Dissertations / Theses on the topic 'Inter-tidal'

This thesis examines functional relationships between the morphologic, hydrodynamic, ecological and sedimentological characteristics of the Warraber reef platform, an inter-tidal reef island system, Central Torres Strait, Australia (10[degrees] 12??? S, 142 [degrees] 49??? E). Hydrodynamic and sediment-transport experiments were conducted on the reef flat using current meters, water level recorders and directional sediment traps. Results showed dominantly SE flows during the dry season and more variable NW to SE flows during the wet season. Topography and reefal water levels modulated the direction and strength of currents and the generation of wind-waves on the reef flat as well as the passage of waves over the reef rim. These hydrodynamic conditions are sufficient to induce significant transport of moderately fast to slow settling sediment (>-5.25 symbol psi) on the reef flat, though the platform as a whole is a relatively closed transport system. Carbonate production was estimated based on the key ecological variables of live assemblage distribution and cover. Overall, only 24% of the reef flat was occupied by carbonate-producing organisms. The average estimated carbonate-production rate for the reef was 1.6 kgm -2y-1 (0.07-4.37 kgm-2y-1). Production is dominated by coral (73%), with subordinate proportions contributed by coralline algae (19%). And molluscs, foraminifera and Halimeda (<4%) though actual reef-flat sediments did not reflect this potential. Instead, they were dominated by molluscs (35-55%), coralline algae (16-26%), coral (8-13%), Halimeda (7-8%) and foraminifera (5-10%). Differential rates of carbonate to sediment conversion meant the reef-platform sediments were more closely related to the cover of live organisms than to the contribution of carbonate production by each parent organism. The settling properties of the least altered particles of the five commonest constituents were measured and these provided the basis for an eco-sedimentological model of the reef-platform system. Modelled textures were compared to the actual textures, indicating the degree of textural alteration resulting from a combination of biological and physical processes, including sediment production, hydraulic sorting and mechanical breakdown. This analysis, integrated with the hydrodynamic, exposure and other data, was used to determine reef-platform surface-sediment sources, sinks and transport pathways. In using both the textual and constituent compositional properties of sediments, as well as information on local biological and physical processes, the model approach developed offers progress towards an integrative, interdisciplinary analysis of carbonate environments.

Integrated Coastal Zone Management (ICZM) depends on the recognition that benefits associated with healthy functioning (function benefits) of ecosystems are irreplaceable in ecological, geomorphological and social terms. A methodology for evaluating different inter-tidal wetlands on the basis of indicators representing their full range of functions is presented. Each inter-tidal wetland is attributed a function related score. These scores are region specific. Whilst they allow a ranking of inter-tidal wetland importance, they do not equate to economic value. A key advantage of this approach is that it quantifies the regional resource, and forms a basis upon which to consider the impact of future pressures and prioritise conservation actions. The methodology has been applied to the Solent and Poole Bay Marine Natural Area (MNA). The 13 inter-tidal wetlands within this region have been scored and ranked, highlighting the relative importance of the large inter-tidal wetlands of Poole, chichester and Langstone Harbours compared with the snmaller inter-tidal wetlands of the north shore of the Isle of Wight. The main challenges facing the conservation of this regional resource are evaluated and the cumulative impact/risk of key pressures is assessed. Lymington/Keyhaven and Southampton Water are considered to be the regional inter-tidal wetlands whose function benefits are most at risk over the next 20 years. A restoration target of 1200 ha of inter-tidal wetland is suggested for the MNA, with a recommendation that re-creation efforts should focus on Chichester Harbour. A detailed case study of the Lymington/Keyhaven inter-tidal wetland is presented. Technical rehabilitation solutions are suggested based on the synthesis of physical and ecological survey date. This research concludes that work to restore inter-tidal wetlands is urgently needed. Such work requires appropriate central Government funding together with a new mechanism, over and above existing compulstory purchase powers, to rationalize coastal landholdings. Investment should concentrate initially on the most easily rehabilitated and re-created sites, to offset the impact of natural forcing mechanisms associated with global environmental change. A role for environmental mediators in identified to raise the political and social acceptability of inter-tidal wetland restoration and a regional ecosystem-based approach is suggested as the best way forward

