Elsevier

Continental Shelf Research

Volume 211, 30 December 2020, 104280
Continental Shelf Research

Trace metal concentrations in soil-plant complex in rocky shore salt marshes of Central Patagonia

https://doi.org/10.1016/j.csr.2020.104280Get rights and content

Highlights

  • Metals on marshes of the Nuevo Gulf tend to accumulate on the southern coastal edge.

  • Cd, Pb, Cr and Ni showed anthropic enrichment and the other metals a natural origin.

  • Fe and Al were higher in soil than in plant, and Pb, Cu and Zn were all similar.

  • Cr and Ni were abundant as pseudototal and showed a high bioaccumulation in roots.

  • Cd was scarce in the soil and was mostly concentrated in Spartina’ roots.

Abstract

Population growth and industrialization involve environmental problems, such as metal pollution, and coastal environments are particularly susceptible to such issues. Within this framework, we aimed: (i) to determine the levels of trace metals in soils and Spartina densiflora tissues in rocky shore marshes of Central Patagonia; (ii) to relate metal concentration patterns in the different soil-plant complex fractions to environmental conditions; and (iii) to investigate whether geographical metal concentration patterns can be explained with anthropogenic influences and sources and/or by local prevailing biogeochemical processes. For this purpose, soil samples and associated vegetation were collected in five rocky shore marshes located at different distances from an urban or industrial area. The concentration of Al, Cd, Cr, Cu, Fe, Ni, Pb, and Zn in soils (pseudototal and bioavailable) and in plants (roots and shoots) was determined. Then the enrichment factor, bioaccumulation and translocation factor were calculated. The soil mineralogy and the behavior of these metals according to different soil variables were discussed. The results showed different behavior and level of anthropic impact according to the metal considered. Salt marshes located on the southern edge of the Nuevo Gulf showed the highest concentrations of metals. Fe, Al, Cu and Zn showed mostly a natural origin. Fe and Al were mainly in soils rather than in plants, while Cu and Zn were similarly distributed in both matrixes. Although Cd in soils showed enrichment, it would have a natural origin. Also, it was scarce in the soil and was mostly concentrated in Spartina’ roots. Pb, Cr and Ni showed anthropic enrichment too, being mainly derived from the port and industrial activities. Pb had significant representation in all soil-plant subsystems and showed the highest bioavailability in soils. Cr and Ni, were found in high concentration in the soil and showed a high bioaccumulation in roots. The human impact level in rocky shore marshes of the Nuevo Gulf in Central Patagonia associated to the trace metals pollution varies from being scarce to significantly important, with the marshes located in its southern margin showing the worst scenarios.

Introduction

Salt marshes are considered one of the most valuable environments due to several ecosystem services that are provided, such as food, shelter, refuge, a place of reproduction for several animal species, coastal protection, water purification through the filtering of nutrients and other pollutants, carbon sequestration, as well as a variety of touristic, recreational and educative uses (Barbier et al., 2011). Such circumstances have led to a notable worldwide increase in research activity for these ecosystems, not excluding the Argentinian’ salt marshes (Alberti et al., 2007; Botté et al., 2008; Daleo et al., 2011; Negrin et al., 2016; among others) and in particular, Patagonian’ salt marshes which were oblivious to this trend during the last few decades. Most of these Patagonian studies were focused on ecological patterns and processes (e.g., Alberti et al., 2007; Daleo and Iribarne 2009; Idaszkin et al., 2011; Sueiro et al., 2011, 2012; Firstater et al., 2016), while others were interested in deleterious effects pursuing environment-related issues, for example, biological invasions (Schwindt et al. 2009, 2020; Mendez et al., 2012; Sueiro et al., 2013) or pollution (Marinho et al., 2013, 2017; Idaszkin et al., 2014, 2015, 2017a,b,c; Pollicelli et al., 2018).

Trace metals are natural components of ecosystems that can be augmented through anthropogenic activities, and inclusively reaching toxic levels for the organism that inhabit there (Kabata-Pendias and Pendias 2000). As intertidal environments, salt marshes, are susceptible to trace metal pollution, being that pollutants wasted in the sea could spread into the intertidal zone during each high tide period (Hung and Chmura 2007). In this way, these environments can capture trace metals of the sea, and depending on the metal and the physico-chemical features of the environment (pH, organic matter content, clay fraction content, mineralogical composition, salinity, redox potential, among others), they could remain in the soil or be absorbed by the biota (Reboreda and Caçador 2007). Also, plants inhabiting salt marshes play an essential role in the behavior of trace metals, by reducing tidewater flow favoring the sedimentation of transported particles and associated trace metals, and/or for being able to produce chemical changes in the soil, affecting metals' mobility, speciation, bioavailability and distribution (Duarte et al., 2010). Depending on soil condition, the metal and the plant species, salt marsh plants can absorb the metals accumulating them in the roots or through translocation metals accumulations are found in their aerial structures (Weis and Weis 2004). In fact, several studies have indicated that salt marsh plants have a crucial role in metal dynamics in these environments by affecting the biogenic cycle of metals (e.g., Almeida et al., 2006; Reboreda and Caçador 2007; Cambrollé et al., 2008; Duarte et al., 2010).

