Tourism development on the north Yucatan coast: Human response to shoreline erosion and hurricanes     

Klaus J. Meyer-Arendt Dr. 《GeoJournal》1991,23(4):327-336

The barrier coast of north Yucatan has been evolving into a beachfront recreational landscape since the introduction of passenger rail service between Mérida and Progreso in 1881. Beginning in the 1950's, middle-class vacation home construction spread laterally outward from Progreso, and even distal fishing and salt-gathering villages became engulfed by a recreational landuse overlay. In spite of geomorphic evidence of marine transgression, such as dune scarps and washover fans, the focus of recreational urbanization has been the beachfront. And although attempts at retarding shore erosion have taken place since the 1960s, hazard perception has remained generally low until the late 1980s. When Hurricane Gilbert blew across the Yucatan peninsula in 1988, damage to beachfront structures, highways, boats, and salt ponds was extensive. The barrier environment exhibited extensive overwashing and breaching, especially in areas of human modification, and the lagoon ecosystem experienced considerable ecologic disruption. Because the north Yucatan coast is a locus of domestic tourism, and the thousands of uninsured summer homes are owned largely by members of Mérida's middle class, reconstruction since Gilbert has been slow. Incipient trends of international tourism development have slowed since 1988.  相似文献   

Back-arc rifting in the Izu-Bonin Island Arc: Structural evolution of Hachijo and Aoga Shima Rifts   总被引：1，自引：0，他引：1  

Adam  Klaus Brian  Taylor Gregory F.  Moore Fumitoshi  Murakami Yukinobu  Okamura 《Island Arc》1992,1(1):16-31

Abstract Multi- and single-channel seismic profiles are used to investigate the structural evolution of back-arc rifting in the intra-oceanic Izu-Bonin Arc. Hachijo and Aoga Shima Rifts, located west of the Izu-Bonin frontal arc, are bounded along-strike by structural and volcanic highs west of Kurose Hole, North Aoga Shima Caldera and Myojin Sho arc volcanoes. Zig-zag and curvilinear faults subdivide the rifts longitudinally into an arc margin (AM), inner rift, outer rift and proto-remnant arc margin (PRA). Hachijo Rift is 65 km long and 20–40 km wide. Aoga Shima Rift is 70 km long and up to 45 km wide. Large-offset border fault zones, with convex and concave dip slopes and uplifted rift flanks, occur along the east (AM) side of the Hachijo Rift and along the west (PRA) side of the Aoga Shima Rift. No cross-rift structures are observed at the transfer zone between these two regions; differential strain may be accommodated by interdigitating rift-parallel faults rather than by strike- or oblique-slip faults. In the Aoga Shima Rift, a 12 km long flank uplift, facing the flank uplift of the PRA, extends northeast from beneath the Myojin Knoll Caldera. Fore-arc sedimentary sequences onlap this uplift creating an unconformity that constrains rift onset to ～1-2Ma. Estimates of extension (～3km) and inferred age suggest that these rifts are in the early syn-rift stage of back-arc formation. A two-stage evolution of early back-arc structural evolution is proposed: initially, half-graben form with synthetically faulted, structural rollovers (ramping side of the half-graben) dipping towards zig-zagging large-offset border fault zones. The half-graben asymmetry alternates sides along-strike. The present ‘full-graben’ stage is dominated by rift-parallel hanging wall collapse and by antithetic faulting that concentrates subsidence in an inner rift. Structurally controlled back-arc magmatism occurs within the rift and PRA during both stages. Significant complications to this simple model occur in the Aoga Shima Rift where the east-dipping half-graben dips away from the flank uplift along the PRA. A linear zone of weakness caused by the greater temperatures and crustal thickness along the arc volcanic line controls the initial locus of rifting. Rifts are better developed between the arc edifices; intrusions may be accommodating extensional strain adjacent to the arc volcanoes. Pre-existing structures have little influence on rift evolution; the rifts cut across large structural and volcanic highs west of the North Aoga Shima Caldera and Aoga Shima. Large, rift-elongate volcanic ridges, usually extruded within the most extended inner rift between arc volcanoes, may be the precursors of sea floor spreading. As extension continues, the fissure ridges may become spreading cells and propagate toward the ends of the rifts (adjacent to the arc volcanoes), eventually coalescing with those in adjacent rift basins to form a continuous spreading centre. Analysis of the rift fault patterns suggests an extension direction of N80°E ± 10° that is orthogonal to the trend of the active volcanic arc (N10°W). The zig-zag pattern of border faults may indicate orthorhombic fault formation in response to this extension. Elongation of arc volcanic constructs may also be developed along one set of the possible orthorhombic orientations. Border fault formation may modify the regional stress field locally within the rift basin resulting in the formation of rift-parallel faults and emplacement of rift-parallel volcanic ridges. The border faults dip 45–55° near the surface and the majority of the basin subsidence is accommodated by only a few of these faults. Distinct border fault reflections decreases dips to only 30° at 2.5 km below the sea floor (possibly flattening to near horizontal at 2.8 km although the overlying rollover geometry shows a deeper detachment) suggesting that these rifting structures may be detached at extremely shallow crustal levels.  相似文献   

