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Saltmarshes are highly valued habitats but the majority of the Eden Estuary's saltmarsh was buried under sea defences and ad hoc rubbish dumps during the last century. Without saltmarsh, the degraded shoreline may be even more vulnerable to rising sea levels and increased wave and tidal energy. This study investigated planting native saltmarsh species, common in the estuaries of Eastern Scotland, to restore saltmarsh development and sedimentation to the Eden Estuary's shoreline. The survival and growth of the sedge Bolboschoenus maritimus (Sea Club-rush) and the grasses Phragmites australis (Common Reed) and Puccinellia maritima (Common Saltmarsh Grass) were compared in planting trials. These were seeded or transplanted onto unvegetated upper mudflats in front of eroded P. maritima saltmarsh and a disused rubbish dump. The longer term sustainability of this practice was assessed by comparing sediment deposition and surface elevation in the transplant sites, natural saltmarsh and upper unvegetated mudflats. B. maritimus outperformed P. australis and P. maritima. Springtime, high density planting was successful, whereas seeds, planting in autumn and low density planting failed. Growth in the transplanted B. maritimus sites was relatively slow for the first three years but subsequently overtook growth of the seaward edge of natural B. maritimus marsh. Sediment was not deposited on natural P. maritima and was low on upper unvegetated mudflats and in young transplant sites. Most deposition occurred in four year old sites of B. maritimus. Sediment surface elevation in natural P. maritima remained constant throughout the year, but increased in all the other sites during the summer. The upper mudflat was the only site to erode during winter. A significant, positive association was found between tide height and sediment deposition, while winds from the south-east were associated with significantly more deposition than winds from the south-west. The direct planting of saltmarsh vegetation has restored a valuable and rapidly disappearing habitat to the degraded shoreline of the Eden Estuary. The low-cost and simplicity of this restoration practice give it great potential as a sustainable coastal management option that should be explored in other Scottish estuaries. This form of restoration could help to increase the resilience and reduce the vulnerability of degraded shorelines to climate change and rising sea levels.

Contemporary sediment transport, suspended sediment flux, rates of intertidal sedimentation, and Holocene sedimentation history are assessed for Hamford Water, a small meso-tidal inlet and saltmarsh embayment in Essex, UK. Sediment transport rates are calculated using semi-empirical equations; suspended sediment flux is computed by integration of suspended sediment concentration and velocity across the inlet throat; intertidal sedimentation rates are assessed from monitoring of discrete markers on saltmarsh and mudflat; and Holocene sedimentation is estimated from radiocarbon dating of buried organic layers, sampled using a vibrocorer. Results show a tidal regime typical of ebb-dominated inlets: moderate, ebb-dominant flow (==1 m S·l) in the central ebb channel is matched by similar flood-dominant marginal channel flows. The sediment dynamics are not influenced by any fluvial input; there is negligible fresh water input. The net direction of sediment transport is predominantly ebb-orientated. Coarse sand transport pathways are circulatory and dependent on longshore drift. Sand (D = 0.25 mm) enters at the margins and is expelled in the central ebb channel. Negligible sand is transported further landward than the mouth; intertidal sedimentation relies mainly on levels of suspended sediment. Rates of intertidal sedimentation are spatially variable: tidal creek sedimentation is greater than saltmarsh, with a mean rate of 4.2mm yr"l. Buried organic horizons. radiocarbon dated to 600 years BP, are attributed to reclaimed land levels. Holocene sedimentation rates since 4300 years BP, estimated from 14C dating of shell bands. accord with current estimates of sea-level rise of approximately 1 mm i 1 • The role and evolution of the inlet entrance and ebb tidal delta are seen as critical to the evolution of the embayment as a whole. The interaction of the embayment with the adjacent coastal zone considered essential when fonnulating shoreline management plans. Hamford Water is considered an integral part of the Stour/OrwelllNaze coastal system.