There is a complex of rocky shore salt marshes of little expansion in the vicinity of the city of Puerto Madryn, Chubut, Argentina (Bortolus 2010), all located on the Nuevo Gulf coast (~81000 inhabitants in 2010; INDEC) where the most important industrial activities are related to aluminium production. These industries are located inside the city leading to significant port activity. Tourism and fisheries are also important in this city, which also implies port movement. All these activities are potential sources of pollutants, that could be transported in the seawater or the air spreading from close areas to long distances before being deposited (Alloway 2010). Previous studies showed that sediments of the port zone have high concentrations of total aliphatic and aromatic hydrocarbons (Commendatore and Esteves 2007; Bigatti et al., 2009) as well as of trace metals (Gil et al., 1999; Primost et al., 2017). However, these substances can also reach nearby salt marshes and can accumulate in both soil and plants. These salt marshes are mainly inhabited by the cordgrass Spartina densiflora, which demonstrate a high tolerance and a capacity to accumulate vast amounts of different metals in their tissues, mainly in the roots (Cambrollé et al., 2008; Redondo-Gómez 2013; Idaszkin et al. 2014, 2015). Accordingly, the aims of this work were: (i) to determine the levels of trace metals in soils and Spartina densiflora tissues in rocky shore marshes of Central Patagonia; (ii) to relate metal concentration patterns in the different soil-plant complex fractions to environmental conditions; and (iii) to investigate whether geographical metal concentration patterns can be explained with anthropogenic influences and sources and/or by local prevailing biogeochemical processes.

Section snippets

Fieldwork and sample processing to soil physico-chemical determinations

In 2017 fieldwork was conducted in five rocky shore salt marshes located on the Nuevo Gulf coast, in Patagonia, Argentina (Fig. 1). Within the littoral sector of the Nuevo Gulf, only six salt marsh environments of little expression are recognized (Bortolus et al., 2009). Specifically, Medano, Pozo, Cerro and Ambrozetti are the salt marshes located from Puerto Madryn city towards the southern shore of the gulf, respectively, and Casino is the accessible salt marsh found towards the north. All

Soil physico-chemical properties and contamination degree analysis

Soil OM content, CEC and EC showed differences among salt marshes and followed a similar pattern of variation, such that these values were lower in the northern salt marsh (i.e. Casino) than in the salt marshes of the other margin of the Nuevo Gulf coast (Fig. 2A–C). Also pH showed certain differences among locations but overall these values were slightly basic in all of them (Fig. 2D). Regarding soil texture, the studied salt marshes were dominantly sandy to sandy loam, with clay percentage

Discussion

Even though rocky salt marshes of the Nuevo Gulf in Central Patagonia are located in an environment considered not very anthropized, they can receive metals from anthropogenic sources such as the city, the port area and industries of Puerto Madryn. In this work, the salt marshes located at the south (i.e. Médano, Pozo, Cerro and Ambrozetti) and the one that is accessible to the north (i.e. Casino) of these potential metal sources surrounding were analyzed. Although within the Nuevo Gulf

Conclusions

At present, the level of human impact in rocky shore salt marshes of the Nuevo Gulf in Central Patagonia associated to the trace metals pollution varies from being scarcely to significantly important, being the anthropogenic sources mainly related to the port and industrial activities. The salt marshes located in its southern margin showing the worst scenarios, due to the effect of the western coastal currents that disperse and transport the metals towards that sector of the gulf.

Some trace

Author contributions

Yanina Idaszkin: Writing - Original Draft preparation. Conceptualization. Investigation. Funding acquisition. Eleonora Carol: Writing- Original draft preparation. Investigation. José Mária Barcia-Piedras: Conceptualization. Investigation. Pablo Bouza: Investigation. Funding acquisition. Enrique Mateos-Naranjo: Conceptualization. Writing- Reviewing and Editing.

