Zoeken
Zoeken kan via de modus 'eenvoudig zoeken' (één veld) of uitgebreid via 'geavanceerd zoeken' (meerdere velden). Zo kan je bv. zoeken op een combinatie van een auteursnaam (auteur), een jaartal (jaar) en een documenttype.
Boekenmand
Nuttige resultaten kan je aanvinken en toevoegen aan een mandje. De inhoud hiervan kan je exporteren of afdrukken (naar bv. PDF).
RSS
Op de hoogte blijven van nieuw toegevoegde publicaties binnen uw interessegebied? Dit kan door een RSS-feed (?) te maken van jouw zoekopdracht.
[ meld een fout in dit record ] | mandje (0): toevoegen | toon |
![]() |
Spatial and temporal variability of meiobenthic density in the Blanes submarine canyon (NW Mediterranean) Romano, C.; Coenjaerts, J.; Flexas, M.M.; Zuniga, D.; Vanreusel, A.; Company, J.B.; Martin, D. (2013). Spatial and temporal variability of meiobenthic density in the Blanes submarine canyon (NW Mediterranean). Prog. Oceanogr. 118: 144-158. dx.doi.org/10.1016/j.pocean.2013.07.026
In: Progress in Oceanography. Pergamon: Oxford,New York,. ISSN 0079-6611; e-ISSN 1873-4472, meer
| ![]() |
Beschikbaar in | Auteurs |
|
Trefwoord |
|
Auteurs | Top | |
|
|
Abstract |
Our multidisciplinary approach allowed to study the hydrodynamics and sedimentary processes in the Blanes Canyon that characterize it as highly heterogeneous environment. Inside the canyon area, particle fluxes were higher than on the slope area, increased from autumn to spring and mostly consisted of lith-ogenic material. Moreover the canyon's locations experienced more intense bottoms' currents and sediment disturbance, being reflected in a greater variability of meiobenthic densities, both between stations and sampling times than on the open slope. No clear trends (e.g. declining densities) associated with increasing depths were observed. Contrary in the open slope, current velocities were relatively lower compared with the canyon area and showed lower temporal variability. At the same time, the nutritional quality of the particle fluxes at deeper grounds were higher, probably allowing the meiofaunal densities not to change over time. In conclusion, the meiobenthos in our system apparently showed a higher temporal variability, inside the canyon area, strongly affected by particle fluxes or erosive and sediment-mixing processes linked to current modifications induced by the canyon topography. |
Top | Auteurs |