Séquence Personnalisée de Nombres Linéaires Croissants & Décroissants (Maximum 10 000) (A)

conductivity; (b) soil heat capacity; (c) soil thermal inertia; (d) soil heat diffusivity; (e, f) surface temperature; (g, h) daily maximum temperature; (i, j) daily minimum

Given the historic necessity of estimating missing data when his- tological sectioning is not possible [ 14 , 21 , 45 , 52 ], fossil hominin ages at death have consider- able

Literature suggests that a sharp break separates East African bovid faunas of the late Middle / early Upper Miocene from those of the late Upper Miocene.. From Fort Ternan

We have shown that geochemistry can constrain a range of conditions of core formation based on compatibility of Ni, Co, V, and Cr concentrations in present-day bulk silicate Earth,

As previously done for other samples [4,5], the goal of this study is to correlate the phase curves parameters with the physical properties of the sample, such as the size and

In September 2003, the Lidar Working Group (LWG) of the Network for Detection of Stratospheric Change (NDSC) initiated an extensive project to compare the ozone and

A common observation of Equator-S in the morningside plasma sheet outside about 9RE and at SM latitudes below 13  is that of large semiperiodic ¯uctuations of magnetic ®eld

Par exemple, le point A est sur la première ligne et son abscisse