四射珊瑚

扬子区早志留世（Llandovery）的众多四射珊瑚属均为世界广布的，但也有许多地方性属（约有22个，占总数的23·4%）。

In the Yangtze Region , numbers of Llandovery rugose genera were cosmopolitan , but comprising many endimics ( about 22 genera , 23.4 % ), some of them first appeared in the Yangtze Region and later dispersed to other regions .

新中国成立以来古生代四射珊瑚研究简史

Research on the History of China Paleozoic Rugose Corals Since 1949

福建晚石炭世&早二叠世早期的四射珊瑚动物群

Rugose coral fauna of Late Carboniferous and early Early Permian in Fujian

新疆东昆仑山早二叠世四射珊瑚新资料

New data of Early Permian TETRACORALS from Eastern Kunlun Mountain of Xinjiang

贵州南部早二叠世几个四射珊瑚新属种

Some new genera and species of Early Permian TETRACORALS from South Guizhou

滇东曲靖地区晚志留世四射珊瑚动物群

Late Silurian rugose coral fauna from the Qujing district , East Yunnan

新疆阿勒泰地区早石炭世晚期菊石相四射珊瑚

Late Early Carboniferous corals in AMMONOID facies from Altay of Northern Xinjiang

中国中、晚石炭世四射珊瑚组合及古生物地理

Middle and Upper Carboniferous TETRACORAL assemblages and biogeography of China

新疆昆仑山、喀喇昆仑山中泥盆世及石炭纪一些四射珊瑚

Middle Devonian and Carboniferous TETRACORALS from Kunlun Mountain and Karakorum mountain , Xinjiang

贵州中泥盆世四射珊瑚新属

Two genera of Middle Devonian rugose corals from Guizhou

中国早石炭世的四射珊瑚组合及主物古地理

Early Carboniferous coral assemblages and paleobiogeography of China

数学方法在四射珊瑚分类中的应用

Application of mathematical methods to classification of TETRACORALS

从四射珊瑚论贵州独山中、上泥盆统的分界湘中地区上泥盆统牙形刺化石及地层划分

On the middle and Upper Devonian boundary by TETRACORALS in Dushan district , southern Guizhou

江苏南部中石炭世的四射珊瑚

Some middle Carboniferous TETRACORALS from southern Jiangsu

中国晚石炭世四射珊瑚地理分区

Upper Carboniferous rugose coral biogeography of China

安徽广德独山船山组四射珊瑚二新属

Two new genera of TETRACORALS EROM the Chuanshan formation in dushan , Guangde of Anhui

山西省晚古生代地层中产有丰富的四射珊瑚化石。

Shanxi Province ( Northern China ) is rich in in Late Paleozoic rugose corals .

贵州、湖南早石炭世四射珊瑚

Lower Carboniferous corals from Kweichow and Hunan

扬子区奥陶纪和志留纪四射珊瑚的起源、扩散及生物古地理关系

Origin , dispersion and biogeographic affinity of Ordovician and Silurian rugose corals in Yangtze Region

湘中地区晚石炭世四射珊瑚

Upper Carboniferous rugose corals from central Hunan

西昆仑山晚石炭世和早二叠世的复体四射珊瑚

Upper Carboniferous and lower Permian compound rugose corals in the Western Kunlun Mountains , Xinjiang

新疆塔里木盆地西西南缘泥盆石炭纪四射珊瑚

The Devonian and Carboniferous TETRACORALS from western and south - Western margins of Tarim basin , xinjiang

新疆泥盆纪四射珊瑚

Devonian tetracoralla in Xinjiang

湖南泥盆纪四射珊瑚化石组合带及中、上泥盆统界线划分松辽盆地白垩系嫩江组介形类化石带的划分及其沉积特征

A discussion of the Devonian TETRACORAL fossil assemblage zones and the determination of the boundary between the middle and Upper Devonian

从四射珊瑚试论新疆天山地区早&中石炭世的过渡层及其时代归属

The Early-Middle Carboniferous transition zone and its age assignment in the Tianshan Mountains region , xinjiang , discussed in the light of TETRACORALS

简要回顾了新中国成立以来古生代中国四射珊瑚的研究历史，试图全面反映我国在四射珊瑚研究方面取得的主要成绩。

The paper reviews the Paleozoic rugose research history in brief , concludes Paleozoic rugose corals research achievements after the founding of New China since 1949 .

记述了福建西部龙岩、宁化等地晚石炭世及早二叠世地层中发现的四射珊瑚5个新属及其典型种。

The present paper describe 5 new rugose coral genera and their typical spe - cies from the districts of Longyan and Ninghua in western Fujian .

本文重点讨论各地质时期四射珊瑚的分类和演化取得的成就，分时间、空间分布和完成人三个方面进行详细说明。

The paper discusses the achievements of rugose structure and classification in each geological time periods . Rugose classification and evolution are described in details based on geologic times , spatial distribution and describing people .

本文对青海湖湖盆南部的高寒灌丛类型及动态进行了初步探讨。湖南泥盆纪四射珊瑚化石组合带及中、上泥盆统界线划分

Alpine shrubs in southern part of Qinghai Lake Basin have been studied in fbis paper . A DISCUSSION OF THE DEVONIAN TETRACORAL FOSSIL ASSEMBLAGE ZONES AND THE DETERMINATION OF THE BOUNDARY BETWEEN THE MIDDLE AND UPPER DEVONIAN

解放后我国研究四射珊瑚的研究机构逐步建立，研究人员倍增，四射珊瑚基础资料得到大量积累，四射珊瑚的分类和演化取得重要进展。

Many rugose research institutes were founded and the number of coral specialists was increased . With the accumulation of the data concerning the rugose corals , there were some important progresses on the rugose classification and evolution .