Articles | Volume 18, issue 5
https://doi.org/10.5194/bg-18-1749-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-18-1749-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Deep maxima of phytoplankton biomass, primary production and bacterial production in the Mediterranean Sea
Department of Ecology and Animal Biology, Universidade de Vigo, 36310 Vigo, Spain
France Van Wambeke
Mediterranean Institute of Oceanography, Aix-Marseille Université, CNRS, Université de Toulon, CNRS, IRD, MIO UM 110, 13288 Marseille, France
Julia Uitz
Laboratoire d'Océanographie de Villefranche, Sorbonne Université, CNRS, 06230 Villefranche-sur-Mer, France
Emmanuel S. Boss
School of Marine Sciences, University of Maine, Orono, Maine, USA
Céline Dimier
Laboratoire d'Océanographie de Villefranche, Sorbonne Université, CNRS, 06230 Villefranche-sur-Mer, France
Julie Dinasquet
Scripps Institution of Oceanography, University of California, San Diego, San Diego, California, USA
Anja Engel
GEOMAR, Helmholtz Centre for Ocean Research Kiel, 24105 Kiel, Germany
Nils Haëntjens
School of Marine Sciences, University of Maine, Orono, Maine, USA
María Pérez-Lorenzo
Department of Ecology and Animal Biology, Universidade de Vigo, 36310 Vigo, Spain
Vincent Taillandier
Laboratoire d'Océanographie de Villefranche, Sorbonne Université, CNRS, 06230 Villefranche-sur-Mer, France
Birthe Zäncker
GEOMAR, Helmholtz Centre for Ocean Research Kiel, 24105 Kiel, Germany
The Marine Biological Association of the United Kingdom, Plymouth, PL1 2PB, United Kingdom
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Latest update: 23 Nov 2024
Short summary
The concentration of chlorophyll is commonly used as an indicator of the abundance of photosynthetic plankton (phytoplankton) in lakes and oceans. Our study investigates why a deep chlorophyll maximum, located near the bottom of the upper, illuminated layer develops in the Mediterranean Sea. We find that the acclimation of cells to low light is the main mechanism involved and that this deep maximum represents also a maximum in the biomass and carbon fixation activity of phytoplankton.
The concentration of chlorophyll is commonly used as an indicator of the abundance of...
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