Swan Bay is a shallow marine embayment of Port Phillip Bay, just north of Queenscliff, Victoria. It has been part of the Harold Holt Marine Reserves since 1977 and is a seagrass habitat. This study investigated the species of fish present in the inter-tidal zone of Swan Bay, collected information on their ecology, investigated the importance of Swan Bay compared to Port Phillip Bay as a nursery and/or breeding area and compared these results with those of similar seagrsss habitats. Field work was carried out monthly over a two year period, from April 1981 to April 1983, using beach seine nets at Swan Bay and Portarlington. Forty four species of fish were identified from Swan Bay and nineteen from Portarlington. Fish were most abundant during the summer and autumn months when seagrass growth was at a maximum and least abundant during winter due to the absence of seasonal residents and decreased numbers of permanent residents. Swan Bay was found to be an important nursery ground for two commercially-caught species: the Yellow-eye Mullet and the King George Whiting. Juvenile Yellow-eye Mullet were more numerous in Swan Bay than at Portarlington. Smell juvenile King George Whiting were more abundant at Portarlington than in Swan Bay where older juveniles were more numerous. The fish fauna of Swan Bay was found to be similar to western Port but the abundance of species varied. Atherinosome microstoma was the dominant species in terms of abundance and biomass. Diet was found to be different from that reported by Robertson (1979) at Western Port due to the different range of prey items.

The cycling of arsenic in the marine photosynthetic plants and algae was examined by analysing total arsenic concentrations and arsenic species in selected marine photosynthetic organisms from the south-east coast, NSW, Australia. A range of elements required for metabolism in photosynthetic organisms were also analysed to determine if any relationship between these elements and arsenic concentrations occurred. Organisms were selected from salt marsh and mangrove ecosystems, marine inter-tidal and estuarine environments, and two species of marine phytoplankton cultured, to represent the different marine environments that primary producers inhabit. Organisms selected were compared to species within their own environment and then a comparison made between the varying ecosystems. In the salt marsh and mangrove ecosystems, the leaves of four species, the mangrove Avicennia marina, the samphire Sarcocornia quinqueflora, the seablight Suaeda australis, and the seagrass Posidonia australis were sampled from three locations from the south-east coast of NSW using nested sampling. Mean total arsenic concentrations (mean � sd) dry mass for all locations were A. marina (0.38 � 0.18 �g g-1 to 1.2 � 0.7 �g g-1), S. quinqueflora (0.13 � 0.06 �g g-1 to 0.46 � 0.22 �g g-1), S. australis (0.03 � 0.06 �g g-1 to 0.05 � 0.03 �g g-1)and P. australis (0.34 � 0.10 �g g-1 to 0.65 � 0.26 �g g-1). Arsenic concentrations were significantly different between species and locations but were consistently low compared to marine macroalgae species. Significant relationships between As and Fe concentrations for A. marina, S. quinqueflora and P. australis and negative relationship between As and Zn concentrations for S. quinqueflora could partially explain arsenic concentrations in these species. No relationship between As and P concentrations were found in this study. All terrestrial species contained predominantly inorganic arsenic in the water extractable and residue fractions with minor concentrations of DMA in the water-soluble fraction. P. australis also contained dimethylated glycerol and phosphate arsenoriboses. The presence of arsenobetaine, arsenocholine and trimethylated glycerol arsonioribose is most likely due to the presence of epiphytes on fronds on P. australis. In contrast, macroalgae contained higher total arsenic concentrations compared to marine terrestrial angiosperms. Total arsenic concentrations also varied between classes of algae: red macroalgae 4.3 �g g-1 to 24.7 �g g-1, green macroalgae 8.0 �g g-1 to 11.0 �g g-1 and blue green algae 10.4 �g g-1 and 18.4 �g g-1. No significant relations were found between As concentrations and concentrations of Fe, Co, Cu, Mn, Mo, Mg, P and Zn concentrations, elements that are required by macroalgae for photosynthesis and growth. Distinct differences between algal classes were found for the proportion of arsenic species present in the lipid and water-soluble fractions, with green algae having a higher proportion of As in lipids than red or estuarine algae. Acid hydrolysis of the lipid extract revealed DMA, glycerol arsenoribose and TMA based arsenolipids. Within water-soluble extracts, red and blue-green algae contained a greater proportion of arsenic as inorganic and simple methylated arsenic species compared to green algae, which contained predominantly glycerol arsenoribose. Arsenobetaine, arsenocholine and tetramethylarsonium was also present in water-soluble extracts but is not normally identified with macroalgae and is again likely due to the presence of attached epiphytes. Residue extracts contained predominantly inorganic arsenic, most likely associated with insoluble constituents of the cell. Mean arsenic