西南石油大学学报(自然科学版) ›› 1986, Vol. 8 ›› Issue (1): 27-35.DOI: 10.3863/j.issn.1000-2634.1986.01.003

• 论文 • 上一篇    下一篇

论牙形石的发展与条件

包德宪   

  1. 地质矿产部华东石油地质局
  • 收稿日期:1900-01-01 修回日期:1900-01-01 出版日期:1986-02-20 发布日期:1986-02-20

DISCUSSION OF CONODONT DEVELOPMENT AND CONDITIONS

Bao Dexian   

  1. East China Bureau of Petroleum Geology;Ministry of Geology anb Mineral Resources
  • Received:1900-01-01 Revised:1900-01-01 Online:1986-02-20 Published:1986-02-20

摘要: 本文以牙形石(243个属)的演化特征为基础,认为符合“间断平衡论”所提出的生物演化以大演化为主的学说。牙形石的三个繁盛期与古地磁极性倒转有关。三个衰退期受到地史时期中的二大冰期,五次海平面变化和大气降雨量的影响。牙形石的绝灭由集群绝灭,气候干燥炎热、造山运动强烈等因素造成。

Abstract: Baseed on conodont (243 Genera) evolution characteristics, the conodont evolution is considered to be in agreement with the theory of "punctuated equilibrium" which suggests that macroevolution is dominative in the creature s evolutions. Three prosperous periods of conodont have relation to Palaeomagnetism Reversal. Three failing periods of conodont are influenced by two ice ages, five sea-level changes and rainfalls in the geological history time. The extinction of conodont results from the colony extinction of conodont results from the colony extinction,dry and hot weather,and moutain-making movements etc.