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  • 1
    Online Resource
    Online Resource
    Oxford :Taylor & Francis Group,
    Keywords: Coastal ecology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (361 pages)
    Edition: 1st ed.
    ISBN: 9781317859314
    DDC: 574.5/2638
    Language: English
    Note: Cover -- Half Title -- Dedication -- Title Page -- Copyright Page -- Table of Contents -- Acknowledgements -- Chapter 1 The coastal context -- What are coastal problems? -- The coastal zone: some fundamental characteristics and principles -- Coastal biogeomorphology -- Coastal use and management -- Approaches to the study and solution of coastal problems -- Types of coastal problem -- How this book is structured -- Chapter 2 How coasts work -- Introduction -- Plate tectonics and coastal type -- The coastal setting: Late Quaternary sea level changes -- Wave processes in the shore zone -- The influence of tides -- Coastal ecology -- Water on land at the coast: seaspray, fluvial inputs and groundwater -- Physical disturbances to coastal biogeomorphology: storm surges and large scale pressure changes -- Global warming, sea level rise and the coastal future -- Chapter 3 Sandy coastlines: beaches and dunes -- Introduction -- Beaches -- Dunes -- Beach-dune interactions -- What problems affect sandy coastlines? -- Dune management -- Barrier islands -- Case study 3.1: Erosion problems along the barrier beach coasts of Nigeria -- Case study 3.2: Dunes of the Dutch coast -- Chapter 4 Rocky coasts: cliffs and platforms -- Introduction -- Distribution and nature of rocky coasts -- Hard rock cliffs -- Cliffs prone to failure -- Shore platforms -- Human influences on rocky coasts -- Meeting the challenges on rocky coasts -- Case study 4.1: Llantwit Major - blasted cliffs! -- Case study 4.2: Jump-Off Joe: building on a disaster -- Chapter 5 Coastal wetlands -- Introduction -- The magic of mud -- Environmental settings of coastal wetlands -- Types of coastal wetland -- Sea level rise and wetland growth and destruction -- Problems affecting coastal wetlands - upsetting the balance -- Future sea level rise - towards a new balance?. , Balancing the possibilities - effective coastal wetland management -- Case study 5.1: The disappearing wetlands of south Louisiana, USA -- Case study 5.2: War and the mangroves of Vietnam -- Chapter 6 Coral reefs -- Introduction -- The biological scale: calcification, coral growth and reef accretion -- The geological scale: reef construction, destruction and net accretion -- The coral reef community -- Corals and temperature -- 'Phase shifts' between hard and soft shallow water communities -- Coral reefs and environmental degradation -- Reef robustness and fragility: a few concluding remarks -- Case study 6.1: Kanehoe Bay, Hawaii -- Case study 6.2: The crown-of-thorns starfish: a highly complex biological phenomenon -- Chapter 7 Cold coasts: permafrost, glaciers, sea ice and fjords -- Introduction -- Ice at the coast -- Types of cold coast -- Geomorphic change and ecology of cold coasts -- Human impacts on cold coasts -- Overview -- Case Study 7.1: The Exxon Valdez oil spill, Alaska: catastrophe or not? -- Case study 7.2: The Antarctic coast: exploitation or conservation? -- Chapter 8 Managing the coast: coping with coastal problems -- Managing the coastal zone - regaining a holistic perspective on coastal problems -- Human influences on the coast -- Sustainable coastal zone use and management -- The coast of Bangladesh, Bay of Bengal -- The Mediterranean Sea -- Conclusions -- Reference -- Index.
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  • 2
    Online Resource
    Online Resource
    Milton :Taylor & Francis Group,
    Keywords: Geomorphology-Tropics. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (399 pages)
    Edition: 1st ed.