Saltmarsh is an important coastal habitat located in the littoral zone of estuaries. Australian saltmarsh area is decreasing due to agricultural and urban development and invasion by mangrove. The aim of the study was to assess the contribution made by saltmarsh as a habitat and a source of food items for fish. Three saltmarsh sites were studied, with Towra Point chosen as a site for detailed ecological study. When corrected for water volume, fish densities were found to be higher within the saltmarsh compared to the adjacent mangrove. Although the fish assemblages in saltmarshes differed significantly from mangroves the overall ratio between commercially and ecologically valuable species in these habitats are similar, a result suggesting the importance of temperate saltmarsh as habitat for economically important fish. Significant export of crab larva from saltmarsh (average crab larval abundance 2124.63 m-3 outgoing water) is a positive contribution to the estuarine food chain supplementing the nutritional requirements of estuarine fish. While the diet of the crabs producing this larvae seems dependant on the saltmarsh environment (given the contrasting isotopic signatures of Sesarma erythrodactyla in saltmarsh and mangrove, and the similarity of isotopic signatures in the saltmarsh for Sesarma erythrodactyla and Helograpsus haswellianus), the crabs do not seem to be dependent on any of the common species of saltmarsh plant, but rather depend on particulate organic matter (POM) derived from local and other sources. Crab larva are a prey item for many estuarine fish, including commercially important species, as evidenced by gut content analysis of fish visiting the saltmarsh flats during spring tides. The results strongly suggest that emphasis be given to ecosystembased management for an estuary rather than component (e.g., vegetation) based managed as defined by the Fisheries Management Act (1994) and the State Environmental Planning Policy 14.

Dissertação(mestrado) - Universidade Federal do Rio Grande, Programa de Pós–Graduação em Oceanografia Biológica, Instituto de Oceanografia, 2011. / Submitted by Cristiane Gomides (cristiane_gomides@hotmail.com) on 2013-12-16T13:10:23Z No. of bitstreams: 1 rubens.pdf: 37071078 bytes, checksum: e7a36c0d198f25aa295e0031caf953d7 (MD5) / Approved for entry into archive by Sabrina Andrade (sabrinabeatriz@ibest.com.br) on 2013-12-18T18:04:16Z (GMT) No. of bitstreams: 1 rubens.pdf: 37071078 bytes, checksum: e7a36c0d198f25aa295e0031caf953d7 (MD5) / Made available in DSpace on 2013-12-18T18:04:16Z (GMT). No. of bitstreams: 1 rubens.pdf: 37071078 bytes, checksum: e7a36c0d198f25aa295e0031caf953d7 (MD5) Previous issue date: 2011 / No estuário da Lagoa dos Patos são escassos os trabalhos sobre a comunidade fúngica. O objetivo deste estudo foi determinar a ocorrência de leveduras em duas áreas de marismas e os fatores abióticos que afetam sua distribuição espacial e temporal. O estudo foi realizado durante o inverno (Agosto) de 2009 e o verão (Fevereiro) de 2010 em duas enseadas rasas no estuário da Lagoa dos Patos, com diferentes níveis de eutrofização. As amostras foram coletadas em marismas dominadas por duas espécies macrófitas emersas: Juncus kraussii e Scirpus olneyi. Nos locais de coleta foram analisados os parâmetros abióticos e coletadas amostras de sedimento, água intersticial e de vegetação. Foi realizado o isolamento das leveduras do sedimento através de diluição em meio de cultivo. A identificação dos isolados foi feita através da análise de caracteres morfológicos e testes fenotípicos de metabolismo através do Sistema Vitek II. Foram isoladas 73 leveduras classificadas em 09 gêneros, com predominância de Ascomycotas. Entretanto, 10 destes isolados de leveduras não identificados e 02 isolados leveduriformes foram identificados como microalgas do gênero Prototheca. Dentre os gêneros de leveduras encontrados, houve uma predominância de leveduras do gênero Candida (n=20), seguidos por Rhodotorula (n=14), Yarrowia (n=07), Cryptococcus (n=06), Clavispora (n=04), Issatchenkia (n=03), Pichia (n=03), Torulaspora (n=03) e Kluyveromyces (n=01). O maior número de leveduras foi isolado em temperatura mais alta, no ambiente menos eutrofizado, em condições com maiores concentrações de nutrientes dissolvidos e no sedimento dominado por detrito de J. kraussii. / In the Patos Lagoon estuary few studies have been conducted on the fungal community. The aim of this study was to determine the occurrence of yeasts and the environments factors that affect their spatial and temporal distribution. The study was conducted during the winter (August) of 2009 and summer (February) 0f 2010 in two shallow bays of the Patos Lagoon estuary with different eutrophication level. The samples were collected in salt marsh areas dominated by two emerged macrophytes species: Juncus kraussii and