concentrations in the green microalgae Dunaliella tertiolecta were 13.3 �g g-1 to 14.5 �g g-1, which is similar to arsenic concentrations found in green macroalgae in this study. Diatom Phaeodactylum tricornutum arsenic concentrations were 1.62 �g g-1 to 2.08 �g g-1. Varying the orthophosphate concentrations had little effect on arsenic uptake of microalgae. D. tertiolecta and P. tricornutum metabolised arsenic, forming simple methylated arsenic species and arsenic riboses. The ratio of phosphate to glycerol arsenoriboses was higher than that normally found in green macroalgae. The hydrolysed lipid fraction contained DMA arsenolipid (16-96%) with minor proportions of phosphate arsenoribose (4-23%). D. tertiolecta at f/10 phosphate concentration, however, contained glycerol arsenoribose and another arsenic lipid with similar retention as TMAO as well as DMA. The similarities between arsenic species in the water-soluble hydrolysed lipids and water-soluble extracts, especially for P. tricornutum, suggests that cells readily bind arsenic within lipids, either for membrane structure or storage, releasing arsenic species into the cytosol as degradation of lipids occurs. Inorganic arsenic was sequestered into insoluble components of the cell. Arsenic species present in D. tertiolecta at lower phosphate concentrations (f/10) were different to other phosphate concentrations (f/2, f/5), and require further investigation to determine whether this is a species-specific response as a result of phosphate deficiency. Although there are similarities in arsenic concentrations and arsenic species in marine photosynthetic organisms, it is evident that response to environmental concentrations of arsenic in uncontaminated environments is dependent on the mode of transfer from the environment, the influence of other elements in arsenic uptake and the ability of the organism to metabolise and sequester inorganic arsenic within the cell. It is not scientifically sound to generalise on arsenic metabolism in �marine plants� when species and the ecosystem in which they exist may influence the transformation of arsenic in higher marine organisms. There is no evidence to suggest that angiosperms produce AB as arsenic is mostly present as inorganic As, with little or no arsenic present in the lipids. However, marine macro- and microalgae both contain lipids with arsenic moieties that may be precursors for AB transformation. Specifically, the presence of TMA and dimethylated arsenoribose based arsenolipids both can transform to AB via intermediates previously identified in marine organisms. Further identification and characterization of As containing lipids is required.

Mergers are known to be essential in the formation of large scale structures and to have a significant role in the history of galaxy formation and evolution. Besides a morphological transformation, mergers induce important bursts of star formation. These starburst are characterised by high Star Formation Efficiencies (SFEs) and Specific Star Formation Rates, i.e., high Star Formation Rates (SFR) per unit of gas mass and high SFR per unit of stellar mass, respectively, compared to spiral galaxies. At all redshifts, starburst galaxies are outliers of the sequence of star-forming galaxies defined by spiral galaxies. We have investigated the origin of the starburst-mode of star formation, in three local interacting systems: Arp 245, Arp 105 and NGC7252. We combined high-resolution JVLA observations of the 21-cm line, tracing the Hi diffuse gas, with UV GALEX observations, tracing the young star-forming regions. We probe the local physical conditions of the Inter- Stellar Medium (ISM) for independent star-forming regions and explore the atomic-to-dense gas transformation in different environments. The SFR/H i ratio is found to be much higher in central regions, compared to outer regions, showing a higher dense gas fraction (or lower Hi gas fraction) in these regions. In the outer regions of the systems, i.e., the tidal tails, where the gas phase is mostly atomic, we find SFR/H i ratios higher than in standard Hi-dominated environments, i.e., outer discs of spiral galaxies and dwarf galaxies. Thus, our analysis reveals that the outer regions of mergers are characterised by high SFEs, compared to the standard mode of star formation. The observation of high dense gas fractions in interacting systems is consistent with the predictions of numerical simulations; it results from the increase of the gas turbulence during a merger. The merger is likely to affect the star-forming properties of the system at all spatial scales, from large scales, with a globally enhanced turbulence, to small scales, with possible modifications of the initial mass function. From a high-resolution numerical simulation of the major merger of two spiral galaxies, we analyse the effects of the galaxy interaction on the star forming properties of the ISM at the scale of star clusters. The increase of the gas turbulence is likely able to explain the formation of Super Star Clusters in the system. Our investigation of the SFR–H i relation in galaxy mergers will be complemented by highresolution Hi data for additional systems, and pushed to yet smaller spatial scales.

