A global perspective on wetland salinization : Ecological consequences of a growing threat to freshwater wetlands
- Herbert, Ellen, Boon, Paul, Burgin, Amy, Neubauer, Scott, Franklin, Rima, Ardon, Marcelo, Hopfensperger, Kristine, Lamers, Leon, Gell, Peter
- Authors: Herbert, Ellen , Boon, Paul , Burgin, Amy , Neubauer, Scott , Franklin, Rima , Ardon, Marcelo , Hopfensperger, Kristine , Lamers, Leon , Gell, Peter
- Date: 2015
- Type: Text , Journal article
- Relation: Ecosphere Vol. 6, no. 10 (2015), p. 1-43
- Full Text:
- Reviewed:
- Description: Salinization, a widespread threat to the structure and ecological functioning of inland and coastal wetlands, is currently occurring at an unprecedented rate and geographic scale. The causes of salinization are diverse and include alterations to freshwater flows, land-clearance, irrigation, disposal of wastewater effluent, sea level rise, storm surges, and applications of de-icing salts. Climate change and anthropogenic modifications to the hydrologic cycle are expected to further increase the extent and severity of wetland salinization. Salinization alters the fundamental physicochemical nature of the soil-water environment, increasing ionic concentrations and altering chemical equilibria and mineral solubility. Increased concentrations of solutes, especially sulfate, alter the biogeochemical cycling of major elements including carbon, nitrogen, phosphorus, sulfur, iron, and silica. The effects of salinization on wetland biogeochemistry typically include decreased inorganic nitrogen removal (with implications for water quality and climate regulation), decreased carbon storage (with implications for climate regulation and wetland accretion), and increased generation of toxic sulfides (with implications for nutrient cycling and the health/functioning of wetland biota). Indeed, increased salt and sulfide concentrations induce physiological stress in wetland biota and ultimately can result in large shifts in wetland communities and their associated ecosystem functions. The productivity and composition of freshwater species assemblages will be highly altered, and there is a high potential for the disruption of existing interspecific interactions. Although there is a wealth of information on how salinization impacts individual ecosystem components, relatively few studies have addressed the complex and often non-linear feedbacks that determine ecosystem-scale responses or considered how wetland salinization will affect landscape-level processes. Although the salinization of wetlands may be unavoidable in many cases, these systems may also prove to be a fertile testing ground for broader ecological theories including (but not limited to): investigations into alternative stable states and tipping points, trophic cascades, disturbance-recovery processes, and the role of historical events and landscape context in driving community response to disturbance. © 2015 Herbert et al.
- Authors: Herbert, Ellen , Boon, Paul , Burgin, Amy , Neubauer, Scott , Franklin, Rima , Ardon, Marcelo , Hopfensperger, Kristine , Lamers, Leon , Gell, Peter
- Date: 2015
- Type: Text , Journal article
- Relation: Ecosphere Vol. 6, no. 10 (2015), p. 1-43
- Full Text:
- Reviewed:
- Description: Salinization, a widespread threat to the structure and ecological functioning of inland and coastal wetlands, is currently occurring at an unprecedented rate and geographic scale. The causes of salinization are diverse and include alterations to freshwater flows, land-clearance, irrigation, disposal of wastewater effluent, sea level rise, storm surges, and applications of de-icing salts. Climate change and anthropogenic modifications to the hydrologic cycle are expected to further increase the extent and severity of wetland salinization. Salinization alters the fundamental physicochemical nature of the soil-water environment, increasing ionic concentrations and altering chemical equilibria and mineral solubility. Increased concentrations of solutes, especially sulfate, alter the biogeochemical cycling of major elements including carbon, nitrogen, phosphorus, sulfur, iron, and silica. The effects of salinization on wetland biogeochemistry typically include decreased inorganic nitrogen removal (with implications for water quality and climate regulation), decreased carbon storage (with implications for climate regulation and wetland accretion), and increased generation of toxic sulfides (with implications for nutrient cycling and the health/functioning of wetland biota). Indeed, increased salt and sulfide concentrations induce physiological stress in wetland biota and ultimately can result in large shifts in wetland communities and their associated ecosystem functions. The productivity and composition of freshwater species assemblages will be highly altered, and there is a high potential for the disruption of existing interspecific interactions. Although there is a wealth of information on how salinization impacts individual ecosystem components, relatively few studies have addressed the complex and often non-linear feedbacks that determine ecosystem-scale responses or considered how wetland salinization will affect landscape-level processes. Although the salinization of wetlands may be unavoidable in many cases, these systems may also prove to be a fertile testing ground for broader ecological theories including (but not limited to): investigations into alternative stable states and tipping points, trophic cascades, disturbance-recovery processes, and the role of historical events and landscape context in driving community response to disturbance. © 2015 Herbert et al.
