Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea)
Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea)...
Ausführliche Beschreibung
Autor*in: |
Faganeli, Jadran [verfasserIn] |
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E-Artikel |
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Englisch |
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2023 |
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Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Übergeordnetes Werk: |
Enthalten in: Journal of soils and sediments - Berlin : Springer, 2001, 23(2023), 12 vom: 21. Apr., Seite 4085-4097 |
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Übergeordnetes Werk: |
volume:23 ; year:2023 ; number:12 ; day:21 ; month:04 ; pages:4085-4097 |
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DOI / URN: |
10.1007/s11368-023-03519-6 |
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Katalog-ID: |
SPR053892542 |
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520 | |a Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. | ||
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700 | 1 | |a Kovač, Nives |4 aut | |
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10.1007/s11368-023-03519-6 doi (DE-627)SPR053892542 (SPR)s11368-023-03519-6-e DE-627 ger DE-627 rakwb eng Faganeli, Jadran verfasserin (orcid)0000-0002-2083-1042 aut Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. Metals (dpeaa)DE-He213 Metalloids (dpeaa)DE-He213 Suspended particulate matter (dpeaa)DE-He213 Plankton (dpeaa)DE-He213 Bioconcentration factor (dpeaa)DE-He213 Northern Adriatic Sea (dpeaa)DE-He213 Falnoga, Ingrid aut Klun, Katja aut Mazej, Darja aut Mozetič, Patricija aut Zuliani, Tea aut Kovač, Nives aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 12 vom: 21. Apr., Seite 4085-4097 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:12 day:21 month:04 pages:4085-4097 https://dx.doi.org/10.1007/s11368-023-03519-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 12 21 04 4085-4097 |
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10.1007/s11368-023-03519-6 doi (DE-627)SPR053892542 (SPR)s11368-023-03519-6-e DE-627 ger DE-627 rakwb eng Faganeli, Jadran verfasserin (orcid)0000-0002-2083-1042 aut Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. Metals (dpeaa)DE-He213 Metalloids (dpeaa)DE-He213 Suspended particulate matter (dpeaa)DE-He213 Plankton (dpeaa)DE-He213 Bioconcentration factor (dpeaa)DE-He213 Northern Adriatic Sea (dpeaa)DE-He213 Falnoga, Ingrid aut Klun, Katja aut Mazej, Darja aut Mozetič, Patricija aut Zuliani, Tea aut Kovač, Nives aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 12 vom: 21. Apr., Seite 4085-4097 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:12 day:21 month:04 pages:4085-4097 https://dx.doi.org/10.1007/s11368-023-03519-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 12 21 04 4085-4097 |
allfields_unstemmed |
10.1007/s11368-023-03519-6 doi (DE-627)SPR053892542 (SPR)s11368-023-03519-6-e DE-627 ger DE-627 rakwb eng Faganeli, Jadran verfasserin (orcid)0000-0002-2083-1042 aut Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. Metals (dpeaa)DE-He213 Metalloids (dpeaa)DE-He213 Suspended particulate matter (dpeaa)DE-He213 Plankton (dpeaa)DE-He213 Bioconcentration factor (dpeaa)DE-He213 Northern Adriatic Sea (dpeaa)DE-He213 Falnoga, Ingrid aut Klun, Katja aut Mazej, Darja aut Mozetič, Patricija aut Zuliani, Tea aut Kovač, Nives aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 12 vom: 21. Apr., Seite 4085-4097 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:12 day:21 month:04 pages:4085-4097 https://dx.doi.org/10.1007/s11368-023-03519-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 12 21 04 4085-4097 |
allfieldsGer |
10.1007/s11368-023-03519-6 doi (DE-627)SPR053892542 (SPR)s11368-023-03519-6-e DE-627 ger DE-627 rakwb eng Faganeli, Jadran verfasserin (orcid)0000-0002-2083-1042 aut Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. Metals (dpeaa)DE-He213 Metalloids (dpeaa)DE-He213 Suspended particulate matter (dpeaa)DE-He213 Plankton (dpeaa)DE-He213 Bioconcentration factor (dpeaa)DE-He213 Northern Adriatic Sea (dpeaa)DE-He213 Falnoga, Ingrid aut Klun, Katja aut Mazej, Darja aut Mozetič, Patricija aut Zuliani, Tea aut Kovač, Nives aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 12 vom: 21. Apr., Seite 4085-4097 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:12 day:21 month:04 pages:4085-4097 https://dx.doi.org/10.1007/s11368-023-03519-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 12 21 04 4085-4097 |
allfieldsSound |
10.1007/s11368-023-03519-6 doi (DE-627)SPR053892542 (SPR)s11368-023-03519-6-e DE-627 ger DE-627 rakwb eng Faganeli, Jadran verfasserin (orcid)0000-0002-2083-1042 aut Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. Metals (dpeaa)DE-He213 Metalloids (dpeaa)DE-He213 Suspended particulate matter (dpeaa)DE-He213 Plankton (dpeaa)DE-He213 Bioconcentration factor (dpeaa)DE-He213 Northern Adriatic Sea (dpeaa)DE-He213 Falnoga, Ingrid aut Klun, Katja aut Mazej, Darja aut Mozetič, Patricija aut Zuliani, Tea aut Kovač, Nives aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 12 vom: 21. Apr., Seite 4085-4097 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:12 day:21 month:04 pages:4085-4097 https://dx.doi.org/10.1007/s11368-023-03519-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 12 21 04 4085-4097 |
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Enthalten in Journal of soils and sediments 23(2023), 12 vom: 21. Apr., Seite 4085-4097 volume:23 year:2023 number:12 day:21 month:04 pages:4085-4097 |
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Journal of soils and sediments |
authorswithroles_txt_mv |
Faganeli, Jadran @@aut@@ Falnoga, Ingrid @@aut@@ Klun, Katja @@aut@@ Mazej, Darja @@aut@@ Mozetič, Patricija @@aut@@ Zuliani, Tea @@aut@@ Kovač, Nives @@aut@@ |
publishDateDaySort_date |
2023-04-21T00:00:00Z |
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373325134 |
