Seasonality, rather than estuarine gradient or particle suspension/sinking dynamics, determines estuarine carbon distributions.

Sci Total Environ

Dept. Plankton and Microbial Ecology, Leibniz Institute for Freshwater Ecology and Inland Fisheries (IGB), Zur Alten Fischerhuette 2, D-16775 Stechlin, Germany; Inst. of Biology and Biochemistry, Potsdam University, Maulbeerallee 2, 14469 Potsdam, Germany. Electronic address:

Published: May 2024

AI Article Synopsis

  • Estuaries play a critical role in the global carbon cycle by exchanging carbon across aquatic, atmospheric, and terrestrial environments, making them key areas for blue carbon storage and greenhouse gas emissions.
  • The study investigated how estuarine gradients impact the interactions of sinking/suspended particles and dissolved organic matter, finding that salinity had minimal influence on microbial degradation and carbon composition, with more significant biological activity in brackish areas.
  • Results showed that organic particles in the Elbe estuary displayed both marine and terrestrial characteristics, with findings providing valuable insights for understanding carbon contributions and implications for greenhouse gas emissions, informing future environmental policies.

Article Abstract

Estuaries are important components of the global carbon cycle; exchanging carbon between aquatic, atmospheric, and terrestrial environments, representing important loci for blue carbon storage and greenhouse gas emissions. However, how estuarine gradients affect sinking/suspended particles, and dissolved organic matter dynamic interactions remains unexplored. We fractionated suspended/sinking particles to assess and characterise carbon fate differences. We investigated bacterial colonisation (SYBR Green I) and exopolymer concentrations (TEP/CSP) with microscopy staining techniques. C/H/N and dry weight analysis identified particle composition differences. Meanwhile, nutrient and carbon analysis, and excitation and emission matrix evaluations with a subsequent parallel factor (PARAFAC) analysis characterised dissolved organic matter. The lack of clear salinity driven patterns in our study are presumably due to strong mixing forces and high particle heterogeneity along the estuary, with only density differences between suspended and sinking particles. Elbe estuary particles' organic portion is made up of marine-like (sinking) and terrestrial-like (suspended) signatures. Salinity did not have a significant role in microbial degradation and carbon composition, although brackish estuary portions were more biologically active. Indicative of increased degradation rates, leading to decreased greenhouse gas emissions, which are especially relevant for estuaries, with their disproportionate greenhouse gas emissions. Bacterial colonisation decreased seawards, indicative of decreased degradation, and shifts in microbial community composition and functions. Our findings span diverse strands of research, concerning steady carbon contributions from both marine and terrestrial sources, carbon aromaticity, humification index, and bioavailability. Their integration highlights the importance of the Elbe estuary as a model system, providing robust information for future policy decisions affecting dissolved and particulate matter dynamics within the Elbe Estuary.

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http://dx.doi.org/10.1016/j.scitotenv.2024.171962DOI Listing

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