首页> 外文期刊>GSA Bulletin >Experimental studies in Precambrian paleontology: Structural and chemical changes in blue-green algae during simulated fossilization in synthetic chert
【24h】

Experimental studies in Precambrian paleontology: Structural and chemical changes in blue-green algae during simulated fossilization in synthetic chert

机译:前寒武纪古生物学的实验研究:人造石模拟化石过程中蓝绿藻的结构和化学变化

获取原文
获取原文并翻译 | 示例
           

摘要

Experimental data concerning the effects of diagenesis and fossilization on soft-bodied microorganisms (particularly algae preserved in siliceous sediments) have been obtained through systematic monitoring of morphological and organic chemical changes in filamentous blue-green algae (Lyngbya majuscula, Oscillatoriaceae) during simulated fossilization in synthetic chert. With increasing time and temperature, there were tendencies toward reddening, darkening, and fragmentation of algal filaments, reduction in the size of algal cells and sheaths, destruction of micellar order in sheaths (with consequent loss of bire-fringent character), coalescence of trichomes, and destruction of intracellular components with preferential preservation of sheaths and cell walls. In addition, some algal filaments were damaged by growth of quartz spherulites, producing artifactual morphologies that appear to have natural counterparts in Precambrian fossiliferous cherts. Original algal hydrocarbons, and particularly normal alkanes, were relatively stable, but several previously absent hydrocarbons were produced through decomposition of other organic compounds. Isoprenoid compounds, chlorins, and probably porphyrins were derived from the degradation of algal chlorophyll. The C13PDB value of algal carbon was unaffected in most experiments but decreased by 3 under extreme time and temperature conditions. Results of this study suggest trends in the morphological degradation of naturally silicified algae, demonstrate that certain morphologies are artifacts of the silicification process, and suggest possible explanations of observed organic chemical trends in recent and ancient sediments. Key Words: Precambrian paleontology • experimental fossilization • silicification • morphological fossils • chemical fossils • blue-green algae • hydrocarbons • pigments • stable carbon isotopes
机译:通过系统的 监测,获得了有关成岩作用和化石 对软质微生物(尤其是硅质沉积物中保存的藻类 )的影响的实验数据。合成fossil石模拟化石过程中 丝状蓝绿藻(Lyngbya majuscula,Oscillatoriaceae) 的形态和有机化学变化。随着 时间和温度的升高,藻丝趋于变红, 变暗和碎裂,藻类细胞和鞘的尺寸减小。 ,破坏鞘中的胶束 顺序(从而导致双指特征丧失),毛状体的 聚结和优先破坏细胞内成分 保护鞘和细胞壁。此外,某些藻类细丝被石英 球晶的生长所破坏,产生的人为形态看起来像 在前寒武纪化石ifer石中具有天然的对应物。 sup> 原始的藻类碳氢化合物,特别是正构烷烃,相对稳定,但是通过其他有机化合物的分解产生了一些先前不存在的碳氢化合物。 类异戊二烯化合物,二氢卟酚和可能的卟啉 源自藻类叶绿素的降解。在大多数实验中,藻类碳的C 13 PDB 值均不受影响,但在极端时间和温度下 降低了3。 该研究结果表明天然硅化藻类的形态降解趋势 ,表明某些形态 是硅化过程的产物,并且建议在最近和 古代沉积物中观察到的有机化学趋势的可能 解释。 关键词:前寒武纪古生物学•实验化石•硅化作用•形态化石•化学化石•蓝藻•碳氢化合物•色素•稳定的碳同位素

著录项

  • 来源
    《GSA Bulletin》 |1976年第1期|117-129|共13页
  • 作者

    JOHN H. OEHLER;

  • 作者单位

    CSIRO, Baas Becking Geobiological Laboratory, Box 378, Canberra City, A.C.T. 2601, Australia;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号