EGU22-9239
https://doi.org/10.5194/egusphere-egu22-9239
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Spatial variability of organic matter in marine sediments from the Gulf of Cadiz

Teodoro Ramírez-Cárdenas1, Esperanza Liger2, and Luís Miguel Fernández-Salas3
Teodoro Ramírez-Cárdenas et al.
  • 1Instituto Español de Oceanografía (IEO, CSIC), C.O. de Málaga, Fuengirola (Málaga), Spain (teodoro.ramirez@ieo.es)
  • 2Universidad de Málaga, Departamento de Física Aplicada II, Málaga, Spain
  • 3Instituto Español de Oceanografía (IEO, CSIC), C.O. de Cádiz, Cádiz, Spain

This work analyses the spatial variability of organic matter (phytopigments, proteins and carbohydrates) in surface sediments from the Gulf of Cadiz (SW Iberian Peninsula). Sediment samples were taken in summer 2019 during the oceanographic cruise “INPULSE-19” at different stations with depths ranging from nearly 500 m to 1000 m depth. The distribution of the different organic matter fractions showed a high variability with marked differences between stations. The spatial distribution of phytopigments (PHYTOPIG) in the upper sediment layer (0-1 cm below the seafloor) evidenced high degree of accumulation at two close stations, where the higher PHYTOPIG concentrations were found, while PHYTOPIG concentrations were one other of magnitude lower at other sampling stations. Protein and carbohydrate concentrations in the water-soluble fractions (PROTWS and CHOWS) from the upper 0-1 cm sediment layer were correlated with each other, although they exhibited some differences in their spatial distribution pattern. Moreover, PROTWS in the 0-1 cm sediment layer was highly correlated to PHYTOPIG, suggesting a similar origin for both fractions, while the correlation with CHOWS was weaker. Alkaline extractable proteins and carbohydrates (PROTALK andCHOALK) were one order of magnitude higher than the concentrations in their respective water-soluble fractions. PROTALK andCHOALK in the 0-1 cm sediment layer were highly correlated with each other, showing a quite similar distribution pattern. The PROTWS/CHOWS ratio, an index of organic matter lability, ranged between 0.3 and 2.1 in the upper sediment layer, while the PROTALK/CHOALK ratio ranged between 1.6 and 3.6 The observed variability in these ratios indicates differences in the lability of sedimentary organic matter at different stations, which might affect the bioavailability of organic matter in the sediments.

How to cite: Ramírez-Cárdenas, T., Liger, E., and Fernández-Salas, L. M.: Spatial variability of organic matter in marine sediments from the Gulf of Cadiz, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9239, https://doi.org/10.5194/egusphere-egu22-9239, 2022.