Réflexion sur l'utilisation des auxiliaires entomophages contreDiprion pini [Hym. Diprionidae]

Résumé Le problème de la lutte biologique en forêt, par utilisation d'entomophages indigènes, est discuté dans le cas d'un hyménoptère, le diprion du pin,Diprion pini L. Des études de dynamique des populations montrent que le schéma de progression spatiale des populations de cet insecte dans le sud du Bassin Parisien semble se renouveler à chaque pullulation. De plus les parasites représentent un véritable “facteur clé”. Leur incidence varie notamment de génération en génération: en faible nombre au début d'une gradation, ils ne peuvent alors en empêcher le développement; mais ensuite leur multiplication assure une régression brutale du ravageur. Dans ces conditions, des interventions assez peu onéreuses et faciles à réaliser, comme de simples transports de matériel parasité pourraient être efficaces; elles supposent toutefois le développement d'un foyer initial d'infestation. En revanche l'élevage d'espèces régulatrices commeAchrysocharella ruforum Krausse etPleolophus basizonus Grav. permettrait d'assurer la préservation permanente des massifs forestiers.

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Summary The spatial pattern of insect populations progression in southern “Bassin Parisien”, showed by population dynamics studies, seems to happen again for every outbreak. Parasites are moreover a true “key-factor”. Their effect is quite different from one generation to another one; scarce at the beginning of an outbreak, they cannot stop its evolution; but then, their increase allows a brutal collape of the pest. In such a case, cheap and easily achieved operations as simple carryings of parasited insects may be efficient, but they need the development of a first infestation focus. In return breeding of regulating species asAchrysocharella ruforum Krausse andPleolophus basizonus Grav. would be able to sure forest stands permanently.

     

Neumark-Nord 2 – A multiphase Middle Palaeolithic open-air site in the Geisel Valley (Central Germany)

The lake basin Neumark-Nord 2 (NN 2) is located in the Geisel Valley in Saxony-Anhalt (Germany). It was scientifically investigated between 2003 and 2008. The sediment sequence, which is about 10 to 11 m thick, consists of limnic deposits, mostly silts mixed with clays and sands. Sedimentological as well as palynological, malacological and palaeomagnetic investigations, supported by absolute datings, date the entire sequence into the Eemian and Early Weichselian. Within the deposits several archaeological find horizons were discovered. Neumark-Nord 2/2 (NN 2/2) at the beginning of the Eemian and Neumark-Nord 2/0 (NN 2/0) with an early Weichselian were the most important archaeological horizons. Both find horizons represent former lake shore sites, where numerous crushed animal bones and other faunal debris were found, which can be regarded as remains of hunted game. With regard to the rich lithic material, both find horizons differ remarkably. In NN2/2, a simple artefact spectrum with a certain Levallois component and a dominance of denticulated, notched and laterally retouched specimens. In NN 2/0, on the other hand, bifacial tools such as backed knives and sometimes finely retouched scrapers are dominant, while the Levallois component fades completely into the background. Thus, NN 2 is one of the few open-air sites in archaeological landscape of Central German where several middle Palaeolithic find horizons occur in superposition.     

Upper Cenomanian bivalves from the Guir Basin (southwestern Algeria): Order Veneroida

The Upper Cretaceous rocks are widely distributed and well exposed in south Algeria and consist in beds rich in macrofauna. For the first time, twenty veneroid species (Bivalvia) are systematically described from the upper Cenomanian deposits of the Guir Basin. While three species were reported since long before [Granocardium desvauxi (Coquand), G. productum (J. de C. Sowerby) and Glossus aquilinus (Coquand)]; Lucina fallax Forbes, Crassatella (Rochella) tenuicostata (Seguenza), Protocardia hillana (J. Sowerby), G. productum (J. de C. Sowerby) var. byzacenica (Pervinquière), Arctica cordata (Sharpe), A. humei (Cox), A. inornata (d’Orbigny), A. picteti (Coquand), Tenea delettrei (Coquand), Paraesa faba (J. de C. Sowerby), Meretrix desvauxi (Coquand) were previously unknown from the Cretaceous of Algerian Sahara. Because of reduced degree of preservation, Sphaera cf. corrugata J. Sowerby, Maghrebella cf. forgemoli (Coquand), Maghrebella sp., Granocardium cf. carolinum (d’Orbigny), Protocardia sp. and Meretrix sp. are tentatively determined. The studied material, found in the lower part of the “Calcaires de Sidi Mohamed Ben Bouziane” Formation, evidences palaeobiogeographic affinities occurring over a wide geographical area: from North Africa, southern Europe to Middle East and India. The present study provides new information to the knowledge of the upper Cenomanian palaeobiology of the studied region.     

Découverte de Thyrsoporella pseudoperplexa Granier et Braik, 2002 (algue dasycladale) dans le Kimméridgien inférieur du bassin d'Essaouira (marge atlantique marocaine)

A dasycladacean alga recently attributed to the species Thyrsoporella pseudoperplexa Granier and Braik 2002, has been discovered within the Jurassic sediments of the Atlantic domain. This alga, only found in the Tethysian domain, was identified in the Early Kimmeridgian sediments of the Essaouira basin (Morocco).     