Floodplain lakes: Evolution and response
- Hausmann, Sonja, Hall, Roland, Gell, Peter
- Authors: Hausmann, Sonja , Hall, Roland , Gell, Peter
- Date: 2011
- Type: Text , Journal article
- Relation: Eos Vol. 92, no. 18 (2011), p. 154
- Full Text: false
- Reviewed:
- Description: PAGES International Floodplain Lakes Workshop; Fayetteville, Arkansas, 16-19 September 2010; Human alteration of the major rivers and floodplains of the world is a global concern because they sustain aquatic ecosystems and supply food and energy to society. When in flood stage, the influence of a river extends across the floodplain and can revitalize productive wetlands. The condition of many rivers has declined worldwide, but the degree of degradation is hard to assess due to natural variability of flow and uncertainty of baseline status. Evidence of changes over decades to millennia in river and wetland conditions, however, can be quantified from physical, chemical, and biological information archived in the accumulated sediments of floodplain lakes.
- Authors: Lynch, Jasmyn
- Date: 2011
- Type: Text , Journal article
- Relation: Environmental Management Vol. 471, no. 1 (2011), p. 40-55
- Full Text: false
- Reviewed:
- Description: There is no comprehensive system of describing threats and disturbances currently used in Australia, despite the widespread impacts of human activities on natural ecosystems. Yet a detailed categorization would facilitate the collation of threatening process information into information systems; enable standardized collection and availability of data; and enable comparative analyses of ecosystem condition between stakeholders, agencies, states, and nations, particularly for environmental reporting and evaluation mechanisms such as State of the Environment. As part of the Queensland Wetlands Programme (QWP), a threat and disturbance framework was developed, focused on the pressure and impacts components of the DPSIR (driver-pressure-state-impacts-response) framework. A wetland inventory database was developed also that included a detailed threat and disturbance categorization using the QWP framework. The categorization encompasses a broad range of anthropogenic and natural processes, and is hierarchical to accommodate varying levels of detail or knowledge. By incorporating detailed qualitative and quantitative information, a comprehensive threats and disturbances categorization can contribute to conceptual or spatially explicit knowledge and management assessments. The application of the framework and categorization to several threatening processes is demonstrated, and its relationship to current natural resource condition indicators is discussed. Threat evaluation is an essential component of ecological assessment and environmental management, and a standardized categorization enables consistency in attributing processes, impacts and their short- to long-term consequences. Such a systematic framework and categorization demonstrates the importance and usefulness of comprehensive approaches, and this approach can be readily adapted to management, monitoring and evaluation of other target ecosystems and biota.
Developing a complementary framework for urban ecology
- Kattel, Giri, Elkadi, Hisham, Meikle, Helen
- Authors: Kattel, Giri , Elkadi, Hisham , Meikle, Helen
- Date: 2013
- Type: Text , Journal article
- Relation: Urban Forestry & Urban Greening Vol. 12, no. 4 (2013), p. 498-508
- Full Text:
- Reviewed:
- Description: Cities are characterized by dynamic interactions between socio-economic and biophysical forces. Currently more than half of the global population reside in cities which influence the global biogeochemical cycles and climate change, substantially exacerbating pressures on urban pollution, water quality and food security, as well as operating costs for infrastructure development. Goods and services such as aesthetic values, water purification, nutrient recycling, and biological diversity, that urban ecosystems generate for the society, are critical to sustain. Urban planners are increasingly facing the considerable challenges of management issues for urban ecosystems. Poor understanding of the complementary roles of urban ecology in urban infrastructure, and the functioning of ecosystems and ecological resilience of a complex human-dominated landscape has impeded effective urban planning over time, resulting in social disharmony. Here a complementary framework for urban ecology is proposed, in which ecosystems interact with land use, architecture and urban design - "E-LAUD"-affecting ecosystem and human health, and building on the concept that land uses in urban green areas, road-strips, wetlands, 'habitat islands' and urban architecture could synergistically benefit when clustered together in different combinations of urban landscapes. It is proposed that incorporation of the E-LAUD framework in urban planning forms the context of a new interdisciplinary research programme on ecological resilience for urban ecosystems and helps promote ecosystem services. (C) 2013 Elsevier GmbH. All rights reserved.
- Authors: Kattel, Giri , Elkadi, Hisham , Meikle, Helen
- Date: 2013
- Type: Text , Journal article
- Relation: Urban Forestry & Urban Greening Vol. 12, no. 4 (2013), p. 498-508
- Full Text:
- Reviewed:
- Description: Cities are characterized by dynamic interactions between socio-economic and biophysical forces. Currently more than half of the global population reside in cities which influence the global biogeochemical cycles and climate change, substantially exacerbating pressures on urban pollution, water quality and food security, as well as operating costs for infrastructure development. Goods and services such as aesthetic values, water purification, nutrient recycling, and biological diversity, that urban ecosystems generate for the society, are critical to sustain. Urban planners are increasingly facing the considerable challenges of management issues for urban ecosystems. Poor understanding of the complementary roles of urban ecology in urban infrastructure, and the functioning of ecosystems and ecological resilience of a complex human-dominated landscape has impeded effective urban planning over time, resulting in social disharmony. Here a complementary framework for urban ecology is proposed, in which ecosystems interact with land use, architecture and urban design - "E-LAUD"-affecting ecosystem and human health, and building on the concept that land uses in urban green areas, road-strips, wetlands, 'habitat islands' and urban architecture could synergistically benefit when clustered together in different combinations of urban landscapes. It is proposed that incorporation of the E-LAUD framework in urban planning forms the context of a new interdisciplinary research programme on ecological resilience for urban ecosystems and helps promote ecosystem services. (C) 2013 Elsevier GmbH. All rights reserved.
