Palynological data were made available from core samples of sediments of the Brent Group which were penetrated by an exploration well. Quantification of the numerous samples supplied frequencies oi palynofacies components and microfossil amounts. The existence of both microfossil-rich and microfossil-poor samples reflects the high heterogeneity of the sediments. Factor analysis and automatic clustering of the palynofacies components show gradations from continental to marine settings and from low to high energy depositional environments. Each sample is successively analysed, processed and plotted at its driller depth on a summary sheet. The sheet shows trends, i.e. ＇＇palynological sequences＇＇ which can be compared to the genetic sequences interpreted from the sedimentological study. More reliable microfossil-rich samples are used for other multidimensional analyses. They further constrain the preliminary results and supply complementary results on microfloristic assemblages and a few other trends (sediment transport for instance). In high energy settings, the poor preservation of the biological material often precludes the identification of palynological sequences, in contrast with the low to medium energy depositional environments in which palynological sequences often match the genetic sequences defined by the sedimentological analysis. In most cases, the rare discrepancies are erased by constructive discussions between palynologists and sedimentologists.