A habilidade de prever mudanças morfológicas nas regiões costeiras é restringida pela falta de dados observacionais com suficiente resolução espacial e temporal. Com o desenvolvimento do sensoriamento remoto, esse problema pode ser minimizado, especialmente com o uso de câmeras de vídeo para o estudo de regiões costeiras. Os objetivos dessa tese são, através do uso de imagens de vídeo, (1) desenvolver um método robusto para extrair a localização da linha de costa; (2) analisar um conjunto de dados inéditos de 26 anos de imagens diárias; (3) caracterizar as escalas espaciais e temporais da variação da linha de costa em um local representativo, a praia de Duck, NC; (4) testar esse método em uma praia reflectiva e com cúspides, a praia de Massaguaçu localizada no litoral brasileiro; (5) descrever recentes observações de feições morfológicas de meso-escalas associadas a um canal de marés usando uma técnica óptica inovadora e documentar as taxas e padrões de migração dessas feições morfológicas em New River Inlet, NC. Um modelo foi desenvolvido, chamado ASLIM (Augmented ShoreLine Intensity Maxima) para extrair as posições da linha de costa baseado na intensidade máxima observada nas imagens de exposição (timex) através de um ajuste Gaussiano com um subsequente filtro Kalman filtro, este para reduzir incertezas e ruídos. O ASLIM quando comparado com dados do levantamentos batimétricos mostrou um boa correlação com coeficiente de 0.85, estatisticamente significativo). As ondas foram caracterizadas em termos da altura significativa e os componentes longitudinal e transversal do fluxo de energia da onda (Px e Py, respectivamente). Menos de 2\\% da altura da onda é explicada por escalas maiores do que um ano. 66\\% da variância foi explicada por períodos maiores do que o ciclo anual, apesar do fato das forçantes (ondas) serem dominadas por períodos curtos (menores que 20 dias). O primeiro modo da EOF para a variação da linha de costa contém 49\\% da variância e representou o movimento transversal da linha de costa. O segundo modo (26\\% da variância) está associado com a alternância de sinais de acresção em cada lado píer, enquanto que os modos mais altos (7\\% e 5.6\\%) descrevem os efeitos locais do píer. O píer apresentou uma influência significativa no comportamento da linha de costa, à qual estende-se a 500 metros ao norte e sul do píer, duas vezes mais do que os valores assumidos por estudos anteriores. O píer restringe o transporte longitudinal sazonal entre a parte sul (verão) e a parte norte (inverno), resultando em uma acumulação de sedimentos sazonalmente reversa no lado up-drift da deriva. Sinais de erosão foram encontrados ao lado down-drift do píer e que propagam-se 1200 m/ano para longe do píer. A linha de costa apresentou uma tendência à erosão apenas no lado norte do píer, esta erosão pode estar relacionada com a tendência de aumento do transporte longitudinal para o norte, que é bloqueado devido ao píer, gerando uma acumulação na parte sul do píer e erosão na parte norte. O método ASLIM também foi testado na Praia de Massaguaçu e mostrou ser uma valiosa ferramenta para investigar variabilidade da linha de costa. Nossas observações em New River Inlet (NC), revelaram um complexo de bancos de espraiamento e feições arenosas de meso-escalas que migraram em um padrão coerente horário onde nas regiões offshore migraram em direção contrária a desembocadura do rio enquanto que as feições na região próxima a costa, migraram em direção ao canal. Para quantificar de forma objetiva as taxas e padrões de migração um algoritmo foi desenvolvido (LLSA - Lagged Least Square Algorithm) usando sequências de imagens de exposição (timex). Esse método compara diferentes imagens que possuem diferentes intervalos de tempo, e encontra o intervalo (lag) onde essas imagens são similares. A taxa média de migração encontrada foi de 1.53 m/dia (com desvio padrão de 0.76 m/dia). 72\\% das taxas estimadas foram maiores que 1.0 m/dia, 31\\% foram maiores que 2 m/dia, e as taxas máximas encontradas foram 3.5 m/day, em 23 dias. As taxas de migração média longitudinais mostraram um nó em 110 metros da linha de costa que separa as feições que migram para longe do canal (offshore) e para a linha de costa. O padrão circular pareceu ser consistente com o fluxo residual esperado em um delta de maré vazante. Em conclusão, nossos resultados mostraram que o uso de câmeras de vídeo são uma ótima ferramenta para fornecer informações sobre a dinâmica de morfologias costeiras com alta resolução temporal e espacial, de curto à longo-prazo.
