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-----Original Message-----Don't cry, Argentina, don't cry !
From: paleonet-owner@nhm.ac.uk [mailto:paleonet-owner@nhm.ac.uk] On Behalf Of Lukas Hottinger
Sent: Thursday, February 26, 2004 7:51 AM
To: paleonet@nhm.ac.uk
Subject: Re: paleonet AGI ReportThe University of Basel, Switzerland, has decided to close the department of Earth Sciences alltogether after having reduced Paleontology to almost nothing some years ago. (There is similar treatment for Astronomy, theoretical Mathematics, Analytical Chemistry and Slavistics). For the Earth Sciences,this means a reduction of research capacities of about 20-30% on the national level. Basic argument in all cases: too few students. Such decisions are possible only since the university got some independance from the state (i.e. the Kanton Basel), with a global budget, and is run like a large firm in the pharmaceutical industry. The society has thus given up to bear the responsibility for the teaching and reseach portfolio in its number one cultural institution. However, is the closure of the Earth Sciences in particular, to some extent also our own fault, i.e. the fault of the generation of researchers active during the last 25 years in the Earth Sciences?
The big boom of the Earth Sciences is over. It came in the sixties with plate tectonics, profoundly changing our view of the world and of its history. It was triggered by new techniques in satellite positioning of ships and new seismic techniques much enhancing the resolution power, which in turn were a result from forced technical advance during world war II. Giant, unprecedented world-wide research projects such as ODP followed and produced data and material for further research still very far from being exhausted. In crystalline rocks, the understanding of chemical equilibria under high pressure and temperature and the role of water together with deep seismics, made a lot of progress and enhanced the understanding of deeper crustal processes, mountain building and volcanism. In Paleontology, many microfossil groups were discovered and inventorized permitting to refine the timescale for at least one order of magnitude, and to recognize environments of deposition of sediments in small samples, in particular from boreholes. However, basic research in order to understand paleoecological and evolutionary processes did not progress at the same pace, in spite of the discovery and/or reinterpretation of fascinating groups such as Mesozoic Mammals, Vendobonita or Archaean bacteria.
What are the innovations of the last 20 years in Earth Sciences? Sequence stratigraphy? Isotope geochemistry? Are they reflecting the genius of our time (Catastrophism) or do they really contribute to our understanding of the processes shaping Earth History? Maybe they do, to a certain extent, but they do not revolutionize our world view as plate tectonics did before. And in Paleontology, what are the innovations there besides the always necessary, never ending, basic supplementation of the inventory of organisms? Are there any? Cladistics? Counting genera or higher taxa over time? Measuring the distribution of taxa in "ecological", illdefined and poorly understood gradients? In varying the same basic ecological model mutatis mutandis for every epoch in Earth History?
Currently, what happens in Paleontology to morphological analysis in an epoch, where face recognition is a frontline research in antiterrorism; what to functional morphology in the vertebrate skeleton, when sports medecine advances rapidly in the search for the optimal functioning of the human body; what to evolutionary theory in a moment, when genetically modified organisms are set free into nature? - Nothing! Sorry, is such a science worth keeping up? This is a serious question, not a negative statement disguised behind a question mark. I can only hope for contradictions and that you join me to find some valid answers. It doesn't help to cry over lost resources.
Lukas Hottinger
PS Its carneval in Basel, time for a carneval jester's speech !
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