Scirpus olneyi. Abiotic parameters were analyzed in the field and sediment samples, interstitial water and vegetation were collected. Yeasts were isolated from the sediment by dilution using the culture medium method. The identification of isolates was performed according to morphological characteristics and through metabolic tests using the Vitek II system. Seventy and three yeasts were isolated and classified in 09 genera with the predominance of Ascomycota. However, 10 of these isolated yeasts were unidentified and 02 yeast-like organisms, were identified as microalgae of the genera Prototheca. Among the identified genera of yeasts, there was a predominance of the genera Candida (n=20), followed by Rhodotorula (n=14), Yarrowia (n=07), Cryptococcus (n=06), Clavispora (n=04), Issatchenkia (n=03), Pichia (n=03), Torulaspora (n=03) e Kluyveromyces (n=01). Highest number of isolates was found in higher temperature, less polluted environment, in water with higher dissolved nutrient concentrations and in sediment dominated by detritus of Juncus kraussii. Key-words:

A detailed geochronological and geochemical study has been undertaken on selected sediment cores from four lowland coastal marsh environments in Argyll, Western Scotland. This region of northern Britain has experienced differential crustal uplift and relative sea-level changes throughout the Holocene in response to glacio-isostatic adjustment. The complex interplay between land movements and relative sea-level continues to influence the morphological development of the Scottish coast. The study of lowland inter-tidal sedimentary environments from this region provides an opportunity to investigate the linkages between current estimated crustal movements, regional relative sea-level rise and the evolution of contemporary coastal saltmarshes derived from the record of historical sedimentation. The four sites are located across a ca. 70 km transect extending from the head of Loch Scridain (western Isle of Mull), across the Firth of Lorne to the head of Loch Etive, (mainland Argyll). Vertical activity distributions of the natural radionuclide 21OPb and anthropogenic isotopes (137Cs and 243Am) have been measured and are used to assess the depositional history of marsh sediment accumulation recorded in the four marsh cores. Down-core activity profiles of radionuclides are only reliable as a means of modelling recent marsh evolution provided no early-diagenetic (redox) reactions have compromised the historical depositional record within the marsh sediments. Solid-phase major and trace element down-core geochemical distributions provide a means of assessing the extent to which post-depositional (redox) reactions may have influenced the reliability of the radiometric dating methods. Marsh sediment geochemistry also serves as a useful proxy for identifying compositional variability over the period of marsh development investigated. Dating of the Argyll saltmarsh cores indicates that over the period corresponding to mature marsh conditions rates of sedimentation vary significantly across the study area. At Loch Scridain an average rate of 1.1 mm yr-1 corresponding to an historical period of ca. 130 years is recorded. Comparison with estimated rates of regional sea-level rise suggest an established asymptotic relationship between marsh accretion and coastal forcing, implying historical crustal stability at this site. At sites within the Firth of Lome (Loch Don and Loch Creran) average rates of 2.5 and 3.3 mm yr-1 are recorded for the ca. 70 year period to 1995 with a figure of 2.2 mm yr-1 recorded in the marsh core from the head of Loch Etive. These values are well in excess of estimated relative sea-level rise during the twentieth century suggesting that these marshes may not yet have reached full equilibrium with sea-level. Microfossil analysis of the Loch Etive core helps to identify a more complex depositional history with an underlying trend of marine transgression for the ca. 110 year period of marsh development recorded in these sediments. Over the most recent period of marsh development (ca. 5 years) a significant increase in the rate of marsh sedimentation at all sites is recorded. This signifies the response of these marshes to a very recent increase in the rate of relative sea-level rise across the region. Comparison with available storm frequency data indicates that the evolution of these marsh environments have not been subject to the influence of significant storm activity over the last in the late Twetieth century. The findings suggest that the more clastic sedimentary composition of the Argyll marshes results in these inter-tidal areas being extremely sensitive to changes in coastal forcing (sea-level rise). The implications of recent relative sea-level rise, current vertical crustal movements and future coastal management are discussed.

