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San Miniato and the history of Earth Science
Written by Boldone   
Monday, 24 December 2007

The hills around San Miniato, Pisa District in Tuscany, are a paleontological heritage. Within an alluvial to open shelf, cyclothemic succession, a testimonial of early late Pliocene Milankovitch-type sea level cycles , lie several shell beds of different nature (Benvenuti et al 2007 ). Collectors of fossil marine molluscs were active here since the Renaissance and in the sixteenth century the first modern hypotheses on the nature of fossils were being formulated. Contemporary of Andrea Cisalpino, one Michele Mercati (1541-1593) from San Miniato, collected minerals, rocks and fossils for the Natural History cabinet of the Pope in Rome and wrote about the origin of fossils in his Metallotheca vaticana , published in 1729 (the value of his work has been recognized by one of the earliest science historians such as Séguier ).

Conus mercati in shell bed

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Back to the Basin
Written by Boldone   
Monday, 03 December 2007

Reference sections for the Paleogene are for the most part located in the Paris Basin (Gely & Lorenz 1991), but much of what could be seen back in the days is no longer visible, due to intense cropping and natural wood cover. There seem not to be much awareness for the maintenance of geological heritage from the national authorities, so that the local action by museums and amateurs for the restoration of classical localities is more than welcome. Among the middle Lutetian localities newly made available for study are Grignon and La Ferme de l’Orme, in the Yvelines, and Fleury-La-Riviere, in the Marne.

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Lower Paleozoic exceptional biota
Written by Boldone   
Wednesday, 31 October 2007
The journal Geology has recently published two reports on exceptionally well-preserved fossil biotas from marginal marine sediments, one of Silurian (von Bitter et al. 2007), the other of late Ordovician age (Young et al. 2007), both from Canada. This findings are particularly important since testimonials to life in an environment that is generally little represented in the fossil record, due to the high-energy conditions met with at the shoreline, making biotic remains easily destroyed.
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