Changing fluxes of sediments and salts as recorded in lower River Murray wetlands, Australia
- Gell, Peter, Fluin, Jennie, Tibby, John, Haynes, Deborah, Khanum, Syeda, Walsh, Brendan, Hancock, Gary, Harrison, Jennifer, Zawadzki, Atun, Little, Fiona
- Authors: Gell, Peter , Fluin, Jennie , Tibby, John , Haynes, Deborah , Khanum, Syeda , Walsh, Brendan , Hancock, Gary , Harrison, Jennifer , Zawadzki, Atun , Little, Fiona
- Date: 2006
- Type: Conference proceedings
- Full Text:
- Description: The River Murray basin, Australia's largest, has been significantly impacted by changed flow regimes and increased fluxes of salts and sediments since settlement in the 1840s. The river's flood plain hosts an array of cut-off meanders, levee lakes and basin depression lakes that archive historical changes. Pre-European sedimentation rates are typically approx. 0.1-1 mm year-1, while those in the period after European arrival are typically 10 to 30 fold greater. This increased sedimentation corresponds to a shift in wetland trophic state from submerged macrophytes in clear waters to phytoplankton-dominated, turbid systems. There is evidence for a decline in sedimentation in some natural wetlands after river regulation from the 1920s, but with the maintenance of the phytoplankton state. Fossil diatom assemblages reveal that, while some wetlands had saline episodes before settlement, others became saline after, and as early as the 1880s. The oxidation of sulphurous salts deposited after regulation has induced hyperacidity in a number of wetlands in recent years. While these wetlands are rightly perceived as being heavily impacted, other, once open water systems, that have infilled and now support rich macrophyte beds, are used as interpretive sites. The rate of filling, however, suggests that the lifespan of these wetlands is short. The rate of wetland loss through such increased infilling is unlikely to be matched by future scouring as regulation has eliminated middle order floods from the lower catchment.
- Authors: Gell, Peter , Fluin, Jennie , Tibby, John , Haynes, Deborah , Khanum, Syeda , Walsh, Brendan , Hancock, Gary , Harrison, Jennifer , Zawadzki, Atun , Little, Fiona
- Date: 2006
- Type: Conference proceedings
- Full Text:
- Description: The River Murray basin, Australia's largest, has been significantly impacted by changed flow regimes and increased fluxes of salts and sediments since settlement in the 1840s. The river's flood plain hosts an array of cut-off meanders, levee lakes and basin depression lakes that archive historical changes. Pre-European sedimentation rates are typically approx. 0.1-1 mm year-1, while those in the period after European arrival are typically 10 to 30 fold greater. This increased sedimentation corresponds to a shift in wetland trophic state from submerged macrophytes in clear waters to phytoplankton-dominated, turbid systems. There is evidence for a decline in sedimentation in some natural wetlands after river regulation from the 1920s, but with the maintenance of the phytoplankton state. Fossil diatom assemblages reveal that, while some wetlands had saline episodes before settlement, others became saline after, and as early as the 1880s. The oxidation of sulphurous salts deposited after regulation has induced hyperacidity in a number of wetlands in recent years. While these wetlands are rightly perceived as being heavily impacted, other, once open water systems, that have infilled and now support rich macrophyte beds, are used as interpretive sites. The rate of filling, however, suggests that the lifespan of these wetlands is short. The rate of wetland loss through such increased infilling is unlikely to be matched by future scouring as regulation has eliminated middle order floods from the lower catchment.
- Grundell, Rosie, Gell, Peter, Mills, Keely, Zawadzki, Atun
- Authors: Grundell, Rosie , Gell, Peter , Mills, Keely , Zawadzki, Atun
- Date: 2012
- Type: Text , Journal article
- Relation: Journal of Paleolimnology Vol. 47, no. 2 (2012), p. 205-219
- Full Text: false
- Reviewed:
- Description: Sinclair Flat is small wetland, located within the gorge section of the Murray River floodplain. situated near Blanchetown, South Australia, the wetland is closely linked to the River and, since regulation, has become permanently inundated. High summer evaporation rates deplete the volume of water within the wetland. However, this is compensated by perennial inflow via a permanent inlet from the River. This site provides an opportunity to explore the relative contribution of river and wetland diatom flora to the sediment record, and the fluvial and aerial contribution of radiometric isotopes to the system. The geochronological and biostratigraphic data provide an insight into the history of the water quality of Sinclair Flat. Evidence exists for the River being a source of sediments and isotopes and of diatom species typical of the main river channel. Prior to 1950, Sinclair Flat was an oligotrophic, oligosaline, clear-water wetland. The wetland shifted gradually to an environment that favoured clear-water benthic species, most likely as a consequence of changes following river regulation in the 1920s, although the capacity to date these sediments is limited. During the 1950s, the wetland became plankton dominated. Peaks in epiphytic diatoms during the 1960s suggest increased emergent macrophyte cover. The contemporary condition is of a connected, turbid, eutrophic and mesosaline lagoon. The ecological condition of Sinclair Flat has diverged considerably from its historical range of condition. This record supports evidence from upstream of widespread state switches in the Murray-Darling Basin floodplain wetlands. This record also lends considerable weight to modern studies attesting to the degraded state of the waterways of the Murray-Darling Basin and the impact of river regulation practices on the water quality of these ecosystems. © 2011 Springer Science+Business Media B.V.
