Transferrin binding to K562 cell line : Effect of heme and sodium butyrate induction

Experiments demonstrating the existence of receptors for iron-saturated transferrin on K562 cells are described. Binding of ¹²⁵I-labelled transferrin is rapid, saturable and reversible, and can be specifically inhibited by unlabelled transferrin, but not by other proteins. The number of receptors determined by Scatchard analysis significantly decreased when K562 cells moved from the exponential to the quiescent phase of growth. Induction by hemin or sodium butyrate resulted in a marked reduction of transferrin binding. This phenomenon was due entirely to reduction in the number of receptors and was without effect on the affinity of interaction. The effect of butyrate and hemin on the number of transferrin receptors in other hematopoietic cell lines was investigated. Butyrate on the various cell lines was variable in its effect, whereas hemin constantly elicited a significant reduction in the number of transferrin receptors.     

Influence de la teneur en oxygène sur la sensibilité de certains stades juvéniles deSitophilus oryzae etS. granarius au dioxyde de carbone

Résumé Certains stades juvéniles de charançons des céréales du genreSitophilus ont été soumis à un séjour prolongé dans des compositions gazeuses modifiées par le dioxyde de carbone (CO₂).Les auteurs se sont placés dans des conditions de teneur en CO₂ constante (50%), associée à des teneurs en oxygène comprises entre 4 et 20%, pour étudier les conditions d'une synergie entre l'effet spécifique du CO₂ et la présence d'une forte teneur résiduelle en oxygène. Les effets ont été observés sur les stades juvéniles les plus évolués (larves et nymphes) des espècesS. oryzae (L.) etS. granarius (L.), (Coleoptera: Curculionidae).L'accroissement de la vitesse de mortalité chezS. oryzae est significative avec l'augmentation de la pression partielle d'oxygène. Cet effet de synergie provoqué par l'oxygène n'est pas significatif avecS. granarius, bien qu'il existe aussi avec cette espèce une tendance à l'amélioration de l'efficacité insecticide à court terme avec les mélanges à forte teneur résiduelle en oxygène.Il en est déduit des hypothèses sur les effets des mélanges gazeux à composition modifiée par le CO₂ au niveau de la physiologie générale de ces insectes, qui est très difficile à appréhender directement à cause du mode de développement des stades juvéniles des charançons (formes cachées dans le grain).     

Histological study of embryogenesis and organogenesis from anthers ofVitis rupestris du Lot cultured in vitro

Summary Anthers ofVitis rupestris du Lot were cultured in vitro at the uninucleate stage of the microspore, in order to investigate the histology of embryogenic and organogenic processes in this genotype. Microspores divided in the anther loculi resulting in the formation of globular structures with a ruptured exine. Somatic embryogenesis and, occasionally, caulogenesis and rhizogenesis occurred in calli produced from all anther tissues except the endothecium. The initial cell of the embryoid was surrounded by a jacket layer when situated deep within the callus. When the embryoid's initial cell was situated in the peripheral callus, a cutinized wall was present and the three-celled proembryoid was almost always segmented, showing the same embryonal type as the zygotic proembryo. Root differentiation and elongation and cap differentiation occurred during the growth phase in liquid medium. The mature root was diarch and contained cells with calcium-oxalate raphides, as seen in vivo. No starch or tannin deposition was ever observed in the mature embryoids.Abbreviations 6-BAP 6-benzylaminopurine - CC3 Nitsch and Nitsch (1969) basal medium - CS cross section - 2,4-D 2,4-dichlorophenoxy-acetic acid - LS longitudinal section     

Origines du peuplement mammalien en Afrique du Nord durant le miocène terminal

The late Miocene North African mammalianassemblage is considered here from three viewpoints: survivals, extinctions, and immigrations. The Eurasiatic affinities of the large mammals slightly prevail over the Ethiopian affinities. Amongst the North African large mammals, 4 to 8 taxa are Eurasiatic immigrants, while 4 to 6 are of Subsaharian origin. Contrarily, the micromammalian fauna is highly endemic, with only one species, a murid (Paraethomys miocaenicus), considered here as being related to an Asiatic form (Karnimata darwini). Our study of Eurasian and African Miocene faunas reveals that during the late Astaracian-early Turolian interval, the Saharo-Arabic belt permitted very little latitudinal faunal exchanges. However, during the middle and late Turolian such faunal exchanges became frequent. The micromammal record unequivocally indicates that a brief period of faunal exchange occurred between Africa and western Europe at the end of the Miocene, corresponding with the Messinian Salinity Crisis. The increased intercontinental faunal exchange between Africa and Eurasia during the late Miocene coincides with, and counterbalances the extinction of more than 10 taxa at the Mio/Pliocene boundary.     

Le prétendu rhinocéros de Nouvelle Calédonie est un marsupial (Zygomaturus diahotensis nov. sp.): Solution d'une énigmeet conséquences paléogéographiques

The first mammalian remain ever found in NewCaledonia is an upper tooth found by golddiggers in the Plio-Pleistocene terrace from the Diahot river. This tooth, given to the Muséum national d'Histoire naturelle (Paris) in 1876, was determined as a rhinoceros tooth and then completely forgotten. Its detailed study shows that it belongs to Zygomaturus, a large marsupial diprotodontid genus whose story is rather complicated. The Diahot tooth represents a new species of Zygomaturus, Z. diahotensis nov. sp., close to Z. trilobus from the Australian Pleistocene. That kinship suggests a Plio-Pleistocene land connection between Australia and New Caledonia, whereas till now New Caledonia was supposed to be separated from Australia since the end of the Cretaceous, because of the total absence of indigenous mammals, fossil or recent, in New Caledonia. The latest geological studies in the East Pacific do not contradict our hypothesis.     

Revision du genre LycopodiopsisB. Renault, 1890

The study of imprints of Lycopsida from Permianof the Gondwana has permitted to specify the organisation of the leaf cushions and their variation in the genus LycopodiopsisB. Renault. The presence of a ligula is showed off. The invalidity of the genera Cyclodendron and Lycopodiophloios is demonstrated, and the species refered to these genera must be refered to the genus Lycopodiopsis for which an emended diagnosis is proposed.     

Observations on Syracosphaera rhombica sp. nov.

A spherical coccosphere and two collapsed coccospheres composed of monomorphic rhombic coccoliths were encountered in 2005 in the Java upwelling system of the SE Indian Ocean, while a further two specimens with elongate coccospheres were recently found in the Gulf of Mexico. All of the specimens were collected from the lower photic zone (75–160 m). The coccoliths possess a proximal flange, a slightly flared wall with a serrated distal margin, and a relatively plain central area structure comprised only of overlapping laths. The taxon appears to be an undescribed species of the Syracosphaera nodosa group, so we describe it herein as Syracosphaera rhombica sp. nov.     

Climatic control on vegetation and sedimentary dynamics during the Miocene (Burdigalian to Langhian) in northeastern Tunisia

Palynological and sedimentological analyses were performed on Miocene sediments of North-East Tunisia in order to detect the changes in depositional environments, including those linked to eustasy, along with changes in vegetation and climate. The specific integration of palynological (pollen and dinocysts) and sedimentological (including facies analysis) data indicate that shallow marine settings persisted until the early Burdigalian–Langhian, and that open marine environments developed progressively in the late Langhian. Since the early Serravallian, deltaic environments developed under a fluctuating, but predominantly warm climate. The palynological data support a subtropical climate during the Burdigalian, with tropical conditions prevailing at the Langhian–Serravallian transition. The observed high frequency values of megathermic and mega-mesothermic pollen taxa represent the vegetation response to the Miocene climatic optimum (MCO).