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Chitinozoans....what are they?
At the moment, I only have only
provided a very brief introduction to the Chitinozoa, but as time
permits, I will update the information to build a comprehensive
resource, with links to other sites of relevance.
Group: Chitinozoa
Chitinozoans are organic-walled microfossils of uncertain
origin. They are composed of 'pseudochitin', a very resistant
organic compound that allows for excellent preservation, and
recovery using the strongest acid digestion techniques.
The
group is entirely Palaeozoic, with a span of some 120 million years,
from the earliest Ordovician to the latest Devonian. They are
found only in marine sediments, and are especially abundant in black
shales, although excellent 3-D preservation has been found in
carbonates.
Chitinozoans themselves are of uncertain origin: the most accepted
hypothesis is that they are the eggs of soft-bodied metazoans, but
more than that is not known at present.
Due
to their abundance and diversity in Palaeozoic strata, chitinozoans
make an excellent biostratigraphical fossil. Detailed biozonal
schemes have been erected for many parts of the Palaeozoic, with
current research (such as my own!) constantly expanding and
integrating the available data. Due to their recognition as a
valuable biostratigraphical tool, chitinozoans have become of
interest to the hydrocarbon exploration industry, and Palaeozoic
source rocks account for a large proportion of the world's oil and
gas reserves.
Chitinozoan taxa are differentiated upon their morphological
characteristics, such as shape, ornamentation, and
appendages/processes, and there are over 1,000 species in 56 genera
to date: they have also been found on every continent. An
excellent review of chitinozoan classification was published by
Paris et al. (1999), and is well worth obtaining for anyone
interested in the group.
Professors Florentin Paris and Jacques Verniers (both world-renowned
chitinozoan experts) provide another excellent, well-illustrated
introduction to chitinozoans in the microfossils section of the new
'Encyclopaedia of Geology' published by Elsevier (reference below).
The
CIMP (Commission Internationale de
Microflore du Paléozoïque)
Subcommission on Chitinozoans has an established website with many
links and resources, and are the main international forum for
chitinozoan research. The next meeting of the CIMP is in
September 2006, in the Czech Republic: details can be found
here.
Further
reading:
PARIS, F., GRAHN, Y., NESTOR, V. and LAKOVA, I. 1999. A revised
chitinozoan classification. Journal of Paleontology, 73,
549–570.
PARIS, F. and VERNIERS, J.
2005. Chitinozoa. In SELLEY, R.C., COCKS, L. R.
M. and PLIMER, I. R. (eds). Encylcopedia of Geology: Volume
Three. Elsevier Academic Press, 428–440.
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