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              <p>The dynamics of the river beds in the lower sections of the Marne and the Oise rivers areanalyzed in relation to the evolution of the slopes during the Lateglacial and the Holocene. The resultsof the study of the morphosedimentary responses are confirmed by the palaeoenvironmental variationsrecorded by malacological, palynological and archaeological data. The Lateglacial evolution appearsto be tightly linked to the climatic changes. Two main periods of sedimentation can be attributed to thePleniglacial I Lateglacial transitional phase and to the Younger Dryas; they are separated by an erosionand soil formation phase which may have occurred during the B0lling and АИегфа phases. At thebeginning of the Holocene, an important phase of vertical cutting can be allocated to the first half of thePreboreal period ; thereafter river beds tend to be more stable. During the Boreal and the Atlanticphases, the stabilization of the slopes and of the river beds by the vegetation cover plays an importantrole in the morphogenic evolution. The detrital input remains very low while the river beds are slowlyfilled in by highly organic material, often dominated by peat formation processes. During the secondhalf of the Atlantic, the various indicators do not show any environmental degradation, but the pollendata show, during the Middle Neolithic times, the expansion of agricultural activities with punctualopening of the landscape and rude- ration. The first episodes of silt sedimentation occur during thesecond half of the Subboreal, in relation to the erosion of the loess covering the slopes. The riverdischarges increase during the Bronze Age, thus frequently creating channels which will be filled induring the La Tène period. During the Roman times, the accumulation of sediment in the mean waterchannels continues in the main valleys; afterwards, the sedimentary dynamics seem to slow down withthe decreasing agricultural pressure during the Late Middle Ages. An important erosion crisis occursduring the modern times, marked by an important deposition of silt in the valleys of minor tributaries.</p>
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              <p>La dynamique des lits fluviaux des bassins aval de la Marne et de l'Oise est analysée enterme de réponse à l'évolution des versants durant le Tardi - et le Postglaciaire. Les réponsesmorphosédimentaires observées sont confrontées aux variations paléoenvironnementales révélées parles données archéologiques, palynologiques et malacologiques. L'évolution tardiglaciaire apparaîtétroitement contrôlée par les fluctuations climatiques. Elle comporte deux principales phases desédimentation, attribuables à la transition Pléniglaciaire-Tardiglaciaire et au Dryas récent et séparéespar une phase de creusement et de pédogenèse durant le B0lling et l'Aller0d. L'Holocène débute parune phase de creusement importante au cours de la première moitié du Préboréal, puis les lits tendentà se stabiliser. Durant le Boréal et l'Atlantique, la fixation des versants et des lits fluviaux par lacouverture végétale joue un rôle déterminant. Les apports détritiques sont très réduits et les litssubissent un colmatage progressif à forte tendance organique, où les processus de tourbogenèsejouent un rôle important. Durant la seconde partie de l'Atlantique, les différents indicateurs ne semblentpas témoigner d'une atteinte importante du milieu naturel mais les données palynologiques révèlent ledéveloppement des activités agricoles du Néolithique moyen traduites par un développement desrudérales et des céréales et une ouverture ponctuelle des paysages. Les premiers colmatageslimoneux liés à l'érosion de la couverture loessique des versants surviennent pendant la secondemoitié du Subboréal; puis les écoulements s'amplifient durant l'Âge du Bronze. Ils déterminentl'apparition fréquente de chenaux, qui seront surtout remblayés lors de La Tène. Durant la périoderomaine, le colmatage des lits mineurs des grandes vallées se parachève, puis les dynamiquessédimentaires semblent se ralentir. Une importante crise d'érosion, marquée par une sédimentationlimoneuse importante dans les vallées secondaires est finalement mise en évidence durant la périodemoderne.</p>
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