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地球学报  2009 

湖北保康白竹陡山沱组磷酸盐化微化石新资料及其地层意义

DOI: 10.3975/cagsb.2009.04.05

Keywords: 陡山沱组,磷酸盐化,微化石,保康,湖北

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Abstract:

周传明(2004)曾报道湖北保康白竹磷矿陡山沱组磷块岩中含有与瓮安生物群类似的磷酸盐化微化石,包括多细胞藻类Wengania,Paramecia,Thallophyca;大型具刺疑源类Meghystrichosphaeridium,Knollisphaeridium;球状蓝菌类Archaeophycus;丝状蓝菌类Siphonophycus,Obruchevella以及新发现的珍珠球藻Bacatisphaera。最近,作者对保康白竹磷矿陡山沱组进行了重新考察和采样研究。结果除发现上述微化石外,还发现大型具刺疑源类Papillomembranacompta,Appenendisphaerasp.;球状化石Megasphaerainornata,Megaclonophycusonustus以及峡东地区常见的丝状蓝菌化石湖北萨洛米藻(Salomehubeiensis)等。研究表明,本文报道的保康白竹磷矿陡山沱组的含化石层位与峡东地区陡山沱组第二段及贵州瓮安上磷矿层下部的微化石层位相当,组合面貌相似。新资料证明峡东地区陡山沱组第二段出现的疑源类下组合,包括多细胞藻类、大型复杂疑源类、球状化石、球状和丝状蓝菌化石等,区域分布广泛,层位稳定,具有重要生物地层学意义。

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