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Uncoupled seasonal variability of transparent exopolymer and Coomassie stainable particles in coastal Mediterranean waters

Bibliographic Data

ID21242032
AuthorsMarina Zamanillo (0000-0002-0753-4748, GEOMAR Helmholtz Centre for Ocean Research Kiel), Eva Ortega-Retuerta (CNRS, Sorbonne Université, UMR 7621, Laboratoire d’Océanographie Microbienne, Banyuls–sur–Mer, France), Eva Ortega‐Retuerta (0000-0003-0780-8347, Centre National de la Recherche Scientifique), Carolina Cisternas-Novoa (GEOMAR Helmholtz Centre for Ocean Research Kiel), Carolina Cisternas‐Novoa (GEOMAR Helmholtz Centre for Ocean Research Kiel), Cèlia Marrasé (0000-0002-5097-4829, Institut Català de Ciències del Clima), Carles Pelejero (0000-0002-7763-7769, Institució Catalana de Recerca i Estudis Avançats), Josep Pascual (0000-0002-7844-1741, Estació Meteorològica de L’Estartit, Girona, Catalonia, Spain), José Antonio Pascual (0000-0001-7485-1092, Agencia Estatal de Meteorología), Josep M Gasol (0000-0001-5238-2387, Edith Cowan University), Anja Engel (0000-0002-1042-1955, GEOMAR Helmholtz Centre for Ocean Research Kiel), Rafel Simó (0000-0003-3276-7663, Institut Català de Ciències del Clima)
Year2021
Volume9
Issue1
Publication date2021-12-03
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.2020.00165
OpenAlexW4205494402
LanguageEN
References cited89

Transparent exopolymer particles (TEP) and Coomassie stainable particles (CSP) are gel-like particles, ubiquitous in the ocean, that affect important biogeochemical processes including organic carbon cycling by planktonic food webs. Despite much research on both groups of particles (especially TEP) over many years, whether they exist as distinctly stainable fractions of the same particles or as independent particles, each with different driving factors, remains unclear. To address this question, we examined the temporal dynamics of TEP and CSP over 2 complete seasonal cycles at 2 coastal sites in the Northwestern Mediterranean Sea, the Blanes Bay Microbial Observatory (BBMO) and the L’Estartit Oceanographic Station (EOS), as well as their spatial distribution along a coast-to-offshore transect. Biological, chemical, and physical variables were measured in parallel. Surface concentrations (mean ± standard deviation [SD]) of TEP were 36.7 ± 21.5 μg Xanthan Gum (XG) eq L–1 at BBMO and 36.6 ± 28.3 μg XG eq L–1 at EOS; for CSP, they were 11.9 ± 6.1 μg BSA eq L–1 at BBMO and 13.0 ± 5.9 μg BSA eq L–1 at EOS. Seasonal variability was more evident at EOS, where surface TEP and CSP concentrations peaked in summer and spring, respectively, and less predictable at the shore-most station, BBMO. Vertical distributions between surface and 80 m, monitored at EOS, showed highest TEP concentrations within the surface mixed layer during the stratification period, whereas CSP concentrations were highest before the onset of summer stratification. Phytoplankton were the main drivers of TEP and CSP distributions, although nutrient limitation and saturating irradiance also appeared to play important roles. The dynamics and distribution of TEP and CSP were uncoupled both in the coastal sites and along the transect, suggesting that they are different types of particles produced and consumed differently in response to environmental variability

Bay · Biogeochemical cycle · Biology · Botany · Exopolymer · Mediterranean climate · Mediterranean sea · Phytoplankton · Picoplankton · Plankton · Seasonality · Surface water · Water column · Chemistry · Coastal and Marine Management · Environmental Science · Marine and coastal ecosystems · Microbial Community Ecology and Physiology · Ecology · Environmental Chemistry · Geology · Oceanography

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