CRediT authorship contribution statement

L. Idaszkin Yanina: Writing - original draft, Conceptualization, Investigation, Funding acquisition. S. Carol Eleonora: Writing - original draft, Investigation. José María Barcia-Piedras: Conceptualization, Investigation. J. Bouza Pablo: Investigation, Funding acquisition. Enrique Mateos-Naranjo: Conceptualization, Writing - review & editing.

Declaration of competing interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Acknowledgements

We are especially grateful to Tomás Bosco for his useful help in the laboratory work and to Julio “Bocha” Rua and Ricardo “Bebote” Vera for their invaluable help in the fieldwork. We thank Fondo para la Investigación Científica y Tecnológica (PICT Nº 2016-0017 and Nº 2018-03802), and Consejo Nacional de Investigaciones Científicas y Tecnológicas (PIP 0190/14). J-M B-P thanks INIA for personal financial support. We also thank the useful comments of the anonymous reviewers who greatly helped to

References (93)

  • M.A. Huerta-Diaz et al.

    Geochemistry of trace metals associated with reduced sulfur in freshwater sediments

    J Appl. Geochem.

    (1998)
  • Y.L. Idaszkin et al.

    The role of Sarcocornia perennis in the interstitial water salinization process

    Continent. Shelf Res.

    (2020)
  • Y.L. Idaszkin et al.

    Trace metal concentrations in Spartina densiflora and associated soil from a Patagonian salt marsh

    Mar. Pollut. Bull.

    (2014)
  • Y.L. Idaszkin et al.

    Mechanism of removal and retention of heavy metals from the acid mine drainage to coastal wetland in the Patagonian marsh

    Chemosphere

    (2017)
  • Y.L. Idaszkin et al.

    Comparison of phytoremediation potential capacity of Spartina densiflora and Sarcocornia perennis for metal polluted soils

    Mar. Pollut. Bull.

    (2017)
  • Y.L. Idaszkin et al.

    Geochemical processes controlling the distribution and concentration of metals in soils from a Patagonian (Argentina) salt marsh affected by mining residues

    Sci. Total Environ.

    (2017)
  • Y.L. Idaszkin et al.

    Accumulation and distribution of trace metals within soils and the austral cordgrass Spartina densiflora in a Patagonian salt marsh

    Mar. Pollut. Bull.

    (2015)
  • V. Illera et al.

    Short-term effects of biosolid and municipal solid waste application on heavy metals distribution in a degraded soil under a semi-arid environment

    Sci. Total Environ.

    (2000)
  • C.H. Marinho et al.

    Distribution and origin of trace metals in sediments of a marine park (Northern San Jorge Gulf) from Argentina

    Mar. Pollut. Bull.

    (2013)
  • R.M. McKenzie

    Proton release during adsorption of heavy metal ions by a hydrous manganese dioxide

    Geochem. Cosmochim. Acta

    (1979)
  • J.W. Morse et al.

    Adsorption and coprecipitation of divalent metals with mackinawite (FeS)

    Geochem. Cosmochim. Acta

    (1993)
  • J.W. Morse et al.

    Chemical influences on trace metal-sulfide interactions in anoxic sediments

    Geochem. Cosmochim. Acta

    (1999)
  • R. Reboreda et al.

    Halophyte vegetation influences in salt marsh retention capacity for heavy metals

    Environ. Pollut.

    (2007)
  • J.H. Rodriguez et al.

    Accumulation of polycyclic aromatic hydrocarbons and heavy metals in the tree foliage of Eucalyptus rostrata, Pinus radiata and Populus hybridus in the vicinity of a large aluminium smelter in Argentina

    Atmos. Environ.

    (2012)
  • J. Sastre et al.

    Determination of Cd, Cu, Pb and Zn in environmental samples: microwave-assisted total digestion versus aqua regia and nitric acid extraction

    Anal. Chim. Acta

    (2002)
  • M.C. Sueiro et al.

    Interactions between ecosystem engineers: a native species indirectly facilitates a non-native one

    Acta Oecol.

    (2013)
  • A. Tessier et al.

    Metal sorption to diagenetic iron and manganese oxyhydroxides and associated organic matter: narrowing the gap between field and laboratory measurements

    Geochem. Cosmochim. Acta

    (1996)
  • J.W. Tonkin et al.

    Modeling sorption of divalent metal cations on hydrous manganese oxide using the diffuse double layer model

    Appl. Geochem.

    (2004)
  • C. Vale et al.

    Presence of metal rich rhizoconcretions on the roots of Spartina maritima from the salt marshes of the Tagus estuary, Portugal

    Sci. Total Environ.

    (1990)
  • J.S. Weis et al.