Future wet grasslands : Ecological implications of climate change
- Joyce, Chris, Simpson, Matthew, Casanova, Michelle
- Authors: Joyce, Chris , Simpson, Matthew , Casanova, Michelle
- Date: 2016
- Type: Text , Journal article
- Relation: Ecosystem Health and Sustainability Vol. 2, no. 9 (2016), p. 1-15
- Full Text:
- Reviewed:
- Description: Wet grasslands are threatened by future climate change, yet these are vital ecosystems for both conservation and agriculture, providing livelihoods for millions of people. These biologically diverse, transitional wetlands are defined by an abundance of grasses and periodic flooding, and maintained by regular disturbances such as grazing or cutting. This study summarizes relevant climate change scenarios projected by the Intergovernmental Panel on Climate Change and identifies implications for wet grasslands globally and regionally. Climate change is predicted to alter wet grassland hydrology, especially through warming, seasonal precipitation variability, and the severity of extreme events such as droughts and floods. Changes in the diversity, composition, and productivity of vegetation will affect functional and competitive relations between species. Extreme storm or flood events will favor ruderal plant species able to respond rapidly to environmental change. In some regions, wet grasslands may dry out during heatwaves and drought. C4 grasses and invasive species could benefit from warming scenarios, the latter facilitated by disturbances such as droughts, floods, and possibly wildfires. Agriculture will be affected as forage available for livestock will likely become less reliable, necessitating adaptations to cutting and grazing regimes by farmers and conservation managers, and possibly leading to land abandonment. It is recommended that agri-environment schemes, and other policies and practices, are adapted to mitigate climate change, with greater emphasis on water maintenance, flexible management, monitoring, and restoration of resilient wet grasslands.
- Authors: Joyce, Chris , Simpson, Matthew , Casanova, Michelle
- Date: 2016
- Type: Text , Journal article
- Relation: Ecosystem Health and Sustainability Vol. 2, no. 9 (2016), p. 1-15
- Full Text:
- Reviewed:
- Description: Wet grasslands are threatened by future climate change, yet these are vital ecosystems for both conservation and agriculture, providing livelihoods for millions of people. These biologically diverse, transitional wetlands are defined by an abundance of grasses and periodic flooding, and maintained by regular disturbances such as grazing or cutting. This study summarizes relevant climate change scenarios projected by the Intergovernmental Panel on Climate Change and identifies implications for wet grasslands globally and regionally. Climate change is predicted to alter wet grassland hydrology, especially through warming, seasonal precipitation variability, and the severity of extreme events such as droughts and floods. Changes in the diversity, composition, and productivity of vegetation will affect functional and competitive relations between species. Extreme storm or flood events will favor ruderal plant species able to respond rapidly to environmental change. In some regions, wet grasslands may dry out during heatwaves and drought. C4 grasses and invasive species could benefit from warming scenarios, the latter facilitated by disturbances such as droughts, floods, and possibly wildfires. Agriculture will be affected as forage available for livestock will likely become less reliable, necessitating adaptations to cutting and grazing regimes by farmers and conservation managers, and possibly leading to land abandonment. It is recommended that agri-environment schemes, and other policies and practices, are adapted to mitigate climate change, with greater emphasis on water maintenance, flexible management, monitoring, and restoration of resilient wet grasslands.
Socio-ecological value of wetlands: The dilemma of balancing human and ecological water needs
- Graymore, Michelle, McBride, Dawn
- Authors: Graymore, Michelle , McBride, Dawn
- Date: 2013
- Type: Text , Journal article
- Relation: Australasian Journal of Environmental Management Vol. 20, no. 3 (2013), p. 225-241
- Full Text:
- Reviewed:
- Description: Humans' need for water has changed flow regimes, degraded ecosystems and depleted water resources. In the Wimmera Mallee in Victoria, the dilemma between human and ecological water requirements began in the colonial era when a channel and dam system was built to transport water. Prolonged drought prompted government to replace this with the Wimmera Mallee Pipeline. This pipeline produced a closed system, reducing water available for the environment, including on-farm wetlands. This study identifies the socio-ecological values of on-farm wetlands and the impact the changed water regime had on these. An interpretative landscape approach was used to integrate geophysical, ecological and social information on nine on-farm wetlands. This identified a range of socio-ecological values on-farm wetlands provide, including aesthetic, amenity, production and biodiversity, that are impacted by the pipeline system. A range of implications for on-farm wetland management were also identified. © 2013 Copyright Environment Institute of Australia and New Zealand Inc.