The ability to predict changes of the coastal morphology has been restricted by the lack of observational data in a sufficient spatial and temporal coverage. With the advent of remote sensing, the low spatial and temporal resolution could be overcome, especially with the development of video cameras to study nearshore environments. The goals of this thesis are, using remote sensing techniques, to (1) develop a robust method for extracting shoreline locations; (2) analyze a unique 16 and 26-year record of daily to hourly video images; (3) characterize the space-time scales of shoreline variability at a representative site at Duck, NC; (4) test this method at a reflective and cuspy beach at Massaguaçu Beach located at Brazilian coast; (5) describe recent observations of meso-scales morphology associated with tidal inlets using an innovative optical method and document rates and patterns of migration of these features at New River Inlet, NC. A model was developed, called ASLIM (Augmented ShoreLine Intensity Maxima) to extract the shoreline positions based on fitting the band of high light intensity in time exposure images to a local Gaussian fit with a subsequent Kalman filter to reduce noise and uncertainty. The ASLIM model showed good agreement with survey data (correlation coefficient of 0.85, significant at 95\\% confidence level). Wave forcing was characterized in terms of the significant wave height and the cross-shore and longshore components of wave energy flux. 66\\% of the shoreline variability was explained by periods longer than the annual cycle, despite the fact that wave forcing is dominated by shorter periods. The first EOF mode of shoreline variability contained 49\\% of the variance and represented the cross-shore movement (landward- seaward) of the shoreline. The second mode (26\\% of the variance) is associated with alternating accretion signals on either side of the pier, while the next two higher EOFs (7\\% and 5.6\\%) describe the local pier effects. The pier was found to have a significant influence on shoreline behavior that extends out to 500 meters, nearly twice the length scales assumed by previous studies. The pier restricts seasonal longshore transport from the south (summer) and north (winter) sides, resulting in a seasonally-reversing sediment accumulation on the up-drift side. Erosion signals on the down-drift side of the pier were found propagate away from the pier at 1200 m/year. A shoreline erosion trend that was found only on the north side of the pier may be related to the trend found in the alongshore transport, that it is increasing toward the north and is being blocked by the pier. The ASLIM method was also tested at Massaguaçu Beach and showed to be a valuable tool to investigate shoreline variability processes. Our observations, at New Rivet Inlet (NC), revealed a complex set of swash bars and meso-scale sand banks that migrated in a coherent clockwise pattern with movement in offshore regions being away from the inlet mouth while nearshore migration was back toward the inlet. To quantify migration rates and patterns objectively based on sequences of time exposure images, a Lagged Least Squares Algorithm (LLSA) was developed that found the vector migration rate for which the suite of lagged images were most similar, computed on a tile-by-tile basis. The mean migration rate was found to be 1.53 m/day (standard deviation of 0.76 m/day). 72\\% percent of estimated rates were greater than 1.0 m/day, 31\\% percent were larger than 2.0 m/day, and the maximum rate round was 3.5 m/day, averaged over 23 days. Alongshore averages of cross-shore migration rates showed a node at 110 m from the shoreline that separates migration away from the inlet (offshore) from migration toward the inlet near the shore. The circular pattern of migration appeared to be consistent with expected residual flow on an ebb delta. In conclusion, our results showed that the use of video cameras are a useful tool for providing information about the dynamics of coastal morphologies with a high temporal and spatial resolution, from short to long-term.

