菊石带,ammonoid zone
1)ammonoid zone菊石带
1.Based on the distribution of ammonoid fauna from the Upper Permian Dalong Formation to the base of the Lower Triassic Daye Formation,four ammonoid zones are recognized:(1)Araxoceras-Konglingites-Sanyangites zone,(2)Sinoceltites zone,(3)Pseudotirolites-Rotodiscoceras zone,and(4)Hypophiceras-Ophiceras-Lytophiceras zone.根据该剖面上二叠统大隆组至下三叠统大冶组底部菊石动物群的分布,自下而上划分为4个菊石带:Araxoceras-Konglingites-Sanyangites带、Sinoceltites带、Pseudotirolites-Rotodiscoceras带和Hypophiceras-Ophiceras-Lytophiceras带。
2)ammonite[英]['?m?nait][美]['?m?,na?t]菊石
1.In the Shangrao and Qianshan area of Jiangxi, ammonite fossils are very abundant in thecoal measure strata of Shangrao Formation which is a contemporaneous heleropic deposit of the Maokou Formation This paper has described in detail a large quantity of ammonites collected from this area and has discussed preliminarily the evolution of some of them.江西上饶和铅山地区茅口期异相沉积的上饶组煤系地层中,寿昌菊石科的菊石化石十分丰富。
英文短句/例句

1.Baculites ovatus fauna杆菊石属卵圆形动物群
2.of or related to fossil cephalopods of the order Ammonoidea.菊石目头足动物的化石或者与这种化石相关的。
3.from 310 million to 345 million years ago; increase of land areas; primitive ammonites; winged insects.陆地增加,原始菊石,有翼昆虫。
4.NEW PROGRESS IN THE STUDY ON PERMIAN AMMONOID BIOSTRATIGRAPHY IN GUANGXI广西二叠纪菊石生物地层学研究新进展
5.Late Triassic and Early Jurassic Ammonoids from Eastern Himalayas东喜马拉雅地区晚三叠世—早侏罗世的菊石
6.The coiled, flat, chambered fossil shell of an extinct mollusk belonging to the class Cephalopoda, which was abundant in the Cretaceous period.菊石,鹦鹉螺化石已灭绝软体动物的螺旋形、扁平的化石外壳,属头足纲动物,大量存在于中生代
7.EARLIEST TRIASSIC AMMONOID FAUNAS FROM JIANGSU AND ZHEJIANG AND THEIR BEARING ON THE DEFINITION OF PERMO-TRIASSIC BOUNDARY论苏、浙一带三叠纪最早期的菊石群及二叠系—三叠系界线的定义
8.Remains of more modern corals, diverse pelecypods, sea urchins and ammonoids characterize the marine strata of the Mesozoic Era.中生代生物的特征是出现较现代的珊瑚,各种各样的瓣鳃,海胆和菊石
9.The Cenozoic faunas often superficially resembled those of the Mesozoic. However, there were no ammonoid cepbalopods in this most recent era.新生代的动物群表面上类似于中生代的动物群,但新生代没有菊石头足纲动物,
10.Late Permian-Earliest Triassic Ammonoid Sequences from the Rencunping Section,Sangzhi County,Hunan Province,South China and Their Regional Correlation湖南桑植县仁村坪上二叠统—下三叠统底部菊石动物群序列及其区域对比
11.Study on Purification Process of Cichoric Acid and Caftaric Acid in Echinacea Purpurea and Property of Cichoric Acid紫锥菊中菊苣酸和单咖啡酰酒石酸纯化工艺及菊苣酸性质研究
12.Broadleaf hedge such as laurel, spirea, photinia, etc.阔叶树篱,如月桂、绣线菊、 光叶石楠等。
13.The chrysanthemum stone was former 280,000,000 years ago.菊花石形成于距今约2.8亿年前。
14.Study on the Chemical Consitituents of Helianthus Annuus, Vernonia Cumingiana and Eritrichium Rupestre;向日葵,毒根斑鸠菊和石生齿缘草化学成分研究
15.A Study on Some Physiological Changes in Postharvest Cut Flowers of Chrysanthemum and Carnation;切花菊和香石竹采后主要衰老生理特性研究
16.Transformation of Lycoris Longituba Agglutinin Gene to Cut Chrysanthemum and Identification of Aphid Resistance in the Transgenic Plants石蒜凝集素基因转化切花菊及抗蚜性鉴定
17.Enantioselective separation of lambda-cyhalothric acid enantiomers by chiral extraction with tartaric esters酒石酸酯立体选择性萃取分离功夫菊酸对映体
18.Drag onto the page to add a broadleaf hedge, such as laurel, spirea, or photinia.拖到绘图页后,可以添加阔叶树篱,如月桂、绣线菊或光叶石楠。
相关短句/例句