- Description: C1
- Authors: Graymore, Michelle , McBride, Dawn
- Date: 2013
- Type: Text , Journal article
- Relation: Australasian Journal of Environmental Management Vol. 20, no. 3 (2013), p. 225-241
- Full Text:
- Reviewed:
- Description: Humans' need for water has changed flow regimes, degraded ecosystems and depleted water resources. In the Wimmera Mallee in Victoria, the dilemma between human and ecological water requirements began in the colonial era when a channel and dam system was built to transport water. Prolonged drought prompted government to replace this with the Wimmera Mallee Pipeline. This pipeline produced a closed system, reducing water available for the environment, including on-farm wetlands. This study identifies the socio-ecological values of on-farm wetlands and the impact the changed water regime had on these. An interpretative landscape approach was used to integrate geophysical, ecological and social information on nine on-farm wetlands. This identified a range of socio-ecological values on-farm wetlands provide, including aesthetic, amenity, production and biodiversity, that are impacted by the pipeline system. A range of implications for on-farm wetland management were also identified. © 2013 Copyright Environment Institute of Australia and New Zealand Inc.
- Description: C1
Tidally driven water column hydro-geochemistry in a remediating acidic wetland
- Johnston, Scott, Keene, Annabelle, Bush, Richard, Sullivan, Leigh, Wong, Vanessa
- Authors: Johnston, Scott , Keene, Annabelle , Bush, Richard , Sullivan, Leigh , Wong, Vanessa
- Date: 2011
- Type: Text , Journal article
- Relation: Journal of Hydrology Vol. 409, no. 1-2 (2011), p. 128-139
- Full Text: false
- Reviewed:
- Description: Managed tidal inundation is a newly evolved technique for remediating coastal acid sulphate soil (CASS) wetlands. However, there remains considerable uncertainty regarding the hydro-geochemical pathways and spatiotemporal dynamics of residual H+ and metal(loid) mobilisation into the tidal fringe surface waters of these uniquely iron-rich landscapes. Here, we examine the hydrology and water column chemistry across the intertidal slope of a remediating CASS wetland during several tide cycles. There was extreme spatial and temporal dynamism in water column chemistry, with pH fluctuating by ∼3 units (∼3.5-6.5) during a single tide cycle. Acute acidity was spatially confined to the upper intertidal slope, reflecting surface sediment properties, and tidal overtopping is an important pathway for mobilisation of residual H+ and Al3+ to the water column. Marine derived HCO3- was depleted from surface waters migrating across the intertidal slope and a strong gradient in HCO3- was observed from the tidal fringe to the adjacent tributary channel and nearby estuary. Tidal forcing generated oscillating hydraulic gradients in the shallow fringing aquifer, favouring ebb-tide seepage and driving rapid, heterogeneous advection of groundwater on the lower intertidal slope via surface connected macropores. A combination of diffusive and advective flux across the sediment-water interface led to persistent, elevated surface water Fe2+ (∼10-1000μM). The geochemical processes associated with Fe2+ mobilisation displayed distinct spatial zonation, with low pH, proton-promoted desorption occurring on the upper intertidal slope, whilst circum-neutral pH, Fe(III)-reducing processes dominated the lower intertidal slope. Arsenic was also mobilised into surface waters on the lower intertidal slope under moderate pH (∼6.0) conditions and was strongly positively correlated with Fe2+. Saturation index values for aragonite were substantially depressed (-1 to -5) and significantly negatively correlated with elevation, thereby presenting a barrier to re-colonisation of the upper intertidal slope by calcifying benthic organisms. These findings highlight the spatially complex hydrological and geochemical controls on surface water quality that can occur in tidally inundated acid sulphate soil environments. © 2011 Elsevier B.V.
Sulfur biogeochemical cycling and novel Fe-S mineralization pathways in a tidally re-flooded wetland
- Burton, Edward, Bush, Richard, Johnston, Scott, Sullivan, Leigh, Keene, Annabelle
- Authors: Burton, Edward , Bush, Richard , Johnston, Scott , Sullivan, Leigh , Keene, Annabelle
- Date: 2011
- Type: Text , Journal article
- Relation: Geochimica et Cosmochimica Acta Vol. 75, no. 12 (2011), p. 3434-3451
- Full Text: false
- Reviewed:
- Description: Sulfur biogeochemical cycling and associated Fe-S mineralization processes exert a major influence over acidity dynamics, electron flow and contaminant mobility in wetlands, benthic sediments and groundwater systems. While S biogeochemical cycling has been studied intensively in many environmental settings, relatively little direct information exists on S cycling in formerly drained wetlands that have been remediated via tidal re-flooding. This study focuses on a tidal wetland that was drained in the 1970s (causing severe soil and water acidification), and subsequently remediated by controlled re-flooding in 2002. We examine SO42- reduction rates and Fe-S mineralization at the tidal fringe, 7years after the commencement of re-flooding. The initial drainage of the wetland examined here caused in-situ pyrite (FeS2) oxidation, resulting in the drained soil layers being highly acidic and rich in SO42--bearing Fe(III) minerals, including jarosite (KFe3(SO4)2(OH)6). Tidal re-flooding has neutralized much of the previous acidity, with the pore-water pH now mostly spanning pH 5-7. The fastest rates of in-situ SO42- reduction (up to ~300nmolcm-3day-1) occur within the inter-tidal zone in the near-surface soil layers (to ~60cm below ground surface). The SO42- reduction rates correlate with pore-water dissolved organic C concentrations, thereby suggesting that electron donor supply was the predominant rate determining factor. Elemental S was a major short-term product of SO42- reduction, comprising up to 69% of reduced inorganic S in the near-surface soil layers. This enrichment in elemental S can be partly attributed to interactions between biogenic H2S and jarosite - a process that also contributed to enrichment in pore-water Fe2+ (up to 55mM) and SO42- (up to 50mM). The iron sulfide thiospinel, greigite (Fe3S4), was abundant in near-surface soil layers within the inter- to sub-tidal zone where tidal water level fluctuations created oscillatory redox conditions. There was evidence for relatively rapid pyrite re-formation within the re-flooded soil layers. However, the results indicate that pyrite re-formation has occurred mainly in the lower formerly drained soil layers, whereas the accumulation of elemental S and greigite has been confined towards the soil surface. The discovery that pyrite formation was spatially decoupled from that of elemental S and greigite challenges the concept that greigite is an essential precursor required for sedimentary pyrite formation. In fact, the results suggest that greigite and pyrite may represent distinct end-points of divergent Fe-S mineralization pathways. Overall, this study highlights novel aspects of Fe-S mineralization within tidal wetlands that have been drained and re-flooded, in contrast to normal, undisturbed tidal wetlands. As such, the long-term biogeochemical trajectory of drained and acidified wetlands that are remediated by tidal re-flooding cannot be predicted from the well-studied behaviour of normal tidal wetlands. © 2011 Elsevier Ltd.
