La longue séquence de Marchésieux: reconstitution de paléoenvironnements marins durant le premier cycle glaciaire de l'hémisphère nord

International audienceA l'échelle des cinq derniers millions d'années, les enregistrements paléoclimatiques restitués par les sédiments océaniques illustrent le contrôle des paramètres orbitaux (précession, obliquité et excentricité) sur le climat global. La tendance au refroidissement qui accompagne la fin du Néogène est ainsi marquée, vers -2,4 Ma, par le développement rapide des calottes de glace de l'hémisphère nord (Shackleton et al., 1984). Alors que l'histoire du climat global restituée par les enregistrements océaniques est sans cesse précisée, les données concernant l'évolution des environnements continentaux et côtiers au cours de ces changements restent essentiellement fragmentaires. Le forage effectué à Marchésieux (Manche; Normandie) a permis de réaliser une étude pluridisciplinaire de la signature de ce premier cycle glaciaire de l'hémisphère nord (Prétiglien). Les premiers résultats stratigraphiques, paléoenvironnementaux (eustatisme, température, paléobathymétrie) sont présentés

La longue séquence pliocène de Marchésieux - Résultats analytiques et premiers résultats

National audienceLe sondage intégralement carotté de Marchésieux a permis d'atteindre l'objectif fixé dans le projet AR42 du BRGM : l'analyse paléoclimatique du premier épisode glaciaire de l'hémisphère nord (Prétiglien, -2,4 Ma) et probablement le premier rafraîchissement de -3,1 Ma. Les 159,3 m de sédiments datés du Reuvérien et du Prétiglien ont déjà livré une quantité importante d'informations aussi bien climatiques que paléoenvironnementales. De par sa position géographique privilégiée et de par son environnement côtier, la "Longue sequence" de Marchésieux a précisé les modalités de la séquence de dégradation climatique en milieu continental et marin à nos latitudes moyennes. La méthodologie fortement pluridisciplinaire, le plus souvent il très haute résolution, permet d'affiner notablement les modalités de la réponse de chaque environnement au changement climatique, et apparaît, en ce sens, beaucoup plus riche que les études monodisciplinaires classiques. Ainsi, les réponses zoologiques, phytosociologiques, sedimentologiques et géochimiques au stimulus climatique externe peuvent être comparées et calibrées

On the systematic position of the oldest insular ruminant Sardomeryx oschiriensis (Mammalia, Ruminantia) and the early evolution of the Giraffomorpha

Sardomeryx oschiriensis is the oldest insular ruminant known (Burdigalian of Oschiri, Sardinia, Italy). Only two isolated upper dentitions compose the type material. The first phylogenetic hypothesis proposed Sardomeryx to be closely related to the Giraffoidea and especially the Late Miocene Sardinian derived giraffid Umbrotherium. Description of new specimens from Laerru (Burdigalian, Sardinia, Italy), including lower teeth and decidual premolars, leads to a reinterpretation of the phylogenetic position of Sardomeryx and of the early evolutionary history of the Giraffomorpha. Based on our phylogenetic hypothesis, Sardomeryx is nested within the Giraffomorpha as a basal Palaeomerycoidea. Sardomeryx may have originated from south-western Europe before the separation of the Corsica-Sardinia Block during the earliest Miocene. The enigmatic latest Oligocene Bedenomeryx from the south-west France is also considered as a basal (and the most ancient) member of the Palaeomerycoidea. Including Bedenomeryx in the Palaeomerycoidea lineage would place the origin of the Giraffoidea, the sister family of Palaeomerycoidea, within the Oligocene. Bedenomeryx is characteristic of arid south-western France, directly echoing the advanced condition observed in the Sardomeryx dentition (e.g. high crowned teeth, absence of the external postprotocristid on lower molar, reduction in length of the premolar row) typical for insular ruminants in arid environments

Iberomeryx minor (Mammalia, Artiodactyla) from the Early Oligocene of Soulce (Canton Jura, NW Switzerland): systematics and palaeodiet

The primitive ruminant genus Iberomeryx is poorly documented, as it is essentially only known from rare occurrences of dental remains. Therefore, the phylogeny and palaeobiology of Iberomeryx remain rather enigmatic. Only two species have been described: the type species I. parvus from the Benara locality in Georgia, and the Western European species I. minor reported from France, Spain, and Switzerland. Iberomeryx savagei from India has recently been placed in the new genus Nalameryx. All these localities are dated to the Rupelian and correspond mainly to MP23 (European mammal reference level). Based on the short height of the tooth-crown and the bunoselenodont pattern of the molars, Iberomeryx has often been considered as a folivore/frugivore. The I. minor remains from Soulce (NW Switzerland) are preserved in Rupelian lacustrine lithographic limestones. One specimen from this locality represents the most complete mandible of the taxon with a partially persevered ramus. Moreover, the unpreserved portion of the mandible left an imprint in the sediment, permitting the reconstruction of the mandible outline. Based on a new description of these specimens, anatomical comparisons and Relative Warp Analysis (24 landmarks) of 94 mandibles (11 fossil and 83 extant) from 31 ruminant genera (10 fossil and 21 extant) and 40 species (11 fossil and 29 extant), this study attempts a preliminary discussion of the phylogeny and the diet of the species I. minor. The results permit to differentiate Pecora and Tragulina on the first principal component axis (first Relative warp) on behalf of the length of the diastema c/cheek teeth, the length of the premolars and the angular process. The mandible shape of I. minor is similar to those of the primitive Tragulina, but it differs somewhat from those of the extant Tragulidae, the only extant family in the Tragulina. This difference is essentially due to a stockier mandible and a deeper incisura vasorum. However, in consideration of the general pattern of its cheek teeth, I. minor as well as possibly Nalameryx should be considered to represent the only known primitive Tragulidae from the Oligocene. Moreover, I. minor should have been a selective browser (fruit and dicot foliage) but, similarly to small Hypertragulidae and Tragulidae, may also have exceptionally consumed animal matter