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On Thursday April 29, 2004, the PESA Queensland
Branch monthly luncheon meeting was fortunate to have a speaker
who is one of Australias pioneering biostratigraphers, Dr
Mary Dettmann.
Mary Dettmann is currently associated with the Botany Department,
University of Queensland, and with the Queensland Museum where she
is involved with research on plant fossils. She graduated from the
University of Melbourne and obtained an MSc from that university
under the supervision of Isabel Cookson, universally recognised
as an important pioneer of palynology. Her PhD studies in Cambridge
were on Cretaceous palynofloras from southeastern Australian basins.
Since returning to Australia in the early 1960s, she has consulted
to exploration companies and government institutions on evaluating
palynofloras from sequences in the majority of eastern Australian
depositional basins. Her research interests have been focused on
southern Gondwanan floras of Mesozoic-Palaeogene age, and on the
evolution and history of Australias present-day vegetation.
Mary was involved in developing one of the first detailed Mesozoic
to Tertiary biostratigraphic zonations for the eastern Australian
basins in the 1960s. This early scheme formed the basis for modern
schemes and many parts of this scheme are still in use today.
Palynology in hydrocarbon exploration: biostratigraphy
and beyond
Abstract
Palynology (the study of acid insoluble microfossils, most of which
are of plant origin) has made significant contributions to hydrocarbon
exploration worldwide for well over half a century. In Australia,
initial palynological studies were concentrated on coal sequences,
but since the discovery of oil in northwest Western Australia during
the 1950s, palynology increasingly has been recognised as an effective
tool for dating and biostratigraphic correlation of marine and non-marine
sequences.
The discipline became an integral adjunct to oil exploration during
the 1960s - 1980s, and palynostratigraphic zonations were proposed
for Palaeozoic-Tertiary sequences represented in the majority of
Australias sedimentary basins. By the late 1980s, a comprehensive
zonal scheme comprising concurrent dinocyst and spore-pollen zones
was published for the Australian Mesozoic, and the scheme was correlated
with previously proposed palynostratigraphies. Similarly for the
Palaeozoic, palynostratigraphic zonations have been compiled. Recent
work has been directed at refining zonal schemes in individual basins,
with particular emphasis on establishing sequence surfaces which
define bioevents reflecting shifts in depositional environments,
and modifications to source floras related to changes in base levels
and/or climate. Nevertheless, exploration geologists are sometimes
confronted by an array of disparate palynological zonations for
the same sequence. This may have stemmed from different concepts
in palynotaxon differentiation, conceptual differences in what are
and what are not stratigraphically and/or temporally significant
palynoevents (eg., first/last appearances or total range/relative
frequencies of a taxon or group of taxa), different data sets, and
variations within those data sets resulting from differences in
sampling and/or preparation procedures.
Palynology has been an important tool in hydrocarbon exploration
and will continue to offer valuable evidence in resolving stratigraphic
and a suite of other problems, not only in hydrocarbon exploration,
but also in other fields of earth and biological sciences. Palynology
has proven an effective and complementary tool in thermal maturation
and source rock studies, and it provides important insights into
palaeoenvironments and palaeoclimates. Moreover, it offers indubitable
and complementary evidence on the composition of contemporaneous
marine and terrestrial floras which provided much of the raw material
for hydrocarbons already extracted and being sought for by exploration
companies.
The presentation provided an overview, with examples, of what palynology
has offered in the past, and focussed on its future potential in
resolving problems associated with hydrocarbon exploration.
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