Oligo-Miocene peatland ecosystems of the Gippsland Basin and modern analogues
Vera A Korasidis, Malcolm W Wallace, Barbara E Wagstaff, Guy R Holdgate
GLOBAL AND PLANETARY CHANGE | ELSEVIER SCIENCE BV | Published : 2017
A detailed examination of the brown coal facies preserved in the Latrobe Valley Morwell 1B seam indicates that the type of peat-forming environment and the associated hydrological regime are the main factors influencing the development of lithotypes in brown coal deposits. New palynological data from the Morwell 1B seam suggests that each respective lithotype in the lightening-upwards lithotype cycles was deposited in a particular depositional environment that was characterised by a distinct floral community. The laminated dark lithotype represents a fire-prone emergent marsh that grew on the margins of a coastal lagoon and/or freshwater swamp. This facies grades into the dark lithotype, rep..View full abstract
AGL Loy Yang and GHD are gratefully acknowledged for enabling the sampling of the M1B seam from the Loy Yang Open Cut Mine. We would particularly like to thank Ben Jansen (GHD) for facilitating our visits to the Loy Yang Open Cut Mine and to Dr. Michael Shawn-Fletcher (University of Melbourne) for his assistance in developing methods used for palynological processing. We are also grateful to Professor Joan Esterle and Dr. Tim Moore for constructive and helpful comments on the manuscript. An Australian Government Research Training Program Scholarship is supporting V. A. Korasidis.