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Approaches to evaluate spatial and temporal variability of deep marine sediment characteristics under the impact of dense water formation events

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Academic year: 2021

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Fig. 2: Sampling area at coring site CCC1900 situated at the  convergence of Lacaze-Duthiers Canyon and Cap de Creus  Canyon (see Fig
Fig. 3: Temporal pattern of sediment composition at site CCC1900 (see Figure 1 for the station location)
Table 2. Temporal variability (TEMP): Core locations, pelitic fraction (%), POC (%), δ13C POC (‰), TN (%), δ15N (‰), Al (%), Cu (µg/g), Hg (ng/g), and Pb (µg/g) content of surface sediment from  October 2005 to November 2010 at coring station CCC1900
Table 3. Large-scale spatial variability (TRANSECT): Core locations, pelitic fraction (%), POC (%), δ13C POC (‰), TN (%), δ15N (‰), Al (%), Cu (µg/g), Cu/Al, Hg (ng/g), Hg/Al and Pb (µg/g),  Pb/Al measurements of surface sediment from the bathymetric South
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