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SPR053892542 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">SPR053892542</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20231129064638.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">231129s2023 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11368-023-03519-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR053892542</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s11368-023-03519-6-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Faganeli, Jadran</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-2083-1042</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea)</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2023</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. 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author |
Faganeli, Jadran |
spellingShingle |
Faganeli, Jadran misc Metals misc Metalloids misc Suspended particulate matter misc Plankton misc Bioconcentration factor misc Northern Adriatic Sea Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) |
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Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) Metals (dpeaa)DE-He213 Metalloids (dpeaa)DE-He213 Suspended particulate matter (dpeaa)DE-He213 Plankton (dpeaa)DE-He213 Bioconcentration factor (dpeaa)DE-He213 Northern Adriatic Sea (dpeaa)DE-He213 |
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misc Metals misc Metalloids misc Suspended particulate matter misc Plankton misc Bioconcentration factor misc Northern Adriatic Sea |
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misc Metals misc Metalloids misc Suspended particulate matter misc Plankton misc Bioconcentration factor misc Northern Adriatic Sea |
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Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) |
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Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) |
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Faganeli, Jadran |
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Journal of soils and sediments |
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Journal of soils and sediments |
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Faganeli, Jadran Falnoga, Ingrid Klun, Katja Mazej, Darja Mozetič, Patricija Zuliani, Tea Kovač, Nives |
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Faganeli, Jadran |
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10.1007/s11368-023-03519-6 |
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(ORCID)0000-0002-2083-1042 |
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(orcid)0000-0002-2083-1042 |
title_sort |
metal(loid)s in suspended particulate matter and plankton from coastal waters (gulf of trieste, northern adriatic sea) |
title_auth |
Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) |
abstract |
Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
abstractGer |
Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
abstract_unstemmed |
Purpose The levels of metal(loid)s at the beginning of the coastal pelagic food web, providing an insight into accumulation in the suspended particulate matter (SPM) and size-fractionated plankton, were studied in the shallow coastal marine environment of the Gulf of Trieste (northern Adriatic Sea) affected by the metal polluted Isonzo/Soča River as a result of historical Hg, and Pb and Zn mining activities in the hinterland. Materials and methods Levels of metal(loid)s were investigated in suspended particulate matter (0.45–20 µm) and fractionated plankton (20–50 µm, 50–200 µm, > 200 µm) collected monthly at the Marine Biology Station oceanographic buoy Vida in the southern part of the Gulf of Trieste. Results and discussion Concentrations of meta(loid)s showed the following order Al,Fe > Zn,Mn > Ni > Cu,Cr > As,Pb,V > Co > Se > Cd > U > Hg and were similar to those of dissolved metal(loid)s of the gulf waters (Al,Fe > Zn > Cu > V > Mn > As > Ni,Se > U,Cr > Cd > Hg) where Hg, Cu, Cr and Se were significantly associated with colloidal organic matter (< 0.2 µm, > 5 kDa). The partition of metal(loid)s between their particulate phase and free ion and inorganic complexes in the water ($ K_{pd} $) confirmed a strong binding of Hg, Al, Mn, Fe, Cr and Pb onto seawater particles. In general, the metal(loid) data for SPM and plankton showed high levels in the 50–200 µm microplankton fraction. Larger plankton fractions, especially > 200 µm, contain a lower amount of metal(loid)s associated with mineral particles originating from sedimentary pelite resuspension and riverine inflows. Variations of metal(loid)s levels in SPM and plankton fractions were related to their biomass (ash free dry weight—AFDW) and organic matter, and mineral (inorganic) content, which is difficult to separate from biogenic particles including organisms, and to the taxonomic composition and feeding behaviour of organisms in various fractions. Conclusions The Redfield's stoichiometric concept including metal(loid)s in the coastal marine plankton (SPM and mesozooplankton) appears unreliable. The bioconcentration factors (log BCFs) of the studied metal(loid)s, ranging between 4 and 6 for Hg, Fe, Mn, Cr, Pb, Co, Zn, Ni, As, Cu and V and lower for Se and U both in micro- and mesoplankton, can possibly be used in micro- and especially in mesoplankton fraction less impacted by mineral metal(loid)s. This should be considered when establishing the metal(loid)s levels at the base of the coastal and estuarine food webs, at the onset of marine bioaccumulation, to provide information for marine organisms consumed by humans. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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title_short |
Metal(loid)s in suspended particulate matter and plankton from coastal waters (Gulf of Trieste, northern Adriatic Sea) |
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|
score |
7.398699 |