Stratégie cynégétique et mode de vie à l'Azilien ancien dans le Bassin parisien : les apports de l'exploitation des chevaux du Closeau (niveau inférieur ; Rueil-Malmaison, Hauts-de-Seine)

The Closeau's lower level (Rueil-Malmaison, Hauts-de-Seine) brought evidence of Early Azilian occupations, in which the horse were the main prey. This paper present the zooarchaeological results of the equid's processing, according to the occupation units 4 and 46. The horse acquisition show that chase-approach hunts were the tactic employed, by a single individual or some small bands. The equids hunts' repetition testify that such activities took place at different moments of the year, especially in autumn and at the end of winter-springtime. These data allow a better understanding of the reasons that can explain why all phases of the animal processing were found in the inside of the occupation structures. The consumption of horse's meat and offal seems to take place only partly in situ. The units 4 and 46 can be interpreted as hunting camps, periodically use par Early Azilian bands. Such function of the site may signify that the mobility of these bands could integrated some traits of logistical pattern to a certain extent, but until now their lifeway stay unclear without new discoveries.     

Les industries acheuléennes de la France septentrionale

The excavations of several open air sites in Northern France and, especially in the Somme basin, have given numerous data concerning the age and the environment of the human occupations for the period from MIS 12 to MIS 8. The quality of the raw material and the function of the different sites have a great effect on the composition of the lithic assemblages as it has been seen for the different sites located near the confluence of the Somme and Avre (Cagny-la Garenne, Cagny-l’Épinette, Ferme de l’Épinette, Gentelles). The characteristics of the lithic industries of Gouzeaucourt show the complexity of the transition from Lower to Middle Palaeolithic.     

New Patagonian baurusuchids (Crocodylomorpha; Notosuchia) from the Bajo de la Carpa Formation (Upper Cretaceous; Neuquén,Argentina): New evidences of the early sebecosuchian diversification in Gondwana

The Bajo de la Carpa Formation (Santonian) of the Neuquén basin (southwestern Argentina) has one of the most complete crocodyliform records of South America, together with the Adamantina and Marília formations of Brazil. In this contribution we report two fragmentary individuals from two different localities of the Bajo de la Carpa Formation: a middle-sized individual (MLP 26-IV-30-2), represented by postcranial remains from the Boca del Sapo locality and a large-bodied individual (MACN Pv-RN 1150), consisting only of snout elements from Paso Córdoba locality. Despite the remains of both specimens are fragmentary, they display anatomical characters of a specialized notosuchian carnivore clade: Baurusuchidae. Our phylogenetic analysis recovers these new individuals as non-baurusuchine baurusuchids, although they take multiple phylogenetic positions on the different most parsimonious trees. These new remains highlight the relevance of the Bajo de la Carpa Formation for understanding the rise of notosuchians during the Late Cretaceous.     

Roveacrinids (Crinoidea,Roveacrinida) from the Cenomanian-Turonian of southwest Algeria (Saharan Atlas and Guir Basin)

In the southwestern part of Algeria, the Cenomanian-Turonian marine deposits build up a prominent ledge in a perched syncline (Ksour Mountains, western Saharan Atlas) or at high radius of curvature (Guir Basin). The petrographical analysis of the Cenomanian-Turonian deposits of the Ksour Mountains and of the Guir Basin reveals unexpected assemblages of roveacrinoidal ossicles comparable with those formerly reported from the Tinrhert area. For the first time, isolated ossicles of genuine and undisputable Roveacrinidae are illustrated. Three sections, Djebel Rhoundjaia (western Saharan Atlas), Berridel and Kénadsa (Guir Basin), were scrutinized to recognize the microcrinoidal sections within the carbonate microfacies and to compile the successive occurrence of respective roveacrinid taxa (besides the classical search for standard index microfossils) in an attempt to pinpoint more precisely the position of the Cenomanian-Turonian boundary (C/T B). These assemblages are particularly morphologically and taxonomically diverse with three species of genus Roveacrinus and one of genus Orthogonocrinus. The presence of Saccocomidae (Applinocrinus) is especially unusual in such stratigraphic levels. The relative abundance and diversity of Roveacrinidae evidence a peak when approaching the C/T B. Such an event is recurring in the latest Cenomanian in various Tethyan and Atlantic areas. These fluctuations are consistent with a high surface-water productivity just before the C/T B.     