Effects of hyper-enriched reactive Fe on sulfidisation in a tidally inundated acid sulfate soil wetland
- Keene, Annabelle, Johnston, Scott, Bush, Richard, Sullivan, Leigh, Burton, Edward, McElnea, Angus, Ahern, Col, Powell, Bernard
- Authors: Keene, Annabelle , Johnston, Scott , Bush, Richard , Sullivan, Leigh , Burton, Edward , McElnea, Angus , Ahern, Col , Powell, Bernard
- Date: 2011
- Type: Text , Journal article
- Relation: Biogeochemistry Vol. 103, no. 1 (2011), p. 263-279
- Full Text:
- Reviewed:
- Description: Solid phase Fe and S fractions were examined in an acid sulfate soil (ASS) wetland undergoing remediation via tidal inundation. Considerable diagenetic enrichment of reactive Fe(III) oxides (HCl- and dithionite-extractable) occurred near the soil surface (0-0.05 m depth), where extremely large concentrations up to 3534 μmol/g accounted for ~90% of the total Fe pool. This major source of reactive Fe exerts a substantial influence on S cycling and the formation, speciation and transformation of reduced inorganic S (RIS) in tidally inundated ASS. Under these geochemical conditions, acid volatile sulfide (AVS; up to 57 μmol/g) and elemental sulfur (S0; up to 41 μmol/g) were the dominant fractions of RIS in near surface soils. AVS-S to pyrite-S ratios exceeded 2.9 near the surface, indicating that abundant reactive Fe favoured the accumulation of AVS minerals and S0 over pyrite. This is supported by the significant correlation of poorly crystalline Fe with AVS-S and S0-S contents (r = 0.83 and r = 0.85, respectively, P < 0.01). XANES spectroscopy provided direct evidence for the presence of a greigite-like phase in AVS-S measured by chemical extraction. While the abundant reactive Fe may limit the transformation of AVS minerals and S0 to pyrite during early diagenesis (~5 years), continued sulfidisation over longer time scales is likely to eventually lead to enhanced sequestration of S within pyrite (with a predicted 8% pyrite by mass). These findings provide an important understanding of sulfidisation processes occurring in reactive Fe-enriched, tidally inundated ASS landscapes. © 2010 Springer Science+Business Media B.V.
- Authors: Keene, Annabelle , Johnston, Scott , Bush, Richard , Sullivan, Leigh , Burton, Edward , McElnea, Angus , Ahern, Col , Powell, Bernard
- Date: 2011
- Type: Text , Journal article
- Relation: Biogeochemistry Vol. 103, no. 1 (2011), p. 263-279
- Full Text:
- Reviewed:
- Description: Solid phase Fe and S fractions were examined in an acid sulfate soil (ASS) wetland undergoing remediation via tidal inundation. Considerable diagenetic enrichment of reactive Fe(III) oxides (HCl- and dithionite-extractable) occurred near the soil surface (0-0.05 m depth), where extremely large concentrations up to 3534 μmol/g accounted for ~90% of the total Fe pool. This major source of reactive Fe exerts a substantial influence on S cycling and the formation, speciation and transformation of reduced inorganic S (RIS) in tidally inundated ASS. Under these geochemical conditions, acid volatile sulfide (AVS; up to 57 μmol/g) and elemental sulfur (S0; up to 41 μmol/g) were the dominant fractions of RIS in near surface soils. AVS-S to pyrite-S ratios exceeded 2.9 near the surface, indicating that abundant reactive Fe favoured the accumulation of AVS minerals and S0 over pyrite. This is supported by the significant correlation of poorly crystalline Fe with AVS-S and S0-S contents (r = 0.83 and r = 0.85, respectively, P < 0.01). XANES spectroscopy provided direct evidence for the presence of a greigite-like phase in AVS-S measured by chemical extraction. While the abundant reactive Fe may limit the transformation of AVS minerals and S0 to pyrite during early diagenesis (~5 years), continued sulfidisation over longer time scales is likely to eventually lead to enhanced sequestration of S within pyrite (with a predicted 8% pyrite by mass). These findings provide an important understanding of sulfidisation processes occurring in reactive Fe-enriched, tidally inundated ASS landscapes. © 2010 Springer Science+Business Media B.V.