Este estudo visa à descrição pontual do comportamento hidrodinâmico do estuário do Rio Mearim, analisando os padrões de corrente de maré, do registro de marés e das possíveis relações entre eles. Durante novembro e dezembro de 2012 um ADCP foi fundeado no canal do estuário, onde coletou dados por 31 dias. Os dados foram qualificados e processados para futura análise e inter-relações. Foi observado que a coluna de água estuarina no ponto de medição move-se como uma coluna de água homogênea com fluxo bidirecional no eixo NE-SW. As medições ocorreram no período de baixo índice de pluviosidade. O espectro de energia de velocidade de correntes indicou contribuições parciais dos harmônicos M2, M4, M6 e M8 no padrão de correntes encontrados. Defasagens no tempo entre os picos de máxima velocidade de corrente durante enchente e vazante mostraram a dominância do processo de maré vazante sobre a enchente no estuário. A análise integrada apresentada permitiu uma melhor compreensão no entendimento do comportamento das correntes forçadas pela maré, as chamadas correntes de maré, no estuário do Rio Mearim.
This study aim to describe the punctual hydrodynamic behavior of Mearim River estuary, analyzing the pattern of the tidal current, the tidal data and possible relationship between them. During 2012 november and december an ADCP was deployed in the estuary channel, where it collected data for 31 days. The data were qualified and processed for further analysis and inter-comparisons. It was observed the estuarine water column in the point of deployment moved as a homogeneous water column with bidirectional flux in axis NE-SW. The deployment was made in a period of low pluviosity index. The energy spectrum of current velocity indicated partial contribution of harmonics M2, M4, M6 e M8 in the current pattern found. Delays between the maximum velocity during flood and ebb conditions, showed the dominance of the edd process over the flood in the estuary. An analysis integrated presented on this paper allowed a better understanding of the behavior of the current forced by tides, called the tidal current in the Mearim River estuary.

Text in English with abstracts in English, Afrikaans and isiXhosa
This thesis describes the development of a methodology to find inter tidal shipwrecks. The discussion revolves around finding a particular shipwreck – that of the Dutch slaver Meermin. The story of the revolt on the Meermin helps to focus the search and development of the methodology to find inter tidal shipwrecks as the Meermin was wrecked in this zone. The thesis contextualises the search and the story by discussing not only maritime archaeology in South Africa, but also looking at slave ship archaeology and the history of slavery at the Cape. One of the key techniques for finding shipwrecks is the use of magnetometers. The discussion defines the types of magnetometers available to archaeologists and how magnetometry was applied during the search for the Meermin. This inevitably includes an examination of the shipwrecks wrecked in the area of the Meermin episode as well as the way this region has changed over time. The results of the magnetometer searches (which included airborne, handheld and marine magnetometers) are discussed as well as the ground truthing of the results. The latter involved excavation and the development of excavation strategies, and excavation results are scrutinized. In the final analysis the search for the Meermin is further contextualised by considering the various impacts the project has had in other spheres.
Hierdie tesis beskryf die ontwikkeling van ‘n metodologie waarmee skeepswrakke in die inter-gety sone opgespoor kan word. Die Hollandse slaweskip, Meermin, is die fokus van die diskussie. Die storie van die slawe opstand op die Meermin help om die ontwikkeling en soektog na skeepswrakke in die inter-gety sone te verskerp, aangesien dit in hierdie sone was waarin die Meermin gestrand het. Die soektog en storie van die Meermin word gekontekstualiseer deur die bespreking van die ontwikkeling van maritieme argeologie in Suid Afrika, die argeologie van slawe skepe en ‘n kort geskiedenis van slawerny aan die Kaap. Magnetometers is een van die belangrikste tegnieke gebruik vir die opspoor van skeepswrakke. Die tipes magnetometers wat deur argeoloë gebruik word, word gedefinieër asook hoe magnetometers gedurende die soektog na die Meermin gebruik is. Daar word ook gekyk na die ander skepe wat in die area van die Meermin gestrand het en die veranderinge wat deur die jare in die streek plaasgevind het. Die resultate van die magnetometer soektogte (insluitend vliegtuig, draagbare en mariene magnetometers) word bespreek so wel as die opgrawings van die resultate. Hierdie opgrawings het noodwendig gelei tot die ontwikkeling van opgrawings tegnieke. Die resultate van die opgrawings word bespreek. Die finale analise kontekstualiseer die soektog na die Meermin met ‘n bepeinsing van die menige impakte wat die projek gehad het.
