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贵州瓮安陡山沱组球状化石元素地球化学浅析
  • ISSN号:0371-5736
  • 期刊名称:地质论评
  • 时间:0
  • 页码:3014-3018
  • 语言:中文
  • 分类:P[天文地球]
  • 作者机构:[1]中国地质科学院地质研究所,北京100037, [2]中国地质科学院地层古生物重点实验室,北京100037, [3]贵州大学资源与环境工程学院,贵阳550003
  • 相关基金:中国地质科学院地层古生物重点实验室专项研究基金(编号JB0705 JB0902); 现代古生物学及地层学国家重点实验室专项研究基金(编号103104); 中国地质调查局工作项目(编号1212010611802 1212010911071); 国家自然科学基金资助项目(编号40772013)的成果
  • 相关项目:陡山沱期磷酸盐化生物群中后生动物化石的再研究
中文摘要:

本文利用电子探针微区分析技术(EPMA),首次分析了采自贵州瓮安北斗山磷矿区陡山沱组外壁呈瘤状及多边形板片状的磷酸盐化球状化石的元素地球化学含量,包括常量元素氧化物含量和部分稀土元素含量。经初步对比发现:具瘤状及板片状外壁的两类球状化石,由内至外常量元素含量的变化趋势大体相似,表明归入同一生物大门类的可能性较大;与磷块岩全岩样品相比,球状化石中除了P、Ca含量更高以外,Na、Ni、Zn和Cl有较高的含量,而且S含量和轻稀土元素Ce等含量均偏高,可能表明球状化石在趋于弱还原的沉积环境中被磷酸盐化保存;K、Al、Mg、Ti、Mn、Fe2+和Si等含量均显著低于围岩。由于还缺乏后生动物的相关对比资料,目前还不能为球状微体化石的生物学属性争议提供元素地球化学方面的确切对比意见,但分析的结果不倾向于归属藻类、硫细菌和海绵动物。这方面的尝试为深化球状化石的亲缘关系研究提供了新途径和新材料。

英文摘要:

The Ediacaran Doushantuo Formation in Weng'an and Fuquan areas of the Guizhou Province in southern China hosts high-grade phosphorus ore deposits and exceptionally well-preserved phosphatic microfossils that are commonly less than 1 mm in diameter. Earlier studies attributed these fossils to algae or acritarchs. In the last decade,researchers found that the spherical microfossils,in a large proportion,show metazoan embryonic development features with early cleavage stages. Thus these spherical microfossils have been considered as diploblast or triploblast embryos and resting eggs of early animals. However,reliable fossils similar to blastula,gastrula embryos,fossils of larvae after hatching,and particularly,the corresponding body fossils of these animal embryos have never been found in the relevant strata. This phenomenon challenges the interpretation that these globular microfossils are animal embryos. Because the major uncertainty on these fossils is whether they are animals or plants,a detailed geochemical analyses across the fossils may help to reveal the differences (between animal and plant) in the composition of cell membrane / wall and cell inclusions,the pattern of physiological metabolism,and the phosphatized mechanisms in particular depositional environments. On this basis and in combination with morphological comparison with the Cambrian microfossils and modern metazoan embryos,elemental geochemistry across the spherical microfossils ( "embryos") of the Weng'an biota may provide new information for better understanding the genetic affinity of the Doushantuo globular fossils. In this paper,the author analyzes the microfossils collected from Weng'an and Fuquan areas in Guizhou by electron probe micro-analyzer (EPMA) to obtain trace elemental geochemistry across the globular fossils. For comparison purposes,two types of fossils have been analyzed,including fossils with tumor-like outer wall and those with polygonal plate-shaped outer wall. Comparing results from these fossils and th

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期刊信息
  • 《地质论评》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学技术协会
  • 主办单位:中国地质学会
  • 主编:杨文采
  • 地址:北京阜成门外百万庄路26号中国地质学会期刊处
  • 邮编:100037
  • 邮箱:georeview@cags.ac.cn
  • 电话:010-68999804
  • 国际标准刊号:ISSN:0371-5736
  • 国内统一刊号:ISSN:11-1952/P
  • 邮发代号:2-382
  • 获奖情况:
  • 中国期刊方阵“双效”期刊
  • 国内外数据库收录:
  • 美国化学文摘(网络版),美国地质文献预评数据库,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:23413