- Lynch, Jasmyn, Ferrier, Asa, Ford, Andrew, Haberle, Simon, Rule, Stephen, Schneider, Larissa, Zawadzki, A., Metcalfe, Daniel
- Authors: Lynch, Jasmyn , Ferrier, Asa , Ford, Andrew , Haberle, Simon , Rule, Stephen , Schneider, Larissa , Zawadzki, A. , Metcalfe, Daniel
- Date: 2020
- Type: Text , Journal article
- Relation: Landscape Ecology Vol. 35, no. 1 (2020), p. 83-99
- Full Text: false
- Reviewed:
- Description: Context: Transdisciplinary research is important where information from multiple fields is required to develop ecologically and culturally appropriate environmental planning that protects local conservation and socio-cultural values. Objectives: Here, we describe research to inform ecosystem restoration and conservation of Chumbrumba Swamp within the Wet Tropics World Heritage Area, Australia. Many such open wetlands in the region have been degraded through agriculture and pastoral production, but there has been little research into their status, history and conservation needs. Methods: The recent to pre-European settlement history of the site was explored, along with spatial variation of vegetation communities at the site, and these data integrated with historical and ethnographical information on the site and its cultural values. Results: The botanical and palaeoecological analyses showed that Chumbrumba Swamp comprises a unique and highly sensitive ecosystem mosaic with high biodiversity. An endangered ecosystem complex, 82 vascular plant species, several disjunct or endemic taxa, and species at new northern range limits were recorded within its 20 ha area. The site comprises a stable swamp site with fringing woodland and rainforest that has persisted for around 5000 years. European settlement overlaid changes in the vegetation from disturbance (e.g. fire, clearing, grazing). However, fire also affected the swamp site during pre-European times. Conclusions: Historical and ethnographic information contextualised the biophysical data and confirmed the cultural importance of the site and the dynamic interactions between ‘people and nature’. These results have been used to inform environmental restoration and validate the importance of a transdisciplinary and precautionary approach to planning wetland restoration and conservation. © 2019, Springer Nature B.V.
Anthropogenic acceleration of sediment accretion in lowland floodplain wetlands, Murray-Darling Basin, Australia
- Gell, Peter, Fluin, Jenny, Tibby, John, Hancock, Gary, Harrison, Jennifer, Zawadzki, Atun, Haynes, Deborah, Khanum, Syeda, Little, Fiona, Walsh, Brendan
- Authors: Gell, Peter , Fluin, Jenny , Tibby, John , Hancock, Gary , Harrison, Jennifer , Zawadzki, Atun , Haynes, Deborah , Khanum, Syeda , Little, Fiona , Walsh, Brendan
- Date: 2009
- Type: Text , Journal article
- Relation: Geomorphology Vol. 108, no. 1-2 (2009), p. 122-126
- Full Text:
- Reviewed:
- Description: Over the last decade there has been a deliberate focus on the application of paleolimnological research to address issues of sediment flux and water quality change in the wetlands of the Murray-Darling Basin of Australia. This paper reports on the research outcomes on cores collected from sixteen wetlands along the Murrumbidgee-Murray River continuum. In all sixteen wetlands radiometric techniques and exotic pollen biomarkers were used to establish sedimentation rates from the collected cores. Fossil diatom assemblages were used to identify water source and quality changes to the wetlands. The sedimentation rates of all wetlands accelerated after European settlement, as little as two-fold, and as much as eighty times the mean rate through the Late Holocene. Some wetlands completely infilled through the Holocene, while others have rapidly progressed towards a terrestrial state due to accelerated accretion rates. Increasing wetland salinity and turbidity commenced within decades of settlement, contributing to sediment inputs. The sedimentation rate was observed to slow after river regulation in one wetland, but has accelerated recently in others. The complex history of flooding and drying, and wetland salinisation and eutrophication, influence the reliability of models used to establish recent, fine-resolution chronologies with confidence and the capacity to attribute causes to documented effects. © 2008 Elsevier B.V.