Étude biostratigraphique et paléoenvironnementale des diatomées pyritisées de l'intervalle Paléocène supérieur-Éocène inférieur du sondage de Saint-Josse (France)

This paper presents the results of a biostratigraphic analysis of pyritized diatom assemblages in the Saint-Josse core (CC82) located in the northern part of the Paris basin (coordinates: X =555?000, Y =307?324 and Z =56.9 m). During the Paleocene-Eocene this locality was situated in a small bight of the North Sea Basin. The results are obtained from sediments of the Thanet and Mont-Bernon group equivalents belonging to the Paleocene-Eocene interval. Thirteen samples were studied and eleven contain pyritized diatoms. By epigenesis, the siliceous frustule of the diatom is changed into a pyritized skeleton with all the ornamentation very well preserved such as the velum, the areolae, the labiate processes, etc. Dispersive X-Ray analyses show this complete replacement of silica by pyrite. Another form of pyritization is crystallization of pyrite (in cubes, pyritohedrons, octahedrons, framboids) in internal cavities of the diatoms to produce internal moulds, also called steinkerns, which preserve the external morphology of the diatoms and some details such as the girdle. Despite pyritization, diatoms can often be recognized at the species level; brackish and marine species were observed but no fresh water specimens were encountered. Pyrite is easily altered into iron oxides. In outcrops, pyritized diatoms can be obscured or destroyed by oxidation. We have chosen borehole samples for this study to avoid the affects of weathering. Deposits from the Sorrus Unit (of the Thanet Group) have low abundances of pyritized diatoms (3 to 25 specimens per sample). This unit contains allochtonous diatom assemblages comprising Actinoptychussenarius, Coscinodiscus morsianus var. morsianus, and Coscinodiscus morsianus var. moelleri. Sample 34.31-34.45 from this unit is particularly interesting. It contains three specimens of Paralia siberica var. laevis, which is typical of an estuarine or littoral paleoenvironment, and corresponds to the more continental deposit of the Sorrus Unit. Seven samples, taken in the Argile de Saint-Aubin Unit (from the Mont-Bernon Group), contain more than 200 pyritized diatoms and between 9 to 16 different species per sample. A brackish assemblage (Actinoptychus senarius, Coscinodiscus commutatus and Stellarima microtrias) and a marine assemblage (C. morsianus var. morsianus, Coscinodiscus var. moelleri, Fenestrella antiqua, Odontellaheibergii, Rhizosolenia sp. 1 and Trinacria regina) are observed. The brackish assemblage expands in the upper part of the Saint-Aubin Unit indicating more widespread brackish paleoenvironmental conditions. Pyritized diatoms are important fossil markers in the Paris basin mainly when siliceous fossils (silicoflagellates or radiolarians) and others microfossils (foraminifers and dinoflagellates) are very poor or absent. Two diatom assemblages have been identified in the Saint-Josse borehole. The first assemblage D1, comprising C. morsianus var. moelleri (high occurrence), C. morsianus (a few) and T. regina (rare), is recorded in the Sorrus, La Calotterie, Bois Gorguette, Le Goulet and lower Saint-Aubin Units. The second assemblage D2, characterized by great abundance of F. antiqua and decreasing numbers of C. morsianus species, is found in the upper part of the Saint-Aubin Unit. These diatom assemblages can be correlated with other biozonations established in the North Sea basin and based on nannoplankton and diatoms (King, 1983), diatoms (Mitlehner, 1996) and calcareous nannoplankton (Martini, 1971). F. antiqua and C. morsianus var. moelleri are the more important diatom species encountered. F. antiqua (previously named Coscinodiscus sp. 1, King, 1983) is the fossil marker used by King to define his NSP4 biozone. The base of NSP4 corresponds to the lowest occurrence of F. antiqua and the top is marked by the highest occurrence of this species. The Sorrus, La Calotterie, Bois Gorguette, Le Goulet and Saint-Aubin (“Sparnacian” stage) Units, the last one comprising F. antiqua (increasing to acme), correspond to the NSP4 zone of King (1983). The Mont-Hulin and Château de la Bruyère Units correspond probably to the NSP5 zone of King (1983). F. antiqua and C. morsianus var. moelleri were also used by Mitlehner (1996) to differentiate the NSP4a zone (low abundance of F. antiqua and abundance of C. morsianus var. moelleri) from the NSP4b zone (great abundance and acme of F. antiqua). The abundance of C. morsianus var. moelleri is recorded in the lower part of Saint-Aubin Unit and the abundance of F. antiqua (high peak at 46% in the sample 17.87) is found in the upper part of Saint-Aubin Unit. Therefore, Sorrus, La Calotterie, Bois Gorguette, Le Goulet and the lower part of Saint-Aubin Units are correlated with the NSP4a zone and the upper part of Saint-Aubin Unit with the NSP4b zone. By correlating the calcareous nannoplankton biozonation (NP) of Martini (1971) with the biozonation of King (1983), adapted by Mitlehner (1996), the boundary between the NP9 and NP10 zones could be located in the 18.75-17.87 interval and the NP10-NP11 boundary at the top of Saint-Aubin Unit. Lithostratigraphic correlations between the units of the Saint-Josse borehole (Paris basin) and the formations of the North Sea basin can be established. The great abundance of C. morsianus var. moelleri and the great abundance (including acme) of F. antiqua are respectively recorded in the Sele and Balder Formations. Therefore, the interval Sorrus/lower Saint-Aubin Units is correlated with the Sele Formation and upper part of Saint-Aubin Unit with the Balder Formation.