Articles | Volume 23, issue 16
https://doi.org/10.5194/bg-23-5961-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/bg-23-5961-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Buoyancy and polarity driven accumulation of dissolved organic matter in the sea surface microlayer during a phytoplankton bloom
Jasper Zöbelein
CORRESPONDING AUTHOR
Institute for Chemistry and Biology of the Marine Environment (ICBM), School of Mathematics and Science, Carl von Ossietzky Universität Oldenburg, Oldenburg, Germany
Shubham Sawle
Institute of Physical Chemistry, Christian-Albrechts-University Kiel, Kiel, Germany
Gernot Friedrichs
Institute of Physical Chemistry, Christian-Albrechts-University Kiel, Kiel, Germany
KMS Kiel Marine Science-Centre for Interdisciplinary Marine Science, Kiel University, Kiel, Germany
Mariana Ribas-Ribas
Institute for Chemistry and Biology of the Marine Environment (ICBM), School of Mathematics and Science, Carl von Ossietzky Universität Oldenburg, Oldenburg, Germany
Carola Lehners
Institute for Chemistry and Biology of the Marine Environment (ICBM), School of Mathematics and Science, Carl von Ossietzky Universität Oldenburg, Oldenburg, Germany
Katharina Paetz
Institute for Chemistry and Biology of the Marine Environment (ICBM), School of Mathematics and Science, Carl von Ossietzky Universität Oldenburg, Oldenburg, Germany
Maximilian Pflaum
Institute of Physical Chemistry, Christian-Albrechts-University Kiel, Kiel, Germany
Hannelore Waska
Institute for Chemistry and Biology of the Marine Environment (ICBM), School of Mathematics and Science, Carl von Ossietzky Universität Oldenburg, Oldenburg, Germany
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Short summary
The ocean is glazed with a one-millimetre biofilm that controls the flow of gases and energy from the atmosphere. To investigate how this film forms, we cultivated microscopic algae in a tank under controlled, windless conditions. Our results show that carbohydrates released by these algae rise to the surface, forming "carbo-slicks" that create a gel-like layer. This demonstrates that biological production is a key driver of the sea surface, which is crucial for understanding carbon exchange.
The ocean is glazed with a one-millimetre biofilm that controls the flow of gases and energy...
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