A geological record of multiple Pleistocene tsunami inundations in an oceanic island: The case of Maio,Cape Verde     

José Madeira  Ricardo S. Ramalho  Dirk L. Hoffmann  João Mata  Mário Moreira 《Sedimentology》2020,67(3):1529-1552

In the Central Atlantic archipelagos – the Canaries, Cape Verde, Madeira and the Azores – tsunami hazard is often regarded as low, when compared with other extreme wave events such as hurricanes and storms. The geological record of many of these islands, however, suggests that tsunami hazard may be underestimated, notwithstanding being lower than in areas adjacent to subduction zones, such as the margins of the Pacific and Indian oceans. Moreover, tsunamis in oceanic islands are generally triggered by local large-scale volcanic flank collapses, for which little is known about their frequency, making it difficult to estimate the probability of a new occurrence. Part of the problem lies in the fact that tsunami deposits are usually difficult to date, and few islands in the world exhibit evidence for repeated tsunami inundation on a protracted timescale. This study reports on the presence of abundant tsunami deposits (conglomerates and sandstones) on Maio Island (Cape Verde) and discusses their stratigraphy, sedimentological characteristics, probable age and tsunamigenic source. Observations indicate that four distinct inundation events of variable magnitude took place during the Pleistocene. One of the tsunami deposits yielded a high-confidence U/Th age of 78·8 ± 0·9 ka, which overlaps within error with the 73 ± 7 ka age proposed for Fogo volcano's flank collapse, an event known to have had a significant tsunami impact on nearby Santiago Island. This shows that the Fogo tsunami also impacted Maio, resulting in runups in excess of 60 m above coeval sea-level at ca 120 km from the source. Two older deposits, possibly linked to recurrent flank collapses of the Tope de Coroa volcano in Santo Antão Island, yielded lower-confidence ages of 479 to 390 ka and 360 to 304 ka. A younger deposit (<78 ka) remains undated. In summary, the geological record of Maio exhibits well-preserved evidence of repeated tsunami inundation, reinforcing the notion that tsunami hazard is not so low at volcanic archipelagos featuring prominent and highly-active volcanoes such as in Cape Verde.  相似文献   

Bifurcation current along the southwest coast of the Kii Peninsula   总被引：1，自引：0，他引：1  

Junichi Takeuchi  Naoto Honda  Yoshitaka Morikawa  Takashi Koike  Yutaka Nagata 《Journal of Oceanography》1998,54(1):45-52

Along the southwest coast of the Kii Peninsula, a bifurcation current is regularly observed. By using ADCP data taken on board the R/V Wakayama of the Wakayama Prefectural Fisheries Experimental Station, characteristics of this bifurcation current are analyzed. The occurrence frequency of the bifurcation current reaches about 70% in the period from 1988 to 1996. The bifurcation point appears to be changeable and occurs almost evenly between Cape Ichie and Cape Shionomisaki. The current divergence in the alongshore direction was also investigated. Positive divergence values dominated in the whole analyzed area, and an onshore current appears to be dominant along the southwest coast of the Kii Peninsula, except in 1990 when the Kuroshio flowed in a large meandering path.  相似文献   

The Social Construction of Tourist Places     

Martin Young 《The Australian geographer》1999,30(3):373-389

Ordinary places become tourist places when they are attributed particular meanings and values which appeal to and attract tourists. In this sense, tourist places are socially constructed and negotiated phenomena. This paper explores place meanings in the context of the Daintree and Cape Tribulation area, Far North Queensland, Australia. Two components of place meaning were examined. Firstly, the meanings of place produced by the tourist industry and, secondly, the meanings of place consumed by tourists visiting the area. There existed significant overlap between these constructions in spite of potentially conflicting on-site evidence, suggesting that actual experience of place does not significantly affect place meanings. This was confirmed by a comparison between different groups of tourists, which revealed that the meaning attributed to place was influenced by pre-visitation variables, including existing knowledge, and environmental preferences and experience. A conceptual model of tourist places is proposed, which argues that the success of a tourist place depends on the level of consensus on meanings negotiated between the systems of place production and place consumption.  相似文献   

