Published July 2018 | Version v1
Journal article

Sources and coastal distribution of dissolved organic matter in the Gulf of Cadiz

  • 1. CEI-MAR International Campus of Excellence of the Sea (Spain)
  • 2. Instituto de Ciencias Marinas de Andalucía (CSIC), Campus Universitario Río San Pedro, 11519 Puerto Real, Cádiz (Spain)
  • 3. Ecología Funcional de Sistemas Acuáticos, Centro Universitario Regional Este, Universidad de la República, Rocha (Uruguay)
  • 4. Departamento de Química-Física, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz, Campus Río San Pedro s/n, Puerto Real, Cádiz 11510 (Spain)
  • 5. Instituto Español de Oceanografía, Centro Oceanográfico de Cádiz, Puerto Pesquero, Muelle de Levante s/n, 11006 Cádiz (Spain)
  • 6. IFAPA Centro El Toruño, Camino Tiro de Pichón s/n, 11500 El Puerto de Santa María (Spain)

Description

Highlights: • Terrestrially derived OM from wetland discharge as major source of DOM in the GoC • DOC transport from the Guadiana-Guadalquivir estuaries to the Mediterranean Sea • Humic-like FDOM production as a by-product of DOM metabolism by plankton organisms • FDOM as a proxy for tracing physical circulation in the Gulf of Cadiz Dissolved organic matter (DOM) is a major component of the organic matter pool, playing a key role in the global ocean functioning. However, studies on DOM in waters of many ocean regions, such as the Gulf of Cadiz (GoC), are poorly known. Advanced aquatic sensors enable autonomous for long-term deployments in situ collection of high frequency DOM data using fluorescent dissolved organic matter (FDOM) as a proxy. The present study evaluates the relevance of FDOM, the estuarine influence and the environmental factors that determine its spatial distribution in the GoC. Our results suggest that the GoC water mass, under the estuarine influence of three main rivers, is receiving large amounts of DOM transported mainly by Guadalquivir and Guadiana rivers and much less from Tinto-Odiel. Salinity is the main factor explaining the FDOM variability within the Guadalquivir and Guadiana rivers and in the inner shelf of the GoC. In the outer shelf of the GoC, plankton-produced DOM could explain the persistent spatial pattern of FDOM, playing an important role in the dynamics of FDOM from the North area of the GoC through the persistent low-salinity Eastern North Atlantic Central Water. The oceanographic dynamics and the spatial pattern of FDOM concentration in the continental shelf of the GoC suggest a net transport of FDOM through the GCC (Gulf of Cadiz Current) to the Mediterranean Sea.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.scitotenv.2018.02.293

Additional details

Identifiers

DOI
10.1016/j.scitotenv.2018.02.293;
PII
S0048969718306934;

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
630
Journal Page Range
p. 1583-1595
ISSN
0048-9697
CODEN
STENDL

Optional Information

Copyright
Copyright (c) 2018 Elsevier B.V. All rights reserved.