Hertzina quadrata, Oistodus fungshanensis, Proconodontus anulatus, Proconodontus longiformis, Prodentatudus dentatus, Prooneotodus alatus, Prooneotodus hamatus, Prosagittodentus lingulatus, Triangulatudus anhuiensis, Westergaardodina incilis) and one subspecies (Proconodontus notchpeakensis serratus) are described here.

上寒武统含牙形刺地层广泛分布于中国许多省份,安徽省是其中之一,根据三叶虫和牙形刺化石组合,作者修改了前人对上寒武统地层的划分方案,建立了三个牙形刺组合带,并可与三个三叶虫化石带进行对比.(见表Ⅱ、Ⅲ) 本文描述了三个新属:原端牙形刺属(Prodistacodus gen.nov),原始齿牙形刺属(prodentatudus gen,nov.),三角形牙形刺属(Triangtdatudus gen.nov.);十个新种:四方黑尔兹牙形刺(Hertzina quadrata sp.nov.),风山箭牙形刺(Oistodus fengshanensis sp.nov.),环纹原牙形刺(proconodontus anulatus sp.nov.),长形原牙形刺(proconodontus longiformis sp.nov.),有齿原始齿牙形刺(prodentatudus dentatus sp.nov.),翼状原奥尼昂塔牙形刺(Prooncotodus alatus sp.nov.),钩状原奥尼昂塔牙形刺(Prooneotodus hamatus sp.nov.),舌状原镞牙形刺prosagitto...

上寒武统含牙形刺地层广泛分布于中国许多省份,安徽省是其中之一,根据三叶虫和牙形刺化石组合,作者修改了前人对上寒武统地层的划分方案,建立了三个牙形刺组合带,并可与三个三叶虫化石带进行对比.(见表Ⅱ、Ⅲ) 本文描述了三个新属:原端牙形刺属(Prodistacodus gen.nov),原始齿牙形刺属(prodentatudus gen,nov.),三角形牙形刺属(Triangtdatudus gen.nov.);十个新种:四方黑尔兹牙形刺(Hertzina quadrata sp.nov.),风山箭牙形刺(Oistodus fengshanensis sp.nov.),环纹原牙形刺(proconodontus anulatus sp.nov.),长形原牙形刺(proconodontus longiformis sp.nov.),有齿原始齿牙形刺(prodentatudus dentatus sp.nov.),翼状原奥尼昂塔牙形刺(Prooncotodus alatus sp.nov.),钩状原奥尼昂塔牙形刺(Prooneotodus hamatus sp.nov.),舌状原镞牙形刺prosagittodontus lingulatus sp.nov.),安徽三角形牙形刺(Triangulatudus anhuiensis sp nov.),浅沟韦斯特牙形刺(Westeryaardodina incilis sp.nov.);及一新亚种:锯齿诺契匹克原牙形刺(proconodontus notchpeakensis serratus subsp.nov).

 
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