    ISBN: 9780429553646
    Series Statement: Routledge Library Editions: Geology Series ; v.7
    DDC: 551.40913
    Language: English
    Note: Cover page -- Halftitle page -- Title page -- Copyright page -- Title page -- Copyright page -- Dedication -- Preface -- Acknowledgements -- Contents -- List of tables -- List of contributors -- Part A INTRODUCTION -- 1 The history of geomorphology in low latitudes -- 2 The significance of environmental change: diversity, disturbance and tropical ecosystems -- 2.1 Introduction -- 2.2 Rainforest structure and change -- 2.3 Coral reef response to environmental stress -- 2.4 Variability in extreme events -- 2.5 The temporal and spatial distribution of hurricanes and tropical cyclones in the Caribbean basin -- Part Β ENVIRONMENT AND PROCESS -- Process and time -- 3 Present-day processes as a ke yto the effects of environmental change -- 3.1 Introduction -- 3.2 Nutrient cycling in tropical forests -- 3.3 Movement of water in tropical rainforest -- 3.4 Sediment and solute transport -- 3.5 Specific environments: New Guinea and Malaysia -- 3.6 Response of geomorphic processes to environmental change -- 4 Aspects of present-day processes of in the seasonally wet Tropics of West Africa -- 4.1 Introduction -- 4.2 Morphoclimatic conditions -- 4.3 Processes and their effects on slopes -- 4.4 Fluvial processes -- 5 The influence of climate, lithology and time on drainage density and relief development in the tropical volcanic terrain of the Windward Islands -- 5.1 Introduction -- 5.2 Measurement of drainage density and relief development -- 5.3 Analysis and interpretation of drainage density -- 5.4 Factors affecting drainage density and relief evolution -- 5.5 Conclusions -- 6 Surface and underground fluvial activity in the Gunung Mulu National Park, Sarawak -- 6.1 Introduction -- 6.2 The study area -- 6.3 The development of the regional and limestone drainage -- 6.4 The clastic cave sediments -- 6.5 Fluvial terraces -- 6.6 Discussion -- 6.7 Conclusions. , Part C ENVIRONMENTAL CHANGE -- Evidence for environmental change -- 7 Relevance of Quaternary palynology to geomorphology in the tropics and subtropics -- 8 Geomorphic implications of late Quaternary hydrological and climatic changes in the Northern Hemisphere tropics -- 8.1 Introduction -- 8.2 The water balance of closed lakes -- 8.3 Methods used in this study -- 8.4 Fluctuations in lake level in Africa and Arabia -- 8.5 Variations in moisture conditions in Central America -- 8.6 Geomorphic implications -- 9 Evidence from lake sediments for recent erosion rates in the highlands of Papua New Guinea -- 9.1 Introduction -- 9.2 Aims and requirements -- 9.3 Previous results -- 9.4 Erosion rates -- 9.5 Sediment sources -- 9.6 Conclusions and prospects -- 10 Evidence of Upper Pleistocene dry climates in northern South America -- 10.1 Introduction -- 10.2 Evidence of climatic change in central Amazonia -- 10.3 Climatic changes on and around the margins of Amazonia -- 10.4 Conclusion -- 11 Pleistocene aridity in tropical Africa, Australia and Asia -- 11.1 The humid tropics: stable or dynamic? -- 11.2 The duration and amplitude of the Quaternary climatic fluctuations -- 11.3 Intertropical ice-age aridity -- 11.4 The evidence of Quaternary climatic change -- 11.5 The late Quaternary climates -- 11.6 Future palaeoclimatic research in the tropics -- Part D LANDFORM EVOLUTION -- Tectonic style and tropical landforms -- 12 Environmental change and episodic etchplanation in the humid tropics of Sierra Leone: the Koidu etchplain -- 12.1 Introduction -- 12.2 Geological and geomorphological background -- 12.3 Landform elements and deposits -- 12.4 Episodic etchplanation and environmental change -- 12.5 Continuous versus episodic etchplanation -- 12.6 Some questions of geomorphic theory -- 13 A provisional world map of duricrust -- 13.1 Introduction. , 13.2 Critical review of previous work -- 13.3 Mapping of the duricrusted areas at the 1:20 000 000 scale -- 13.4 Conclusion -- 14 Tectonic background to long-term landform development in tropical Africa -- 14.1 Introduction -- 14.2 Domal uplifts and rift systems -- 14.3 Mechanisms of uplift and rifting -- 14.4 Morphotectonics of continental margin development -- 14.5 Some more general implications -- 14.6 Conclusions -- 15 Soil and slope development in the wet zone of Sri Lanka -- 15.1 Introduction -- 15.2 Steep slopes and caves -- 15.3 Moderate slopes and regolith -- 15.4 Shallow slopes -- 15.5 Slope development -- 15.6 Conclusion -- 16 Relief generation and soil in the dry zone of Sri Lanka -- 16.1 Climatic characteristics -- 16.2 Geological overview -- 16.3 The oldest relief generations -- 16.4 Landform development in the Upper Tertiary -- 16.5 The youngest planation surface -- 16.6 Fossil sediments and palaeosols and their implications for landform evolution -- 16.7 Discussion -- Part E CONCLUSION -- 17 Findings, answers to questions and implications for the future -- 17.1 Typical tropical landforms -- 17.2 The effects of climatic contrasts on geomorphic processes -- 17.3 The role of plate tectonics and other tectonic events -- 17.4 Parallel sequences of landform evolution in different continents -- 17.5 The effect of sea-level changes -- 17.6 Ecosystem dynamics and landform development -- 17.7 Geomorphic events and scales of change -- References and bibliography -- Index.