    Metal uptake, transport and release by wetland plants: implications for phytoremediation and restoration

    Environ. Int.

    (2004)
  • T.P. Williams et al.

    Metal accumulation within salt marsh environments: a review

    Mar. Pollut. Bull.

    (1994)
  • L. Windham et al.

    Uptake and distribution of metals in two dominant salt marsh macrophytes, Spartina alterniflora (cordgrass) and Phragmites australis (common reed)

    Estuar. Coast Shelf Sci.

    (2003)
  • J. Yoon et al.

    Accumulation of Pb, Cu, and Zn in native plants growing on a contaminated Florida site

    Sci. Total Environ.

    (2006)
  • S. Zhao et al.

    Salinity increases themobility of Cd, Cu,Mn, and Pb in the sediments of Yangtze Estuary: relative role of sediments properties and metal speciation

    Chemosphere

    (2013)
  • H. Agemian et al.

    Evaluation of extraction techniques for the determination of metals aquatic sediments

    Analyst

    (1976)
  • G.A. Ahearn et al.

    Mechanisms of heavy-metal sequestration and detoxification in crustaceans: a review

    J. Comp. Physiol. B

    (2004)
  • J. Alberti et al.

    Local and geographic variation in grazing intensity by herbivorous crabs in SW Atlantic salt marshes

    Mar. Ecol. Prog. Ser.

    (2007)
  • B.J. Alloway

    Heavy Metals in Soils. Trace Metals and Metalloids in Soils and Their Bioavailability

    (2010)
  • C.A.J. Appelo et al.

    Geochemistry, Groundwater and Pollution

    (2005)
  • E.B. Barbier et al.

    The value of estuarine and coastal ecosystem services

    Ecol. Monogr.

    (2011)
  • G.F. Birch

    A test of normalization methods for marine sediment, including a new post-extraction normalization (PEN) technique

    Hydrobiologia

    (2003)
  • C. Bloomfield

    The translocation of metal in soil

  • A. Bortolus

    Marismas patagónicas: las últimas de Sudamérica

    Ciencia Hoy

    (2010)
  • A. Bortolus et al.

    A characterization of Patagonian salt marshes

    Wetlands

    (2009)
  • S.E. Botté et al.

    Salt marshes: role within the Bahía Blanca estuary

  • P.J. Bouza et al.

    Patagonian salt marsh soils and oxidizable pedogenic pyrite: solid phases controlling aluminum and iron contents in acidic soil solutions

    Environ. Earth Sci.

    (2019)
  • Cited by (7)

    • Contamination status and associated ecological risk assessment of heavy metals in different wetland sediments from an urbanized estuarine ecosystem

      2022, Marine Pollution Bulletin
      Citation Excerpt :

      However, the present findings were assessed by comparing with other similar works (Table 2) as there was no existing data on metal loads at different types of wetlands in this river. It was observed that the load of Pb, Zn, and Ni in the saltmarsh of this study was higher than previous studies (Rakib et al., 2021; Idaszkin et al., 2020). In contrast, Pb, Zn, Ni, and Cr load in mudflat of this experiment was lower than that of Ulhas Estuary, India (Fernandes and Nayak, 2012).

    • Soil metal pollution assessment in Sarcocornia salt marshes in a South American estuary

      2021, Marine Pollution Bulletin
      Citation Excerpt :

      OM content was low but in the range observed in Sarcocornia salt marshes worldwide (Duarte et al., 2010; Curado et al., 2014; Pedro et al., 2015; Idaszkin et al., 2017a); moreover, low OM levels are consistent with values usually found in the BBE, both in soils vegetated by S. alterniflora (Negrin et al., 2019) and in unvegetated tidal flats (Spetter et al., 2015; Simonetti et al., 2017; Serra et al., 2017). Salinity was higher than values found in other studies in Sarcocornia marshes (Duarte et al., 2010; Curado et al., 2014; Idaszkin et al., 2017a, 2017b, 2020) whereas Eh was lower than usually reported for Sarcocornia marshes both in the BBE (Negrin et al., 2013) and in other salt marshes (Duarte et al., 2010; Curado et al., 2014; Idaszkin et al., 2017a). Eh values in this study were always negative, varying between approximately −10 and −240 mV, indicating reduced conditions (Reddy and DeLaune, 2008), which might be related to the fact that the previous high tide reached 4.5 m (it was a spring tide) and flooded the high marsh which is usually not flooded considering that the mean high tide in the BBE is 3.3 m (Perillo and Piccolo, 1991).

    View all citing articles on Scopus
    View full text