Coastal wetland plants serve as ecological engineers in a physiologically stressful environment and the loss of coastal wetlands can cause negative effects throughout the estuarine system. Due to increased degradation of coastal habitats worldwide, interest in restoration has increased around the world. An understanding of the biotic processes affecting species distribution and diversity is critical for future conservation, management, and restoration of coastal wetlands. The purpose of my study was to test the effects of biotic interactions on native coastal wetland plants and determine how these interactions may be incorporated into current and future restoration projects. I had three primary goals for my dissertation. First, I evaluated the effectiveness of natural regeneration of coastal wetland communities following hydrological restoration. Second, I examined effects of biotic interactions between mangroves and other wetland species by experimentally testing: 1) trapping capabilities of early successional plant species on Rhizophora mangle propagules, 2) effects of pre-dispersal propagule damage on native mangrove species, 3) facilitative and competitive interactions between the plants Rhizophora mangle, Batis maritima, Sarcocornia perennis, and the fiddler crab, Uca pugilator using mesocosms. Third, I evaluated the combined effects of biotic and abiotic interactions on survival and growth of R. mangle propagules during their first year of establishment using a manipulative field experiment. Results from my study increase our knowledge of the importance of biotic interactions in coastal wetland communities, their role in early successional stages, and have direct applications to coastal wetland restoration and management.

Saltmarshes in SE England are eroding rapidly and one potential impact is the loss of habitat for fishes. Saltmarshes have been created by setting back the existing line of flood defence through managed realignment. The use by fishes of natural and managed realignment habitats at Tollesbury, Abbotts Hall and Orplands was examined (2005-07). Three seasonal groups were apparent in the fish assemblages of the managed realignment sites: February-April (Pomatoschistus microps and Sprattus sprattus), May-September (Dicentrarchus labrax and Atherina presbyter) and October-January (Liza aurata and Liza ramada). The sites were used mainly by 0- and 1-group fishes and adult P. microps. The mean abundance (July - August 2007) was 558 0.1 ha' (range 76 - 2699 0.1 ha'). In summer, small (< 30 mm) zooplanktivorous D. labrax fed successfully at all sites. Larger (30-59 mm) D. labrax consumed more macroinvertebrates in the Tollesbury managed realignment and two established marshes than at Abbotts Hall and Orplands. By autumn there were no site-specific differences in gut fullness of D. labrax. Stable isotope ratio analysis and gut contents analysis revealed that small (< 50 mm) D. labrax, S. sprattus and A. presbyter assimilated zooplankton which eat detritus, resuspended microphytobenthos and some phytoplankton. L. aurata assimilated zooplankton and microphytobenthos. P. microps (20-50 mm) and A. presbyter (80-99 mm) assimilated benthic meiofauna. Larger (50-230 mm) D. labrax assimilated macroinvertebrates which eat microphytobenthos, Ulva spp., C3 plants and detritus. Some recommendations for saltmarsh restoration are provided with an estimate of the economic value of bass in saltmarshes,to highlight further areas of research.