Over het archief
Het OWA, het open archief van het Waterbouwkundig Laboratorium heeft tot doel alle vrij toegankelijke onderzoeksresultaten van dit instituut in digitale vorm aan te bieden. Op die manier wil het de zichtbaarheid, verspreiding en gebruik van deze onderzoeksresultaten, alsook de wetenschappelijke communicatie maximaal bevorderen.
Dit archief wordt uitgebouwd en beheerd volgens de principes van de Open Access Movement, en het daaruit ontstane Open Archives Initiative.
Basisinformatie over ‘Open Access to scholarly information'.
one publication added to basket [302982] |
An assessment of bottom current controlled sedimentation in Pacific Ocean abyssal environments
In: Marine Geology. Elsevier: Amsterdam. ISSN 0025-3227; e-ISSN 1872-6151, meer
| |
Author keywords |
Geomorphology; Sedimentary basins; Bottom currents; Contourites; Tropical Pacific |
Abstract |
The effect of the circulation of polar-sourced dense waters on the deep seafloor is still largely unknown. This paper presents multibeam bathymetric evidence for the existence of present-day contourite drifts on the central Pacific ocean at depths ranging between 4000 and 5000 m, based on the identification of their diagnostic erosive (moats, linear moats, furrows and abyssal sinuous channels) and depositional (plastered, elongated separated and abyssal contourite-fan drifts) contourite morphological features. These contourite drifts display a patchy distribution, sculpted by the secondary flows of the Lower Circumpolar Water (LCPW) and the North Pacific Deep Waters (NPDW), as well as local dynamics of the flow in the form of internal waves and bottom currents modulated by tides, which are capable of accelerating the typically sluggish bottom currents and contribute to the erosion, transport and deposition of sediments. The formation of contourites is also predominantly controlled by the presence of large-scale tectonic and volcanic features (ridges, seamounts and deep elongated valleys), which affect the morphology and distribution of the basins and induce the acceleration of bottom currents. Overall, this study allows to re-assess the effects, distribution and significance of bottom-current controlled sedimentation in abyssal environments, where examples of contourite features are still rather scarce in part because of the technical challenges and their remote location, but also because the effect of bottom currents is not well known in the central oceanic basins and only capable of marginally affecting their sedimentological record. |
Dataset |
- Flanders Marine Institute; Renard Centre of Marine Geology - Ugent (2019). Global contourite distribution database, version 3. Available online at https://www.marineregions.org, meer
|
IMIS is ontwikkeld en wordt gehost door het VLIZ.