2007
DOI: 10.1016/j.margeo.2007.04.016
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Provenance of organic matter and nutrient conditions on a river- and upwelling influenced shelf: A case study from the Portuguese Margin

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Cited by 45 publications
(24 citation statements)
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“…BIT index) showed that terrestrial organic matter decreases seawards. Furthermore, a study off the Douro River (Alt- Epping et al, 2007) established that δ 13 C TOC could be used as an indicator of the source (marine vs. terrestrial) of organic matter in this zone. δ 13 C TOC at 100 m water depth has values around −24‰, showing that organic matter is a mixture of terrestrial and marine sources.…”
Section: Tablementioning
confidence: 99%
“…BIT index) showed that terrestrial organic matter decreases seawards. Furthermore, a study off the Douro River (Alt- Epping et al, 2007) established that δ 13 C TOC could be used as an indicator of the source (marine vs. terrestrial) of organic matter in this zone. δ 13 C TOC at 100 m water depth has values around −24‰, showing that organic matter is a mixture of terrestrial and marine sources.…”
Section: Tablementioning
confidence: 99%
“…Our δ 13 C OC data from the marine surface sediments indicate that the majority of the OC on the Portuguese shelf is of marine origin. Even in the estuary, only 50 to 65 % of OC content is estimated to be of terrestrial origin (Alt-Epping et al, 2007). The Tagus River acts mainly as a supplier of terrigenous lithogenic particles to the coastal ocean, while the majority of the terrestrial organic matter is retained inside the estuary (Jouanneau et al, 1998).…”
Section: Characteristics Of the Bulk Organic Mattermentioning
confidence: 99%
“…Besides internal tides that operate more vigorously at the proximal sections of the canyon at time scales of hours (upper section) to weeks (middle section), sediment gravity flows may occur on a yearly or longer timescales and turbidity currents strong enough to transport sand down the canyon take place on a centennial timescale (de Stigter et al, 2007). The material captured in the canyon consists predominantly of terrigenous silt and clay (Alt-Epping et al, 2007;de Stigter et al, 2007;Arzola et al, 2008) and several studies point to chlorophyll-a and organic carbon concentrations that are significantly higher in the canyon than in the adjacent open slope sediments (García et al, 2008;Ingels et al, 2009;Pusceddu et al, 2010).…”
Section: Study Areamentioning
confidence: 99%
“…Further increased concentrations observed in the Nazaré and Cascais canyons (Garcia and Thomsen, 2008;Ingels et al, 2009;Pusceddu et al, 2010) are likely to result from their effectiveness to capture sediment from lateral transport along the shelf. The Nazaré Canyon is very active and captures predominantly material of terrigenous origin (Alt-Epping et al, 2007;de Stigter et al, 2007;Arzola et al, 2008). This refractory carbon is of very limited nutrient value but, although the higher C:N values reflect the relative poor quality of the organic matter, macrofauna density and both TN and TOC concentrations were higher than in the Setú bal and Cascais canyons.…”
Section: Environmental Influences On Abundance and Biomassmentioning
confidence: 99%