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Submarine karstic springs as a source of nutrients and bioactive trace metals for the oligotrophic Northwest Mediterranean Sea.
Tamborski, Joseph; van Beek, Pieter; Conan, Pascal; Pujo-Pay, Mireille; Odobel, Charlene; Ghiglione, Jean-François; Seidel, Jean-Luc; Arfib, Bruno; Diego-Feliu, Marc; Garcia-Orellana, Jordi; Szafran, Armand; Souhaut, Marc.
Affiliation
  • Tamborski J; LEGOS, Laboratoire d'Etudes en Géophysique et Océanographie Spatiales, Université de Toulouse, CNES, CNRS, IRD, UPS, Observatoire Midi Pyrénées, 14 Ave Edouard Belin, 31400 Toulouse, France. Electronic address: jtamborski@whoi.edu.
  • van Beek P; LEGOS, Laboratoire d'Etudes en Géophysique et Océanographie Spatiales, Université de Toulouse, CNES, CNRS, IRD, UPS, Observatoire Midi Pyrénées, 14 Ave Edouard Belin, 31400 Toulouse, France.
  • Conan P; LOMIC, Laboratoire d'Océanographie Microbienne, Observatoire Océanologique, Sorbonne Université, CNRS, UPMC Univ Paris 06, UMR7621, 66650 Banyuls/Mer, France.
  • Pujo-Pay M; LOMIC, Laboratoire d'Océanographie Microbienne, Observatoire Océanologique, Sorbonne Université, CNRS, UPMC Univ Paris 06, UMR7621, 66650 Banyuls/Mer, France.
  • Odobel C; LOMIC, Laboratoire d'Océanographie Microbienne, Observatoire Océanologique, Sorbonne Université, CNRS, UPMC Univ Paris 06, UMR7621, 66650 Banyuls/Mer, France.
  • Ghiglione JF; LOMIC, Laboratoire d'Océanographie Microbienne, Observatoire Océanologique, Sorbonne Université, CNRS, UPMC Univ Paris 06, UMR7621, 66650 Banyuls/Mer, France.
  • Seidel JL; HydroSciences Montpellier, UMR 5569 - UM2 - CNRS - IRD - UM1 Place Eugène Bataillon -CC MSE, 34095 Montpellier Cedex 5, France.
  • Arfib B; Aix Marseille Université, CNRS, IRD, INRAE, Coll France, CEREGE, Aix-en-Provence, France.
  • Diego-Feliu M; Institut de Ciència i Tecnologia Ambientals (ICTA-UAB), Universitat Autònoma de Barcelona, Bellaterra, Catalunya, Spain.
  • Garcia-Orellana J; Institut de Ciència i Tecnologia Ambientals (ICTA-UAB), Universitat Autònoma de Barcelona, Bellaterra, Catalunya, Spain; Department de Física, Universitat Autònoma de Barcelona, Bellaterra, Catalunya, Spain.
  • Szafran A; LEGOS, Laboratoire d'Etudes en Géophysique et Océanographie Spatiales, Université de Toulouse, CNES, CNRS, IRD, UPS, Observatoire Midi Pyrénées, 14 Ave Edouard Belin, 31400 Toulouse, France.
  • Souhaut M; LEGOS, Laboratoire d'Etudes en Géophysique et Océanographie Spatiales, Université de Toulouse, CNES, CNRS, IRD, UPS, Observatoire Midi Pyrénées, 14 Ave Edouard Belin, 31400 Toulouse, France.
Sci Total Environ ; 732: 139106, 2020 Aug 25.
Article de En | MEDLINE | ID: mdl-32422479
ABSTRACT
Groundwater springs in karstified carbonate aquifers are known to transport carbon, nutrients and trace elements to the coastal ocean. The biogeochemical significance of submarine karstic springs and their impact on coastal primary production are often difficult to quantify. We investigated several karstic springs, including the first-order Port-Miou spring, in an urbanized watershed that is also severely impacted by sewage effluent (Calanques of Marseille-Cassis, France). Karstic springs were elevated in major nutrients and bioactive trace metals over Mediterranean seawater, with relatively low concentration ranges. Groundwater NO3- was likely derived from atmosphere-aquifer interactions, while DOCDON ratios reveal that NO2- and NH4+ was autochthonously produced during mixing between karst groundwater and seawater. Submarine groundwater discharge (SGD) during March 2018 (wet season, baseflow conditions) was 6.7 ± 2.0 m3 s-1 for the entire investigated coastline, determined from simultaneous 224Ra and 226Ra mass balances. The contribution of groundwater PO43-, the major limiting nutrient of the Mediterranean Sea, sustained only 1% of primary production adjacent to sewage outfall, but between 7 and 100% of the local primary production in areas that were not impacted by sewage. Groundwater and seawater FeDIN and FeDIP ratios suggest that Fe was not a limiting micro-nutrient during the period of study, where bioactive trace metal fluxes were dominated by sewage and atmospheric deposition, although excess Fe from groundwater may locally enhance N fixation. Groundwater solute fluxes may easily vary by a factor of two or more over time because karst aquifers are sensitive to precipitation, as is the case of the regional carbonate karstified aquifer of Port-Miou, highlighting the critical importance of properly characterizing nutrient and trace metal inputs in these coastal environments.
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Texte intégral: 1 Collection: 01-internacional Base de données: MEDLINE Langue: En Journal: Sci Total Environ Année: 2020 Type de document: Article

Texte intégral: 1 Collection: 01-internacional Base de données: MEDLINE Langue: En Journal: Sci Total Environ Année: 2020 Type de document: Article
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