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I too have a mixed background; a BSc in Microbiology, a PhD in marine phytoplankton, and two postdocs in Quaternary micropalaeontology. Now I am a lecturer in an Earth & Environmental Science Department teaching Palaeontology, Oceanography, and in the summer holidays a course in freshwater phytoplankton ecology/palaeoecology (being in Japan I also teach English). I have followed the recent discussion with interest and agree with many points. I also have problems deciding what I am - a palaeobiologist or a geologist with a biological interest. I seem to encounter problems in both departments. As I study systematics other (more applied) biologists view me as a 'stamp collector' with no real benefit to mankind. Whilst in geology, because Quaternary researchers have one foot in biology, I am frequently introduced to visiting geologists with a dismissive, "...oh and he's a biologist". The Head of Geophysics in one establishment once held one of my fossil taxonomic papers up by its corner and with a twisted face said "What is this ?" [incidently, he later terminated my project !!]. Reactions like these sometimes make us feel unwanted or angry, but the use of palaeontology in applied geology has already been proven. Some people call this new analytical period, the Age of the Geochemist, and say that using fossils as environmental proxies is not precise enough. Naturally their data is very useful to us, and they have a good marketing team when it comes to funding which we should try to emulate, but I think we haven't finished refining our tools yet. After all, our stratigraphy and palaeoenvironmental reconstruction is only as good as our taxonomic evaluation, i.e. the better our systematics, the better our interpretations. Look at any palaeontology-related journal and new species, new indicators and stratigraphic ranges are being reported all the time. So I fully expect a newer, better Age of the Palaeontologist in the near future. If one studies the Late Quaternary, having a biological background is essential, after all, the sediments contain only recently dead things and preservation is usually excellent. You can make use of your studies of the ecological preferences of the living species to reconstruct the past. However, once you become involved in much older sediments, your indicators are absent (i.e. nearly all the species are extinct ones with no known preferences) and past climate reconstruction becomes a nightmare for the biologist. This is definitely the realm of geologists, and palaeontologists working with older sediments are totally dependent on geological information. So I think palaeontologists can belong in both biology and geology departments - of course some departments get out of this problem by calling themselves Geoscience or Environmental Science - and that trying to put us all in one place will, as one person has already said, be bad for the survival of palaeontology in the long run. What we need to do is remain diversified, and do the same things that we have always done, but with one addition, we must learn to shout our message louder. In terms of funding: the most active and loudest of the hungry chicks always gets fed first. So we need to advertise our science at a higher profile. It also pays to have experienced palaeontologists represented on high level committees (national and international) so that our message doesn't fall on deaf ears. Ric Jordan Yamagata University Ric W. Jordan Department of Earth & Environmental Sciences, Faculty of Science, Yamagata University, Yamagata 990 JAPAN TEL: (81) 236-28-4645 FAX: (81) 236-28-4661
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