ammonite[英]['?m?nait][美]['?m?,na?t]菊石
1.In the Shangrao and Qianshan area of Jiangxi, ammonite fossils are very abundant in thecoal measure strata of Shangrao Formation which is a contemporaneous heleropic deposit of the Maokou Formation This paper has described in detail a large quantity of ammonites collected from this area and has discussed preliminarily the evolution of some of them.江西上饶和铅山地区茅口期异相沉积的上饶组煤系地层中,寿昌菊石科的菊石化石十分丰富。
3)ammonites菊石
1.With the suture line of ammonites as an example, the morphological feature in this paper is quantitatively described in view of fractal geometry.以菊石为例,应用分形几何学的观点对菊石缝合线的形态进行了定量描述。
4)ammonoid[英]['?m?,n?id][美]['?m?,n??d]菊石
1.Ma jiashan , Northwest Chaohu City, Anhui Province, East China, where the Lower Triassic is well developed and composed of the alternations of mudrock and limestone deposited on a deep part of the Lower Yangtze carbonate ramp, containing rich ammonoid fossils.由于地处低纬度下扬子碳酸盐缓坡台地较深水区 ,安徽巢湖地区的下三叠统由一系列泥、灰岩旋回层组成 ,并含有丰富的菊石化石。
2.Restricted sea ammonoid-bearing (siliceous) muddy deposit, IV.海域内的菊石群专属性地发育于(硅)泥质沉积,强烈的土著性质显示其生活环境的局限性,不同于陆缘海斜坡同期的“南丹型”菊石和沉积。
5)ammonoid fossil菊石化石
1.Because of the chaotic stratigraphic division of the Mid-Lower Jurassic dark-colored rock series in the Doima stratigraphic area, southern Qiangtang, the authors measured the Songke′er section in Sêwa during the petroleum geological survey in 2005 and systematically collected abundant ammonoid fossils with chronological significance.针对南羌塘多玛地层分区中—下侏罗统深色岩系地层划分的混乱状况,2005年在进行羌塘盆地石油地质调查中实测了色哇地区松可尔剖面,并系统采集到大量有时代意义的菊石化石。
6)Ophiceras蛇菊石
1.THE DISCOVERY OF Ophiceras IN THE KAYITOU FORMATION IN EASTERN YUNNAN PROVINCE AND ITS SIGNIFICANCE;Ophiceras(蛇菊石)在滇东卡以头组的发现及其意义
延伸阅读

菊石菊石ammonoid软体动物门头足纲的一个亚纲。是已绝灭的海生无脊椎动物,生存于中奥陶世至晚白垩世。菊石化石菊石壳以碳酸钙为主要成分。壳体以胎壳为中心在一个平面内旋卷,少数壳体呈直壳、螺卷或其他不规则形状。菊石动物在生长过程中周期性地由外套膜分泌出隔壁,因此壳体可以分为两部分:动物体栖居而没有隔壁的部分,称为住室;具有一系列隔壁的部分是气壳,被相邻两个隔壁所分隔的空间叫做气室;隔壁与壳壁的接触线叫做缝合线;每一个隔壁有一个圆形隔壁孔,为体管所在位置,通常位于腹部边缘,少数在背部或近中心位置。壳体表面有时平滑,有时有生长线纹、纵旋线纹、横肋、瘤、刺、沟、脊等装饰,菊石的壳口覆以口盖。菊石的系统分类中缝合线的特征具有特别重要的意义。每条缝合线可以分为壳体外表面的一段叫外缝合线,背部表面的一段叫内缝合线。缝合线的基本要素是叶和鞍。叶是缝合线向后弯曲的部分,鞍则是向前弯曲的部分。按照叶和鞍分布的位置,分别称为腹叶(或腹鞍)、背叶(或背鞍)、侧叶(或侧鞍)等。在侧面未完全变成独立的鞍和叶的一系列褶曲称为肋线系。按照叶和鞍的形态,可以将菊石缝合线归纳为无棱菊石式、棱菊石式、齿菊石式和菊石式。菊石通常分为9目约80个超科,约280个科和约2000个属,以及许多种和亚种等。菊石化石均产于浅海沉积的地层中,并与许多海生生物化石共生。通过研究,推测菊石栖居在热带至温带的有一定深度的海域,壳壁较厚和具粗强壳饰的类型是较不活动的类型;壳壁较薄、表面平滑和具尖饼状壳形者是较活动的栖居于较深水体的类型。菊石是划分和对比地层最有效的标准化石,可划分出颇为精细的菊石带。在中国古生代和中生代地层中所含的各种菊石,都具有重要的意义。