Déterminer Chaque Question sur l'Addition et la Soustraction des Nombres Jusqu'à 20 à l'Aide d'une Droite Graduée (A)

As the proxy data constraints are met using a fairly wide range of forcing functions in the PRP/TP space, the model suggests that changes in inorganic weathering of DIC and ALK are

Comparison between direct and retrieved microphysical parameters (CONC: cloud droplet concentration, LWC: liquid water content, DM: mean diameter, Def: mean e€ective diameter and

Biodegradation tests of var- ious single organic compounds present in cloud water per- formed on 60 microbial strains (bacteria and yeasts) previ- ously isolated from cloud

To confirm the abnormal nature of Group 2 AMS fabric and to check unambiguously the hypothesis of an inverse fabric induced by SD grains (Potter & Stephenson 1988), we measured

Since larger stress perturbations are expected in the vicinity of fractures, with an intensity that depends on fracture size, we expect the stress-driven nucleation in the

Stage 4: At the latitude of the continental block, the slab starts to break off by a necking process localized at the continent/ocean boundary at ~300 km depth (Figure 8) because of

Late Cretaceous stratigraphy and paleoceanographic evolution in the Great Australian Bight Basin based on results from IODP Site

The first Mesozoic amphipod, Gammaroidorum vonki, found in the Early Cretaceous Wealden 168. of the Weald, is morphologically somewhat similar to a diminutive recent gammaroid