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Par Collection Par Auteur- SKEI (J. M.) ed. (3)
- SYVITSKI (J. P. M.) ed. (3)
- BARRIE, C. Q. (1)
- DE IURE, A. M. (1)
- LETSON, J. R. J. (1)
- SYVITSKI, J. P. M. (1)
- BURRELL, D. C. (1)
- LEWIS, A. G. (1)
- PIPER, D. J. W. (1)
- 1983 (3)
- Physical geography (3)
- Alaska ; Boca de Quadra ; Carbone ; Cycle biogéochimique ; Eau de mer ; Fjord ; Géochimie ; Géographie physique ; Milieu marin ; Océanologie ; Oxygène dissous ; Resurrection Bay (1)
- Canada ; Drumlin ; Fjord ; Fluvioglaciaire ; Glaciaire ; Géographie physique ; Géomorphodynamique ; Littoral ; Sédimentation ; Transgression marine (1)
- Eau de mer ; Fjord ; Géographie physique ; Littoral ; Milieu marin ; Nutriment ; Pelletisation ; Pellets fécaux ; Plancton ; Suspension ; Sédiment marin ; Sédimentation marine ; Taux de sédimentation (1)
- Patterns of carbon supply and distribution and oxygen renewal in two alaskan fjords in Sedimentology of fjords. (1)
- Sediment accumulation in low sedimentation, wave-dominated, glaciated inlets in Sedimentology of fjords. (1)
- The interaction of plankton and suspended sediment in fjords in Sedimentology of fjords. (1)
- flux of suspended sediments. Pelletization also allows the transport of undigested food to greater depths providing an important source of organic material to benthic sediments and food to deep-water organisms.
- Many fjords situated in lowland areas of resistant bedrock are characterized by a comparatively low fluvial sediment flux and are often dominated by wave processes. Several such fjords in Eastern Canada are used as examples to develop a generalized
- carbon supply to the basin was from fish-processing waste. The relatively high flux of allochtonous carbon into Boca de Quadra appears to consist predominantly of refractory material which does not create a significant oxygen demand within the basin.