Palynology of Archean microfossils (c. 3.0 Ga) from the Mount Grant area, Pilbara Craton, Western Australia: Further evidence of biogenicity

被引:32
|
作者
Grey, Kathleen [1 ]
Sugitani, Kenichiro [2 ]
机构
[1] Geol Survey Western Australia, Dept Mines & Petr, Perth, WA 6004, Australia
[2] Nagoya Univ, Dept Environm Engn & Architecture, Grad Sch Environm Studies, Nagoya, Aichi 4648601, Japan
基金
日本学术振兴会;
关键词
Palynology; Archean; Microfossils; Mount Grant; Pilbara; SEDIMENTARY PETROLOGY; CONTINENTAL-CRUST; MT; GOLDSWORTHY; EVOLUTION; CHERT;
D O I
10.1016/j.precamres.2009.02.003
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Palynological techniques have only rarely been applied to Archean rocks, mainly because of concerns about contamination. However, where microstructures are abundant and well documented, palynology can add considerably to interpretations based on thin-section examination. A modified palynological preparation method, which avoids vigorous physical or chemical methods that might cause the fragmentation of fragile specimens, was applied to black chert from the c. 3.0 Ga Farrel Quartzite of the Mount Grant area, Pilbara Craton, Western Australia, known to contain abundant microstructures of putative biogenic origin. Four main morphological types have been reported from chert thin sections: threads, films, hollow spheres and spindles. These microstructures exhibit morphological and chemical signatures consistent with a biological origin as well as showing features indicative of taphonomic degradation. Nevertheless, the possibility remains that they are artefacts. Similar structures have been attributed to physical processes, such as the accretion of fine particulate matter that has subsequently been redistributed as a result of crystal growth. By extracting structures palynologically, we have increased the probability of a biogenic origin. Firstly, examination of the morphology free of the encompassing matrix demonstrates that they are indeed three-dimensional structures with complex morphology; secondly, the extraction of entire specimens militates against them being particulate matter aggregations, which would simply disintegrate during preparation and thirdly, the chemicals used remove silicates and most other minerals, confirming the organic composition of the structures. To date, we have extracted films, hollow spheres and a few poorly preserved spindles, but preparation continues. The fact that the specimens retain their morphological integrity during palynological extraction argues strongly in favour of a biogenic origin for the microstructures. Crown Copyright (C) 2009 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:60 / 69
页数:10
相关论文
共 12 条
  • [1] Taxonomy and biogenicity of Archaean spheroidal microfossils (ca. 3.0 Ga) from the Mount Goldsworthy-Mount Grant area in the northeastern Pilbara Craton, Western Australia
    Sugitani, Kenichiro
    Grey, Kathleen
    Nagaoka, Tsutomu
    Mimura, Koichi
    Walter, Malcolm R.
    [J]. PRECAMBRIAN RESEARCH, 2009, 173 (1-4) : 50 - 59
  • [2] Diverse microstructures from Archaean chert from the mount goldsworthy-mount grant area, pilbara craton, western australia: Microfossils, dubiofossils, or pseudofossils?
    Sugitani, Kenichiro
    Grey, Kathleen
    Allwood, Abigail
    Nagaoka, Tsutomu
    Mimura, Koichi
    Minami, Masayo
    Marshall, Craig P.
    Van Kranendonk, Martin J.
    Walter, Malcolm R.
    [J]. PRECAMBRIAN RESEARCH, 2007, 158 (3-4) : 228 - 262
  • [3] 3.0 Ga ocean floor metamorphism in the cleaverville area, pilbara craton, western Australia
    Shibuya, T
    Kitajima, K
    Komiya, T
    Maruyama, S
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 2003, 67 (18) : A426 - A426
  • [4] 3.1-GA TUFF FROM THE SHOLL BELT IN THE WEST PILBARA - FURTHER EVIDENCE FOR DIACHRONOUS VOLCANISM IN THE PILBARA CRATON OF WESTERN-AUSTRALIA
    HORWITZ, RC
    PIDGEON, RT
    [J]. PRECAMBRIAN RESEARCH, 1993, 60 (1-4) : 175 - 183
  • [5] Taxonomic Framework and Possible Affinities of Diverse and Complex Microfossils from c 3 0 Ga Chert in the Pilbara Craton, Western Australia
    Sugitani, K.
    Grey, K.
    Nagaoka, T.
    Mimura, K.
    Walter, M. R.
    [J]. ORIGINS OF LIFE AND EVOLUTION OF BIOSPHERES, 2010, 40 (06): : 525 - 525
  • [6] Evidence for early LREE-enriched mantle source regions:: Diverse magmas from the c. 3.0 Ga Mallina Basin, Pilbara Craton, NW Australia
    Smithies, RH
    Champion, DC
    Sun, SS
    [J]. JOURNAL OF PETROLOGY, 2004, 45 (08) : 1515 - 1537
  • [7] Lack of late-accreted material as the origin of 182W excesses in the Archean mantle: Evidence from the Pilbara Craton, Western Australia
    Archer, Gregory J.
    Brennecka, Gregory A.
    Gleissner, Philipp
    Stracke, Andreas
    Becker, Harry
    Kleine, Thorsten
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 2019, 528
  • [8] Volcanic degassing, hydrothermal circulation and the flourishing of early life on Earth: A review of the evidence from c. 3490-3240 Ma rocks of the Pilbara Supergroup, Pilbara Craton, Western Australia
    Van Kranendonk, MJ
    [J]. EARTH-SCIENCE REVIEWS, 2006, 74 (3-4) : 197 - 240
  • [9] Mo-Cr isotope evidence for a reducing Archean atmosphere in 3.46-2.76 Ga black shales from the Pilbara, Western Australia
    Wille, Martin
    Nebel, Oliver
    Van Kranendonk, Martin J.
    Schoenberg, Ronny
    Kleinhanns, Ilka C.
    Ellwood, Michael J.
    [J]. CHEMICAL GEOLOGY, 2013, 340 : 68 - 76
  • [10] Presence of evolved continental crust in Archean Pilbara craton, Western Australia: Evidence from Re-Os isotopic systematics of 3.4Gyr cherts
    Suzuki, K
    Shimizu, F
    Okamoto, M
    Hattori, Y
    Minami, M
    Shimoda, G
    Tatsumi, Y
    Adachi, M
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 2002, 66 (15A) : A755 - A755