Effects of turbulence on TEP dynamics under contrasting nutrient conditions: implications for aggregation and sedimentation processes

• Published in: Marine ecology. Progress series (Halstenbek) 2006-10, Vol.323, p.47-57
• Main Authors: Beauvais, S., Pedrotti, M. L., Egge, J., Iversen, K., Marrasé, C.
• Format: Article
• Language: English
• Subjects: Aggregation; Animal and plant ecology; Animal, plant and microbial ecology; Bacillariophyceae; Bacteria; Biological and medical sciences; Carbon; Cell aggregates; Diatoms; Earth Sciences; Fundamental and applied biological sciences. Psychology; Marine; Nutrients; Oceanography; Phytoplankton; Plankton; Sciences of the Universe; Sea water; Sea water ecosystems; Synecology; Turbulence
• ISSN: 0171-8630; 1616-1599
• DOI: 10.3354/meps323047

The effect of different small-scale turbulence intensities on transparent exopolymeric particle (TEP) dynamics was studied in natural North Sea coastal waters. The abundance, volume, size spectra and carbon content of TEP were examined in mesocosms with and without added nutrients: no addition (T series) and a Redfield ratio supply on Day 1 (NT series), fertilized with 16 μM N:1 μM P:32 μM Si to favor phytoplankton production in the form of a bloom. Turbulence was generated by vertically oscillating grids, operating continuously for 14 d. We determined whether TEP production, under contrasting nutrient conditions, changes with level of turbulence. TEP concentration increased with turbulence. The effect of turbulence was likely indirect, by inducing an increase in growth rates of diatoms that actively exude TEP precursor, particularly when nutrients were exhausted. Following TEP production, the ratio of particulate organic carbon to nitrogen increased after the bloom, regardless of turbulence level. TEP formation led to a decoupling of carbon and nitrogen dynamics, with a large flow of carbon channeled into the TEP pool, representing up to 44% of the primary production, and was constant with the turbulence intensity. While turbulence had no effect on small particles (40 μm. We found significant sedimentation of TEP when turbulence was lower (5 to 8 × 10–2cm² s–3) and a persistence of the TEP pool in the tanks without sinking at higher levels of turbulence intensity, typical of storm events (ε = 1 cm² s–3).