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  • 3
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    PANGAEA
    In:  Supplement to: Möller, Iris; Kudella, Matthias; Rupprecht, Franziska; Spencer, Tom; Paul, Maike; van Wesenbeeck, Bregje K; Wolters, Guido; Jensen, Kai; Bouma, Tjeerd J; Miranda-Lange, Martin; Schimmels, Stefan (2014): Wave attenuation over coastal salt marshes under storm surge conditions. Nature Geoscience, 7(10), 727-731, https://doi.org/10.1038/ngeo2251
    Publication Date: 2023-01-13
    Description: Coastal communities around the world face increasing risk from flooding as a result of rising sea level, increasing storminess, and land subsidence. Salt marshes can act as natural buffer zones, providing protection from waves during storms. However, the effectiveness of marshes in protecting the coastline during extreme events when water levels and waves are highest is poorly understood. Here, we experimentally assess wave dissipation under storm surge conditions in a 300-m-long wave flume that contains a transplanted section of natural salt marsh. We find that the presence of marsh vegetation causes considerable wave attenuation, even when water levels and waves are high. From a comparison with experiments without vegetation, we estimate that up to 60% of observed wave reduction is attributed to vegetation. We also find that although waves progressively flatten and break vegetation stems and thereby reduce dissipation, the marsh substrate remained remarkably stable and resistant to surface erosion under all conditions.The effectiveness of storm wave dissipation and the resilience of tidal marshes even at extreme conditions suggest that salt marsh ecosystems can be a valuable component of coastal protection schemes.
    Keywords: File content; File name; File size; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 4
    Publication Date: 2024-04-20
    Description: The excel document contains three tabs: README - provides column descriptions for the remaining two tabs. RawData - Eighteen unique profiles were modelled, with ten runs per profile, for two scenarios: morphological updating enabled, and then disabled. This results in a dataset comprising 360 individual model runs. Each row represents one run as is described in the README tab. Statistics - Calculates the average overtopping discharge (with and without morphological change) for each representative profile. The methodology used to generate this data set is described in: Pollard et al. (2021).
    Keywords: Blakeney_Pt; England; Gravel barrier morphology; Storm surge modelling; XBeachG
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 44.4 kBytes
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  • 5
    Publication Date: 2024-04-20
    Description: This dataset comprises measurements of particle size distribution, peak shear strength, residual shear strength and compressibility from two salt marshes in the UK. It also provides information on the angle of internal friction and the strength attributed to cohesion at each measurement location. The salt marshes chosen were Warton marsh, North West England and Tillingham Marsh, South East England. Undisturbed samples were taken for the shear box, ring shear and oedometer tests. Three sampling sites at each marsh were chosen for undisturbed samples: tidal flat (0-30 cm depth below the surface), marsh edge (0-30 cm and 30-60 cm depth below the surface). Bulk samples were taken from four sites within the marsh: the tidal flat, marsh edge, creek edge and inner marsh. Bulk samples were taken for root mass and particle size analysis at 0-10 cm, 10-20 cm and 20-30 cm at each of these locations, with additional samples at 30-40 cm, 40-50 cm and 50-60 cm at the marsh edge location. Field sampling and measurements were undertaken on 17th-19th July 2017 and 28th September-1st October 2017 at Tillingham and 6th-10th July 2018 at Warton.
