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'.
Megathrust earthquake drives drastic organic carbon supply to the hadal trench
Kioka, A.; Schwestermann, T.; Moernaut, J.; Ikehara, K.; Kanamatsu, T.; McHugh, C.M.; dos Santos Ferreira, C.; Wiemer, G.; Haghipour, N.; Kopf, A.J.; Eglinton, T.I.; Strasser, M. (2019). Megathrust earthquake drives drastic organic carbon supply to the hadal trench. NPG Scientific Reports 9: 1553. https://dx.doi.org/10.1038/s41598-019-38834-x
In: Scientific Reports (Nature Publishing Group). Nature Publishing Group: London. ISSN 2045-2322; e-ISSN 2045-2322, meer
| |
Auteurs | | Top |
- Kioka, A.
- Schwestermann, T.
- Moernaut, J., meer
- Ikehara, K.
|
- Kanamatsu, T.
- McHugh, C.M.
- dos Santos Ferreira, C.
- Wiemer, G.
|
- Haghipour, N.
- Kopf, A.J.
- Eglinton, T.I.
- Strasser, M.
|
Abstract |
The giant 2011 Tohoku-oki earthquake has been inferred to remobilise fine-grained, young surface sediment enriched in organic matter from the slope into the >7 km deep Japan Trench. Yet, this hypothesis and assessment of its significance for the carbon cycle has been hindered by limited data density and resolution in the hadal zone. Here we combine new high-resolution bathymetry data with sub-bottom profiler images and sediment cores taken during 2012–2016 in order to map for the first time the spatial extent of the earthquake-triggered event deposit along the hadal Japan Trench. We quantify a sediment volume of ~0.2 km3 deposited from spatially-widespread remobilisation of young surficial seafloor slope sediments triggered by the 2011 earthquake and its aftershock sequence. The mapped volume and organic carbon content in sediment cores encompassing the 2011 event reveals that this single tectonic event delivered >1 Tg of organic carbon to the hadal trench. This carbon supply is comparable to high carbon fluxes described for other Earth system processes, shedding new light on the impact of large earthquakes on long-term carbon cycling in the deep-sea. |
IMIS is ontwikkeld en wordt gehost door het VLIZ.