Abstract (english) | The impact of atmospheric deposition on seas and oceans requires consideration of interfacial processes within the sea surface microlayer (SML), the uppermost layer at the air-sea interface. This study examines the impact of anthropogenic (AA) and biomass burning (BB) aerosol particles on plankton community structure and organic matter accumulation in the SML compared to the underlying water (ULW; 1 m depth) through microcosm amendment experiments in the coastal Adriatic Sea. Results confirm that realistic additions of AA and BB aerosols affect the SML and ULW differently, highlighting complex interactions between nutrient availability, toxicity, and plankton species competition. The sudden supply of nutrients, like nitrogen favoured larger phytoplankton, while elevated trace metals and organic pollutants could have a toxic effect, particularly on smaller species. The study highlights the vulnerability of the neuston community in the SML to pollutants, as the higher UV radiation likely enhanced the toxicity of specific atmospheric components compared to the ULW plankton community. Changes in neuston diversity due to atmospheric deposition strengthened the SML accumulation of dissolved and particulate organic carbon, including surfactants, which may reduce CO2 exchange between the ocean and the atmosphere. This study is one of the few to highlight the critical role of the SML in understanding the broader impacts of atmospheric deposition on marine systems, advancing our knowledge of environmental interfaces and their role in mediating increasing environmental pressures.
The dataset of the microcosm experiment is archived, and on the first sheet, there is an explanation of the abbreviations used in the document |
Methods (english) | Aerosol Analyses: Aerosol AA and BB materials were analysed for anions (Cl-, NO3-, NO2-, SO42-, PO43-) and cations (Na+, NH4+, K+, Ca2+, Mg2+) by ion chromatography with suppressed conductivity detection on dual channel capillary ion chromatograph (ICS-5000, Thermo Fisher Scientific, USA) as described in detail in Gluščić et al. (2023). Trace metals (V, Mn, Fe, Co, Ni, Cu, Zn, As, Sr, Cd, Pb, Al) were determined by inductively coupled plasma mass spectrometry (ICP-MS 7500cx, Agilent Technologies, Germany), after sample digestion in an UltraCLAVE digestion system (Milestone Srl, Italy) as described in detail in Penezić et al. (2021). Water soluble organic carbon (WSOC) was determined after filtration of PM water extracts (0.7 μm GF/F filters, Whatman, UK; pre-combusted at 450 °C for 5 h) by TOC-VCPH analyser (Shimadzu, Japan) by standardized thermo-optical methods. Filter extracts re-dissolved in acetonitrile were analysed for polycyclic aromatic hydrocarbons (PAH; list in Supporting Information, Table S1) using high-performance liquid chromatography with a fluorescence detector (1260 Infinity, Agilent Technologies, USA) as described in Jakovljević et al. (2021). Analysis of nitroaromatic compounds (NAC: list in Table S1) has been performed by UltiMate 3000 UHPLC system (Thermo Scientific, USA) coupled with a triple quadrupole/linear ion trap mass spectrometer (Agilent Technologies, USA), following the procedure described in Frka et al. (2022).
Seawater Analyses: Detailed procedures for the analyses of nutrients, organic carbon, surface-active substances, phytoplankton, and microbial community abundances are described in detail in Milinković et al. (2022) and are also available in the Appendix 2 of the Supporting Information. Briefly, to determine nutrient (dissolved NO3-, NO2-, NH4+ and PO43-), dissolved (DOC) and particulate organic carbon (POC) concentrations, seawater aliquots were filtrated through 0.7 μm GF/F filters (Whatman, UK) pre-combusted at 450 °C for 5 h. Nutrient concentrations were determined spectrophotometrically. Total dissolved inorganic nitrogen (DIN) concentrations were calculated as the sum of concentrations of all dissolved N species measured. DOC measurements were conducted using a TOC-VCPH analyser (Shimadzu, Japan) with standardized thermo-optical methods. Filters for POC were dried and analysed via elemental analyser (Flash EA 1112, Thermo Scientific, USA). Concentrations of surfactants or surface-active substances (SAS), expressed in equivalents of non-ionic surfactant tetra-octylphenolethoxylate (mg T eq. L-1), were determined by phase sensitive alternating current (ac.) voltammetry. The initial chemical characteristics of the SML and ULW are presented in the Appendix 3, Table S3. Composition and abundance of nanophytoplankton (NP; 2 – 20 µm) and microphytoplankton (MP, 20 – 200 µm) were assessed through microscopy, while heterotrophic bacteria (HB), also classified into high nucleic acid (HNA) and low nucleic acid (LNA) bacteria, Prochlorococcus (Pro), Synechococcus (Syn), picoeukaryotes (hereafter picophytoplankton, PP) and heterotrophic nanoflagellate communities (HNF) were determined through flow cytometry. Note that the abundance of MP and NP was determined at 0, 40, and 88 h, while the abundances of other communities were measured at 0, 18, 40, 64 and 88 h. The carbon contribution of the individual autotrophs and heterotrophs to the total POC was estimated based on literature data as described within Supporting Information (Appendix 1, 1.6.). The initial biological characteristics of the SML and ULW are presented in the Table S4. |