% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Dutta:57651,
      author       = {Dutta, S. and Steiner, M. and Banerjee, S. and Erdtmann,
                      B.-D. and van Jeevankumar, S. and Mann, U.},
      title        = {{C}huaria circularis from the early {M}esoproterozoic
                      {S}uket {S}hale, {V}indhyan {S}upergroup, {I}ndia:
                      {I}nsights from light and electron microscopy and
                      pyrolysis-gas chromatography},
      journal      = {Journal of earth system science},
      volume       = {115},
      issn         = {0253-4126},
      address      = {Bangalore},
      publisher    = {Indian Acad. of Sciences},
      reportid     = {PreJuSER-57651},
      pages        = {99 - 112},
      year         = {2006},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Chuaria circularis (Walcott 1899) from the Suket Shale of
                      the Vindhyan Supergroup (central India) has been
                      reinvestigated for its morphology and chemical composition
                      using biostatistics, electron microscopy and pyrolysis-gas
                      chromatography. Morphology and microscopic investigations
                      provide little clues on the specific biological affinity of
                      Chuaria as numerous preservational artifacts seem to be
                      incorporated. On the contrary, the predominance of
                      n-aliphatic pyrolysates of presently studied Chuaria from
                      India rather supports an algal affinity. Moreover, the
                      reflectance of C. circularis can be used to obtain a
                      comparative maturity parameter of the Precambrian sediments.
                      The review of the age and geographical distribution of C.
                      circularis constrains that this species cannot be considered
                      as an index fossil for the Proterozoic time.},
      keywords     = {J (WoSType)},
      cin          = {ICG-V},
      ddc          = {000},
      cid          = {I:(DE-Juel1)VDB51},
      pnm          = {Geosysteme - Erde im Wandel},
      pid          = {G:(DE-Juel1)FUEK405},
      shelfmark    = {Geosciences, Multidisciplinary / Multidisciplinary
                      Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000236375500008},
      doi          = {10.1007/BF02703028},
      url          = {https://juser.fz-juelich.de/record/57651},
}