- Description: 2003006710
- Authors: Gell, Peter , Fluin, Jenny , Tibby, John , Hancock, Gary , Harrison, Jennifer , Zawadzki, Atun , Haynes, Deborah , Khanum, Syeda , Little, Fiona , Walsh, Brendan
- Date: 2009
- Type: Text , Journal article
- Relation: Geomorphology Vol. 108, no. 1-2 (2009), p. 122-126
- Full Text:
- Reviewed:
- Description: Over the last decade there has been a deliberate focus on the application of paleolimnological research to address issues of sediment flux and water quality change in the wetlands of the Murray-Darling Basin of Australia. This paper reports on the research outcomes on cores collected from sixteen wetlands along the Murrumbidgee-Murray River continuum. In all sixteen wetlands radiometric techniques and exotic pollen biomarkers were used to establish sedimentation rates from the collected cores. Fossil diatom assemblages were used to identify water source and quality changes to the wetlands. The sedimentation rates of all wetlands accelerated after European settlement, as little as two-fold, and as much as eighty times the mean rate through the Late Holocene. Some wetlands completely infilled through the Holocene, while others have rapidly progressed towards a terrestrial state due to accelerated accretion rates. Increasing wetland salinity and turbidity commenced within decades of settlement, contributing to sediment inputs. The sedimentation rate was observed to slow after river regulation in one wetland, but has accelerated recently in others. The complex history of flooding and drying, and wetland salinisation and eutrophication, influence the reliability of models used to establish recent, fine-resolution chronologies with confidence and the capacity to attribute causes to documented effects. © 2008 Elsevier B.V.
- Description: 2003006710
Seasonal and interannual variations in diatom assemblages in Murray River connected wetlands in north-west Victoria, Australia
- Gell, Peter, Sluiter, Ian, Fluin, Jenny
- Authors: Gell, Peter , Sluiter, Ian , Fluin, Jenny
- Date: 2002
- Type: Text , Journal article
- Relation: Marine and Freshwater Research Vol. 53, no. 6 (2002), p. 981-992
- Full Text:
- Description: Epipelic diatom assemblages collected from three wetlands connected to the Murray River displayed considerable variation in response to flooding and drying phases. Murray River water input usually generated diatom assemblages dominated by Aulacoseira species. After isolation, the diatom flora of two wetlands shifted to assemblages of small Fragilariaceae forms. Elevated nutrient levels corresponded with the appearance of eutraphentic taxa such as Cyclotella meneghiniana, Eolimna subminuscula, Luticola mutica and Nitzschia palea. Further evapoconcentration induced shifts to taxa tolerant of elevated salinity levels including Amphora coffeaeformis, Navicula incertata, Staurophora salina and Tryblionella hungarica. Ordination analyses reveal a strong chemical control on the diatom taxa present in the wetlands, in accordance with known ecological preferences for salinity and nutrients. The influence of nitrogen and phosphorus concentrations in controlling diatom assemblages was subordinate to salinity once conductivity values exceeded 1400 μS cm–1. The results of such biomonitoring provide a means of interpreting wetland history from fossil assemblages contained in sediment sequences.
- Authors: Gell, Peter , Sluiter, Ian , Fluin, Jenny
- Date: 2002
- Type: Text , Journal article
- Relation: Marine and Freshwater Research Vol. 53, no. 6 (2002), p. 981-992
- Full Text:
- Description: Epipelic diatom assemblages collected from three wetlands connected to the Murray River displayed considerable variation in response to flooding and drying phases. Murray River water input usually generated diatom assemblages dominated by Aulacoseira species. After isolation, the diatom flora of two wetlands shifted to assemblages of small Fragilariaceae forms. Elevated nutrient levels corresponded with the appearance of eutraphentic taxa such as Cyclotella meneghiniana, Eolimna subminuscula, Luticola mutica and Nitzschia palea. Further evapoconcentration induced shifts to taxa tolerant of elevated salinity levels including Amphora coffeaeformis, Navicula incertata, Staurophora salina and Tryblionella hungarica. Ordination analyses reveal a strong chemical control on the diatom taxa present in the wetlands, in accordance with known ecological preferences for salinity and nutrients. The influence of nitrogen and phosphorus concentrations in controlling diatom assemblages was subordinate to salinity once conductivity values exceeded 1400 μS cm–1. The results of such biomonitoring provide a means of interpreting wetland history from fossil assemblages contained in sediment sequences.
- Tibby, John, Gell, Peter, Fluin, Jenny, Sluiter, Ian
- Authors: Tibby, John , Gell, Peter , Fluin, Jenny , Sluiter, Ian
- Date: 2007
- Type: Text , Journal article
- Relation: Hydrobiologia Vol. 591, no. 1 (2007), p. 207-218
- Full Text:
- Description: Diatoms are among the most widely used indicators of human and climate induced wetland salinity history in the world. This is particularly as a result of the development of diatom-based models for inferring past salinity. These models have primarily been developed from relationships between diatoms and salinity measured at the time of sampling or during the preceding year. Although within site variation in salinity has the potential to reduce the efficacy of such models, its influence has been rarely considered. Hence, diatom-conductivity relationships in eight seasonally monitored wetlands have been investigated. In developing a diatom-conductivity transfer function from these sites, we sought to assess the influence of conductivity variation on diatom inference model performance. Our sites were characterised by variability in conductivity that was not correlated to its range and thus were well suited to an investigation of this type. We found, contrary to expectations, that short-term (seasonal) changes in conductivity which were often dramatic did not result in unduly reduced transfer function performance. By contrast, sites that were more variable in the medium term (5-6 years) tended to have larger model errors. In addition, we identified a secondary ecological gradient in the diatom data which could not be related to any measured variable (including pH, turbidity or nutrient concentrations).
- «
- ‹
- 1
- ›
- »