Le thisisi icacisa ngenkqubela kulwazi-nkqubo lokufumana iinqanawa ezaphuka phakathi kokuzala nokurhoxa kolwandle. Ingxoxo zimalunga nokufunyanwa kwenqanawa ethile eyaphukayo – kanye leyo yayithutha amakhoboka amaHolani i-Meermin. Ibali lovukelo kwi-Meermin liyasinceda siqwalasele uphando nenkqubela kulwazi-nkqubo lokufumana iinqanawa ezaphuka phakathi kokuzala nokurhoxa kolwandle njengoko i-Meermin yaqhekeka kanye kulo mmandla. Ithisisi le isicacisela kanye ngophando nembali ngokuxoxa hayi ngobunzululwazi ngezakudala emanzini eMzantsi Afrika nje kuphela, koko iphinde ijonge ngobunzululwazi ngezakudala kwinqanawa yokuthutha amakhoboka nembali yobukhoboka eKapa. Obunye bobuqili obuphambili ekufumaneni iinqanawa eziqhekekileyo kukusetyenziswa kwezixhobo zokulinganisa iintshukumo. Ingxoxo ibalula iindidi zezixhobo zokulinganisa iintshukumo ezisetyenziswa ziinzululwazi ngezakudala nendlela ekwasetyenziswa ngayo ukulinganiswa kwentshukumo ngethuba kuphandwa i-Meermin. Ngokuqhelekileyo oku kuquka ukucutyungulwa kweenqanawa ezaqhekekayo ziqhekeka kummandla wesehlo esisodwa se-Meermin kunye nendlela le ngingqi eguquke ngayo emveni koko. Iziphumo zophando ngezixhobo zokulinganisa iintshukumo (ziquka ezo zasesibhakabhakeni, ezibanjwa ngesandla nezasemanzini) ziyaxoxwa kunye neziphumo zenyani yenene. Le yokugqibela iquka ukwembiwa nenkqubela kwindlela zokomba, iziphumo zokomba nazo ziqwalaselwe. Kuye kwaphinda kwacaciswa kwintlahlela yokugqibela kuphando lwe-Meermin kuqwalaselwa iimpembelelo ezithile umsebenzi othe wangquzulena nazo nakwezinye iindawo.
Anthropology and Archaeology
M.A. (Archaeology)

碩士
國立臺灣海洋大學
教育研究所
103
In this study, researcher teaches sixth grade students for the study, using a three-stage learning cycle teaching model development “intertidal ecological conservation program,” and for a period of about two months, a total of sixteen sections of teaching. During the study, through learning single, student interviews, teaching reflection notes, Coordinating teacher observations, expert seminars and other research tools, to enhance the understanding of the situation between the sixth grade three students intertidal ecological conservation concepts. Researchers investigate the students through the intertidal growth scenario with the concept of ecological conservation. The results are shown below: First, curriculum design of a three-stage learning cycle: 1. Using multiple mediums to promote students' motivation to explore. 2. In Term Introduction, curriculum combining with students’ life experiences will be easy to reach learning outcomes. 3. In Concept Application, teacher provides multi-problem situations and multi-reflection can promote application of the concept. Second, student learning: 1. Students learn the intertidal zone between ecological conservation knowledge. 2. Students understand the problems facing the intertidal zone of ecological conservation. 3. Students establish the correct values and implement actions to maintain the intertidal environment. The results of this study will provide marine ecological conservation program developers, researchers, related units of promoting marine education and teachers as a reference. Key word: marine education, intertidal zone ecological conservation, learning cycle, action research