雷州半岛灯楼角沙岬的形成   总被引：1，自引：1，他引：0  

赵焕庭  王丽荣  宋朝景 《热带地理》2007,27(5):405-410

沙岬(沙嘴)是一种海岸动力地貌类型。通过区域地貌背景、海底地貌-浅地层、海洋动力条件、相关的海岸沙坝和现代海滩的分析,认为灯楼角沙岬是来自琼州海峡的东向波浪和来自北部湾的西向波浪两种相向波浪动力平衡、灯楼角东沿岸存在逆时针环流和灯楼角西沿岸存在顺时针环流两者于此辐合,并把带来的砂子沉积下来的结果。  相似文献   

Potential adverse effects of inorganic pollutants on clinical parameters of loggerhead sea turtles (Caretta caretta): Results from a nesting colony from Cape Verde,West Africa     

《Marine environmental research》2013

A large number of nesting loggerhead sea turtles (n = 201) were sampled to establish the blood levels of 11 elements (Cu, Mn, Pb, Zn, Cd, Ni, Cr, As, Al, Hg, and Se). Almost all of the samples showed detectable levels of these 11 elements, and Zn and Se exhibited the highest concentrations (median values as high as 6.05 and 2.28 μg/g, respectively). The median concentrations of the most toxic compounds, As, Cd, Pb, and Hg, were relatively low (0.38, 0.24, 0.06, and 0.03 μg/g, respectively). We also determined the haematological and biochemical parameters in a subsample of 50 turtles to evaluate the potential effects of these contaminants on clinical parameters and found several associations. Our study reinforces the usefulness of blood for the monitoring of the levels of contaminating elements and their adverse effects on blood parameters in sea turtles.  相似文献   

Dynamics of a mesoscale eddy off Cape Ann, Massachusetts in May 2005     

Mingshun Jiang  Meng Zhou  Scott P. Libby  Donald M. Anderson 《Deep Sea Research Part I: Oceanographic Research Papers》2011,58(11):1130-1146

Observations and numerical modeling indicate that a mesoscale anti-cyclonic eddy formed south of Cape Ann at the northern entrance of Massachusetts Bay (MB) during May 2005, when large river discharges in the western Gulf of Maine and two strong Nor'easters passing through the regions led to an unprecedented toxic Alexandrium fundyense bloom (red tide). Both model results and field measurements suggest that the western Maine Coastal Current separated from Cape Ann around May 7–8, and the eddy formed on around May 10. The eddy was trapped at the formation location for about a week before detaching from the coastline and moving slowly southward on May 17. Both model results and theoretical analysis suggest that the separation of the coastal current from the coast and subsequent eddy formation were initiated at the subsurface by an adverse pressure gradient between Cape Ann and MB due to the higher sea level set up by onshore Ekman transport and higher density in downstream MB. After the formation, the eddy was maintained by the input of vorticity transported by the coastal current from the north, and local vorticity generation around the cape by the horizontal gradients of wind-driven currents, bottom stress, and water density induced by the Merrimack River plume. Observations and model results indicate that the anti-cyclonic eddy significantly changed the pathway of nutrient and biota transport into the coastal areas and enhanced phytoplankton including Alexandrium abundances around the perimeter of the eddy and in the western coast of MB.  相似文献   

What role do beds of submerged macrophytes play in structuring estuarine fish assemblages? Lessons from a warm-temperate South African estuary     

Jill N. Sheppard  Nicola C. James  Alan K. Whitfield  Paul D. Cowley 《Estuarine, Coastal and Shelf Science》2011

