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Aretz et al_2011.pdf - ORBi - Université de Liège

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Kölner Forum Geol. P<strong>al</strong>äont., 19 (2011)<br />

M. ARETZ, S. DELCULÉE, J. DENAYER & E. POTY (Eds.)<br />

Abstracts, 11th Symposium on Fossil Cnidaria and Sponges, <strong>Liège</strong>, August 19-29, 2011<br />

_________________________________________________________________________________________________________<br />

ARCHAEOCYATHA: Computer-ai<strong>de</strong>d i<strong>de</strong>ntification of genera<br />

A<strong>de</strong>line KERNER 1 & Françoise DEBRENNE 2<br />

1 CNRS, UMR 7207, Centre <strong>de</strong> Recherche sur la P<strong>al</strong>éobiodiversité <strong>et</strong> les P<strong>al</strong>éoenvironnements, Laboratoire<br />

Informatique <strong>et</strong> Systématique, MNHN, Département Histoire <strong>de</strong> la Terre, Bâtiment <strong>de</strong> Géologie, CP48, 57<br />

rue Cuvier, 75005 Paris, France; kerner@mnhn.fr<br />

2 13 rue du long foin, 91700 Sainte Geneviève <strong>de</strong>s bois, France; francoise.<strong>de</strong>brenne@gmail.com<br />

Archaeocyatha are a key-group in different fields of Life and Earth History. Assigned to various phyla,<br />

they are now recognized as a class within the Phylum Porifera. The discovery of living aspiculate sponges<br />

with a c<strong>al</strong>cified skel<strong>et</strong>on by scuba divers in sub-marine caves of the Caribbeans in the late seventies, has<br />

renewed interest in the biology, phylogeny and ecology of related fossils with previously problematic<br />

status, such as Archaeocyatha. Morphologic<strong>al</strong> structures shows a great similarity in growth pattern,<br />

immune reactions, and types of asexu<strong>al</strong> reproduction (interc<strong>al</strong>icular budding) in both groups. Presently,<br />

the class consists of 6 or<strong>de</strong>rs, 120 families and 307 genera.<br />

They are an important group of marine sessile organisms <strong>al</strong>most entirely Early Cambrian, with some<br />

relicts persisting into the Middle and Late Cambrian. Due to counter-clockwise rotation of Gondwana, the<br />

only archaeocyaths species of post-Early Cambrian age are found in Antarctica which <strong>al</strong>one remained in<br />

low latitu<strong>de</strong>s.<br />

They provi<strong>de</strong> reliable basis for biozonation in key regions. The first stage subdivision based on<br />

Archaeocyatha was established on Siberian Platform. Morocco, Western Europe, Austr<strong>al</strong>ia, China and<br />

Laurentia have provi<strong>de</strong>d region<strong>al</strong> sc<strong>al</strong>es.<br />

Reef dwellers, they are necessary substrate for c<strong>al</strong>cified cyanobacteria and cement but they seldom<br />

produced a true framework to reefs. The Cambrian system is gener<strong>al</strong>ly characterized by the absence of any<br />

climate indicators useable as constraints for tectonic reconstructions. Then the distribution of Early<br />

Cambrian reefs may provi<strong>de</strong> suitable constraints to s<strong>et</strong>tle tropic<strong>al</strong> p<strong>al</strong>eolatitu<strong>de</strong>s. Early Cambrian provinces<br />

and re<strong>al</strong>ms are <strong>de</strong>limited using an exhaustive compendium of archaeocyathan genera.<br />

Since Archaeocyatha are important Cambrian organisms, it is necessary for scientists <strong>de</strong><strong>al</strong>ing with<br />

P<strong>al</strong>eozoic rocks to i<strong>de</strong>ntify those fossils. But keys, easy to use and adapted even to incompl<strong>et</strong>e specimens,<br />

are lacking. Up to now, a knowledge-database in English, carried out with the software XPER², is now<br />

available online free: http://www.infosyslab.fr/archaeocyatha<br />

It comprises the 307 v<strong>al</strong>id genera <strong>de</strong>scribed with 120 <strong>de</strong>scriptors (85 morphologic<strong>al</strong> and ontogen<strong>et</strong>ic, 8<br />

stratigraphic and geographic and 27 taxonomic).<br />

This site comprises information about Archaeocyatha (morphology, bibliography…), d<strong>et</strong>ailed<br />

<strong>de</strong>scriptive cards with figures of type-specimens and eventu<strong>al</strong>ly addition<strong>al</strong> figures to illustrate<br />

morphologic<strong>al</strong> d<strong>et</strong>ails. Information of the database is used to build an i<strong>de</strong>ntification unit as an interactive<br />

key with free access.<br />

Results of this study <strong>al</strong>low the standardization of currently used <strong>de</strong>scriptors, the <strong>de</strong>finition of a revised<br />

terminology and the possibility to i<strong>de</strong>ntify synonyms. The need of establishing new characters and/or<br />

states of characters may appear during the work.<br />

Fig. 1 is an example for the i<strong>de</strong>ntification module. The interface is composed of three parts: on the left,<br />

the list of <strong>de</strong>scriptors to be chosen by the user, at the center, information about the <strong>de</strong>scriptors (<strong>de</strong>finitions,<br />

figures) and on the right, the lists of remaining and discar<strong>de</strong>d taxa. I<strong>de</strong>ntification consists of the rep<strong>et</strong>ition<br />

of successive steps: firstly, the choice of a <strong>de</strong>scriptor, secondly, the choice of one or sever<strong>al</strong> states of the<br />

<strong>de</strong>scriptors and fin<strong>al</strong>ly a confirmation with the submit button. At each v<strong>al</strong>idation, lists of remaining and<br />

discar<strong>de</strong>d taxa and list of possible <strong>de</strong>scriptors are updated. Descriptors can be sorted to facilitate<br />

i<strong>de</strong>ntification.<br />

With this interactive key, different lists (i.e. <strong>al</strong>l Austr<strong>al</strong>ian genera during Atdabanian…) may be rapidly<br />

established. Another possibility is to bring into light similarities and differences (i.e. b<strong>et</strong>ween genera of the<br />

same family).<br />

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