2010
DOI: 10.1130/g30895.1
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Efficient burial of carbon in a submarine canyon

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Cited by 69 publications
(50 citation statements)
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“…The sediment is predominantly of terrigenous silt and clay origin (Alt-Epping et al, 2007). The sediment is actively transported from the upper continental shelf to the canyon and out onto the abyssal plain by sediment gravity flows that occur on annual or longer timescales and are particularly vigorous during periods of winter storms (de Stigter et al, 2007;Masson et al, 2010). The currents flowing down the canyon lead to cycles of resuspension and deposition, alternating with intervals during which the sediment is deposited on the sea bed (de Stigter et al, 2007).…”
Section: Study Areamentioning
confidence: 99%
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“…The sediment is predominantly of terrigenous silt and clay origin (Alt-Epping et al, 2007). The sediment is actively transported from the upper continental shelf to the canyon and out onto the abyssal plain by sediment gravity flows that occur on annual or longer timescales and are particularly vigorous during periods of winter storms (de Stigter et al, 2007;Masson et al, 2010). The currents flowing down the canyon lead to cycles of resuspension and deposition, alternating with intervals during which the sediment is deposited on the sea bed (de Stigter et al, 2007).…”
Section: Study Areamentioning
confidence: 99%
“…Large concentrations of organic C and biopolymeric C (BPC) have been observed within the middle section of the Nazaré Canyon, suggesting this canyon may act as a sink for OM burial (Schmidt et al, 2001; T. Amaro et al: The trophic biology of the holothurian Molpadia musculus 2007; Masson et al, 2010;Pusceddu et al, 2010). Sediments and OM are transported from the continental shelf down the canyon and into the deep sea (de Stigter et al, 2007;Oliveira et al, 2007;de Leo et al, 2010;Vetter et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
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“…Submarine canyons play a crucial role in the redistribution of carbon and anthropogenic materials derived from marine primary production and terrestrial runoff (Weaver et al, 2004). They are considered major pathways for the transportation and burial of organic carbon, acting as buffers for carbon storage; burial of organic carbon in marine sediments moderates atmospheric CO 2 levels on geological time scales (Masson et al, 2010).…”
Section: Submarine Canyons On the Continental Slope (Eunis A681)mentioning
confidence: 99%
“…They can represent either a sink for particulate matter of autochthonous origin (i.e. derived from biological productivity of surface waters and/or exported from the land), or a source of organic material fueling the deep ocean's interior by lateral transport (Buscail and Germain, 1997;Bauer and Druffel 1998;Canals et al, 2006;Sampéré et al, 2008;Sanchez-Vidal et al, 2008;Masson et al, 2010;Pusceddu et al, 2010). Nevertheless, the extent to which such material is transported and distributed downslope is not consistent along latitudinal or longitudinal gradients, nor constant in time, mainly due to differences in hydrodynamic, topographic, climatic and ecological conditions (Liu et al, 2010).…”
Section: Introductionmentioning
confidence: 99%