Development of a Standard, Pure-Compound Base Gasoline Mixture for Use as a Reference in Field and Laboratory Experiments   总被引：2，自引：0，他引：2  

David K. Kreamer  Klaus J. Stetzenbach 《Ground Water Monitoring & Remediation》1990,10(2):135-145

In recent years, leaking underground petroleum storage tanks have become a major environmental concern. Federal, state, and local agencies are making efforts to assess, control, and remediate petroleum product leaks. Because petroleum products are mixtures of many compounds and the composition frequently changes, there exists a need for a standard reference mixture that can be used as a basis for comparison in the study of fluid transport properties in porous media and to evaluate leak detection devices. The proposed standard presented here retains the most important liquid and vapor properties (such as vapor density, air diffusion coefficient, and basic chemical constituency) of gasoline mixtures. It also reduces the complexity of the mixture to make it an acceptable standard for routine use in laboratory and field experiments.  相似文献   

A Two-Channel Focal Reducer for Small (Diameter ≥ 1 M) F/8 Telescopes     

Klaus Jockers 《Experimental Astronomy》1997,7(4):305-318

The new Two-Channel Focal Reducer of the Max-Planck-Institut für Aeronomie is described. The instrument is primarily designed for astronomical imaging of solar system objects, where, because of changes in time scales of about 10-30 min not only the photon flux but also the total number of photons is limited. Colour dividers allow to split the light of the object into a "blue" and a "red" channel. Both channels are observed simultaneously with two separate CCD cameras. Besides wide-band imaging with filters derived from the Gunn photometric system, the instrument allows simultaneous determination of polarization and colour in a small field and imaging with interference filters and with a tunable Fabry-Perot interferometer. One Fabry-Perot system serves both channels. Proper selection of the interference order allows simultaneous observing in narrow bands of about 3 width for a large number of wavelength pairs. There is also a coronagraph mode with Lyot stops in both channels which allows observations of the torus associated with Jupiter's satellite Io. Long-slit two-channel spectroscopy will be possible as soon as the necessary grating prisms will have been acquired.  相似文献   

Inherited igneous zircons in jadeitite predate high-pressure metamorphism and jadeitite formation in the Jagua Clara serpentinite mélange of the Rio San Juan Complex (Dominican Republic)     

Andreas Hertwig  William C. McClelland  Kouki Kitajima  Hans-Peter Schertl  Walter V. Maresch  Klaus Stanek  John W. Valley  Sergey A. Sergeev 《Contributions to Mineralogy and Petrology》2016,171(5):48

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Adaptation of reef and mangrove sponges to stress: evidence for ecological speciation exemplified by Chondrilla caribensis new species (Demospongiae, Chondrosida)     

Klaus Rützler  Sandra Duran  & Carla Piantoni 《Marine Ecology》2007,28(S1):95-111

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The Black Band Disease of Atlantic Reef Corals.   总被引：4，自引：0，他引：4  

Klaus  Rutzler  Deborah L.  Santavy Arnfried  Antonius 《Marine Ecology》1983,4(4):329-358

Abstract. The cyanophyte (Cyanobaclerium) that causes black band disease of Atlantic reef corals is described under the name Phormidium corallyticum , new species (family Oscillatoriaceae) , and its generic placement is discussed from the standpoint of the GEITLERian (classical) and D rouet systems. Distinguishing characters include densely interwoven filaments that form a blackish mat and trichomes without significant cell wall constrictions, almost isodiametric cells (4.2 μm mean width, 4.0μm mean length) tapering end cells, and thin (0.1 μm or less) mucilaginous wall coating. Transmission electron microscopy shows typical cyanophyte cell walls, sheath, nucleoplasm, and cytoplasmic inclusions, but an unusual thylakoid of straight, and, as seen in cell cross section, radiating lamellae. The dark coloration is due to a high concentration of phycocyanin and some phycoerythrin. The species is similar to Oscillatoria (= Phormidium) submembranacea , which differs in several morphological features and does not infect coral tissue. It is concluded that Phormidium should be used for this and related species that have external mucilage but not the distinct sheath found in Lyngbya.  相似文献   

The Influence of Metoclopramide and Melatonin on Activity and Schooling Behaviour in Chromis viridis (CUVIER, 1830; Pomacentridae, Teleostei)     

Klaus  Sparwasser 《Marine Ecology》1987,8(4):297-312

Abstract. The role of prolactin (PRL) in the neuroendocrine control of schooling behaviour and activity in the demoiselle Chromis viridis is analysed by administration of a prolactin-releasing drug, metoclopramide (Paspertin®). In addition, the dependence of the activity state, schooling time, and colour changes on the administration of an epiphysial hormone, melatonin, is examined. Each substance tested affects schooling behaviour and activity by a different mechanism.  相似文献   

On the problem of future replacement of Knudsen-Ekman's equation of state of seawater     

Klaus Grasshoff 《Journal of Oceanography》1976,32(3):151-153

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IGU Study group “famine research and food production systems”     

A. H. Bakhit  Klaus Müller-Hohenstein 《GeoJournal》1991,25(1):127-128

IGU-Reports

IGU Study group famine research and food production systems  相似文献