Articles | Volume 14, issue 9
https://doi.org/10.5194/bg-14-2245-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-14-2245-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Low planktic foraminiferal diversity and abundance observed in a spring 2013 west–east Mediterranean Sea plankton tow transect
Miguel Mallo
CORRESPONDING AUTHOR
Institute of Environmental Science and Technology (ICTA), Autonomous
University of Barcelona (UAB), Bellaterra 08193, Spain
Patrizia Ziveri
CORRESPONDING AUTHOR
Institute of Environmental Science and Technology (ICTA), Autonomous
University of Barcelona (UAB), Bellaterra 08193, Spain
Catalan Institution for Research and Advanced Studies (ICREA), Pg.
Lluís Companys 23, Barcelona 08010, Spain
P. Graham Mortyn
Institute of Environmental Science and Technology (ICTA), Autonomous
University of Barcelona (UAB), Bellaterra 08193, Spain
Geography Department, UAB, Bellaterra 08193, Spain
Ralf Schiebel
Climate Geochemistry, Max Planck Institute for Chemistry,
Hahn-Meitner-Weg 1, 55128 Mainz, Germany
Michael Grelaud
Institute of Environmental Science and Technology (ICTA), Autonomous
University of Barcelona (UAB), Bellaterra 08193, Spain
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Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
Single-celled living calcareous planktic foraminifera data across the Mediterranean Sea suggest that stratification of the surface water column, food availability, temperature, and seawater carbonate chemistry are the main factors controlling their distribution and mass. Increasing temperature, salinity, surface ocean stratification, and trophic conditions could be the causes of reduced abundance, diversity and species-specific changes in calcification in planktic foraminifera.
Single-celled living calcareous planktic foraminifera data across the Mediterranean Sea suggest...
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