    Keywords: Dengie Peninsula; Morecambe Bay; MULT; Multiple investigations; nature-based solutions; oedometer; ring shear; Saltmarsh; shear box; Tidal wetlands; Tillingham_Creek; Tillingham_Inner; Tillingham_Marsh_Edge; Tillingham_Tidal_Flat; United Kingdom; Warton_Creek; Warton_Inner; Warton_Marsh_Edge; Warton_Tidal_Flat
    Type: Dataset
    Format: application/zip, 154.7 kBytes
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  • 6
    Publication Date: 2024-04-20
    Description: This dataset comprises measurements of substrate composition (water content, organic content, carbonate content, particle size, particle density, root mass content), erodibility (Cohesive Strength Meter; CSM) and undrained shear strength (vane) from two salt marshes in the UK. The salt marshes chosen were Warton marsh, North West England and Tillingham Marsh, South East England. Four sampling sites at each marsh were chosen: tidal flat, marsh edge, creek edge and inner marsh. Samples were taken for compositional analysis at 0-10 cm, 10-20 cm and 20-30 cm at each location, with additional samples at 30-40 cm, 40-50 cm and 50-60 cm at the marsh edge location. The same sampling strategy was used for the CSM, shear vane and torvane measurements, but these could only be sampled until the water table was reached. Shear vane measurements began at 10 cm depth below the surface, as the vane paddles reached 10cm below the surface at their lowest point. At each sampling location, three replicate CSM measurements were taken, ten replicate shear vane measurements, and ten replicate torvane measurements. Samples were taken between 29th September and 1st October 2017 at Tillingham and 6th and 10th July 2018 at Warton. CSM and vane analyses were undertaken on 15th-16th October and 29th November 2018 at Tillingham, and 18th-20th October 2018 at Warton.
    Keywords: Cohesive Strength Meter (CSM); erodibility; MULT; Multiple investigations; sediment composition; stability; Tillingham_Creek; Tillingham_Inner; Tillingham_Marsh_Edge; Tillingham_Tidal_Flat; United Kingdom; vane shear testing; Warton_Creek; Warton_Inner; Warton_Marsh_Edge; Warton_Tidal_Flat; wetlands
    Type: Dataset
    Format: application/zip, 28.8 kBytes
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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 370 (1994), S. 338-339 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] JUST as huge areas of the Earth, such as the 165 million km2 of the Pacific Ocean, are usually squeezed into the last page of an atlas, so island geology, geomorphol-ogy and, to a lesser extent, biogeography rarely take scientific centre stage. Yet islands have a strong intellectual pedigree (one ...
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Coral reefs 4 (1985), S. 59-70 
    ISSN: 1432-0975
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract Direct measurements of surface lowering, using the micro-erosion meter technique, have been obtained from Pleistocene and Tertiary limestones in subtidal and intertidal environments on Grand Cayman Island, West Indies. Overall, erosion rates averaged 0.99 mm yr-1; however this figure conceals the fact that the mean erosion rate on open coasts (X=2.77 mm yr−1) was over six times greater than the rate on reef-protected shores (X=0.45 mm yr−1). On lagoonal rocky coasts abrasion and biological action appear to be the dominant erosional processes, but on coasts exposed to high wave surf, bioconstruction dominates over bio-erosion and surface erosion is slight (X=0.17 mm yr−1). Thus, the magnitude and relative importance of physical, chemical and biological erosion processes differ from one locality to the next with variations in coastal exposure and between reef areas with changes in tidal range and wave regime.
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2021-05-19
    Description: There are 74 coralline islands in the Southern Seychelles, from which representative reefs have been selected for this report, comprising an atoll (Alphonse), a raised platform island (St Pierre), a carbonate bank (Providence-Cerf) and a drowned atoll (Cöetivy) (Figure 1). Aldabra Atoll is treated in a separate section in this publication (see Teleki et al., this volume). Qualitative observations of reef morphology, coral community composition and reef health in the southern Seychelles were made between March and May 1998 (Southern Seychelles Atoll Research Programme - SSARP), February and March 1999 (Thalassi/Shoals of Capricorn Expedition) and November 1999 (Aldabra Marine Programme – AMP). These observations were supplemented by quantitative descriptions of coral communities at 48 sites at four study locations. Twenty-five meter long transects were set out at water depths, where possible, of 5 m, 10 m, 15 m and 20 m. Transects were surveyed using both a line point intercept method and digital videographic imagery which was subsequently analysed using point sampling to generate estimates of benthic cover. Digital stills of individual coral species were obtained from each site for taxonomic inventory purposes.
    Keywords: Coral reefs
    Repository Name: AquaDocs
    Type: Preprint
    Format: 153077 bytes
    Format: application/pdf
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  • 10
    Publication Date: 2022-01-07
    Description: Development of a prototype data-driven modelling and visualisation tool to be tested with selected stakeholders. The prototype will be used to create a roadmap for visualising data leading to better coastal resilience decisions in the management of future sea level rise. The deliverable will include a brief report.
    Type: Report , NonPeerReviewed , info:eu-repo/semantics/book
    Format: text
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