Habitat variability is one of the factors influencing species richness within estuarine systems, and a loss of habitat can result in a restructuring of the estuarine ichthyofaunal assemblage, particularly if these conditions persist over long time periods. The potential effects of the loss of extensive submerged macrophyte beds (Ruppia cirrhosa and Potamogeton pectinatus) on an estuarine fish assemblage were investigated through an analysis of a long-term seine net catch dataset from the temporarily open/closed East Kleinemonde Estuary, South Africa. Catch data for a 12-year period, encompassing six years of macrophyte presence and six years of macrophyte senescence, indicated that the loss of this habitat did not influence species richness but changes in the relative abundance of certain species were evident. A shift in dominance from vegetation-associated species to those associated with sandy environments (e.g. members of the family Mugilidae) was observed. However, species wholly dependent on macrophytes such as the critically endangered estuarine pipefish Syngnathus watermeyeri were only recorded during years when macrophyte beds were present, while vegetation-associated species such as the sparid Rhabdosargus holubi persisted at lower levels of relative abundance. The reduced abundance of all vegetation-associated fish species during years of macrophyte senescence was probably reflective of declining food resources resulting from the loss of macrophyte beds and/or increased vulnerability to predation. Submerged beds of aquatic plants are therefore important habitats within temporarily open/closed estuaries, South Africa’s dominant estuary type.  相似文献   

Source, sea level and circulation effects on the sediment flux to the deep ocean over the past 15 ka off eastern New Zealand     

Lionel Carter  Barbara Manighetti  Mike Elliot  Noel Trustrum  Basil Gomez 《Global and Planetary Change》2002,33(3-4)

The last post-glacial transgression and present highstand of sea level were accompanied by a reduction in the terrigenous flux to the deep ocean bordering the active convergent margin off the eastern North Island of New Zealand. Although in accord with long-established models of highstand shelf deposition, new data from giant piston core MD97 2121 (2314 m depth) reveal that the flux also varied with terrigenous supply and palaeocirculation. Between 15 and 9.5 ka, the flux reduced from 33 to 20 g/cm²/ka as supply declined with an expanding vegetation cover, and mud depocentres became established on the continental shelf. An increase from 20 to 27 g/cm²/ka during 9.5–3.5 ka coincided with a strengthened East Cape Current which probably introduced sediment from fluvial and shelf sources in the north. The flux profile shows no immediate response to the establishment of modern sea level 7 ka. However, accumulation decreased from 3.5 to 1 ka as more sediments were retained on the shelf, possibly under wind-strengthened, along-shelf currents. Over the last 1 ka, the flux decline halted under increased terrigenous supply during anthropogenic development of the land.Despite the proximity of the North Island's Central Volcanic Region, major eruptions caused only brief increases (centuries duration) in the terrigenous flux through direct deposition of airfall and possibly fluvial redistribution of onshore volcanic deposits. Frequent earthquakes also had little short-term effect on accumulation although such events, along with volcanism, probably contribute to the long-term high flux of the region.The other measured flux component, biogenic carbonate, reached maxima of 6 g/cm²/ka between 11 and 8.5 ka when nutrient-bearing waters of the East Cape Current dominated the palaeoceanography. After these peaks, carbonate accumulation declined gradually to modern levels of 3 g/cm²/ka.  相似文献   

AGRICULTURAL EVOLUTION ON THE FRONTIER*     

William Norton 《The Professional geographer》1984,36(1):18-27

The evolving agricultural landscapes of frontier settlement are related to distance from entry points, to distance from urban centers, and to aspects of the physical environment. Canonical correlation procedures applied to nineteenth century data for Cape Province, South Africa, and southern Ontario, Canada suggest that commercialization, regionalization and specialization increase through time. Results for southern Ontario are confirmed while those for Cape Province reflect the impact of an expanding frontier area.  相似文献   

A late Pleistocene–Holocene multi‐proxy record of palaeoenvironmental change from Still Bay,southern Cape Coast,South Africa          下载免费PDF全文

Lynne J. Quick  Andrew S. Carr  Michael E. Meadows  Arnoud Boom  Mark D. Bateman  David L. Roberts  Paula J. Reimer  Brian M. Chase 《第四纪科学杂志》2015,30(8):870-885

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