Variation in the abundance of sandeels Ammodytes marinus off southeast Scotland: an evaluation of area-closure fisheries management and stock abundance assessment methods     

Greenstreet  Simon P.R.; Armstrong  Eric; Mosegaard  Henrik; Jensen  Henrik; Gibb  Iain M.; Fraser  Helen M.; Scott  Beth E.; Holland  Gayle J.; Sharples  Jonathan 《ICES Journal of Marine Science》2006,63(8):1530-1550

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Religion on the Fringe: the representation of space and minority religious facilities in the rural–urban fringe of metropolitan Sydney,Australia     

Laura Beth Bugg 《The Australian geographer》2012,43(3):273-289

This article examines land-use development applications for minority religious facilities in two local government areas on the rural–urban fringe of metropolitan Sydney, Australia. Using critical discourse analysis and underpinned by Lefebvre's (1991) conceptual triad of space, the work interrogates the way in which place identity is generated and codified both by land-use planners and local residents through spatial representation. This representation is revealed in discourses around the compatibility of minority religious facilities for particular zones, lack of a sufficient minority population and social disruption. These discourses reveal a construction of peri-urban space that is aligned with particular elite Anglo-Australian activities (horse riding and gentleman farms) and land uses (rural residential, small-scale agriculture and the ‘bush-church’). These case studies illustrate the potential for the creation of exclusionary, abstract space by urban planners but also the ways in which local residents use discoursive strategies to ensure the stability of their position as elites in rapidly changing spatial situations.  相似文献   

Spectroscopy of K-complex asteroids: Parent bodies of carbonaceous meteorites?     

Beth Ellen Clark  Maureen E. Ockert-Bell  David Nesvorny  Schelte J. Bus 《Icarus》2009,202(1):119-133

This is the first focused study of non-Eos K asteroids. We have observed a total of 30 K-complex objects (12 K-2 Sk- and 13 Xk-type asteroids (from the Bus taxonomy), plus 3 K-candidates from previous work) and we present an analysis of their spectral properties from 0.4 to 2.5 μm. We targeted these asteroids because their previous observations are spectrally similar enough to suggest a possible compositional relationship. All objects have exhibited spectral redness in the visible wavelengths and minor absorptions near 1 micron. If, as suggested, K-complex asteroids (including K, Xk, and Sk) are the parent bodies of carbonaceous meteorites, knowledge of K-asteroid properties and distribution is essential to our understanding of the cosmochemical importance of some of the most primitive meteorite materials in our collection. This paper presents initial results of our analysis of telescopic data, with supporting analysis of laboratory measurements of meteorite analogs. Our results indicate that K-complex asteroids are distinct from other main belt asteroid types (S, B, C, F, and G). They do not appear to be a subset of these other types. K asteroids nearly span the range of band center positions and geometric albedos exhibited by the carbonaceous chondrites (CO, CM, CV, CH, CK, CR, and CI). We find that B-, C-, F- and G-type asteroids tend to be darker than meteorites, and can have band centers longer than any of the chondrites measured here. This could indicate that K-complex asteroids are better spectral analogues for the majority of our carbonaceous meteorites than the traditional B-, C-, F- and G-matches suggested in the literature. This paper present first results of our ongoing survey to determine K-type mineralogy, meteorite linkages, and significance to the geology of the asteroid regions.  相似文献   

Potential climate-change impacts on the Chesapeake Bay   总被引：1，自引：0，他引：1  

Raymond G. Najjar  Christopher R. Pyke  Mary Beth Adams  Denise Breitburg  Carl Hershner  Michael Kemp  Robert Howarth  Margaret R. Mulholland  Michael Paolisso  David Secor  Kevin Sellner  Denice Wardrop  Robert Wood 《Estuarine, Coastal and Shelf Science》2010

We review current understanding of the potential impact of climate change on the Chesapeake Bay. Scenarios for CO₂ emissions indicate that by the end of the 21^st century the Bay region will experience significant changes in climate forcings with respect to historical conditions, including increases in CO₂ concentrations, sea level, and water temperature of 50–160%, 0.7–1.6 m, and 2–6 °C, respectively. Also likely are increases in precipitation amount (very likely in the winter and spring), precipitation intensity, intensity of tropical and extratropical cyclones (though their frequency may decrease), and sea-level variability. The greatest uncertainty is associated with changes in annual streamflow, though it is likely that winter and spring flows will increase. Climate change alone will cause the Bay to function very differently in the future. Likely changes include: (1) an increase in coastal flooding and submergence of estuarine wetlands; (2) an increase in salinity variability on many time scales; (3) an increase in harmful algae; (4) an increase in hypoxia; (5) a reduction of eelgrass, the dominant submerged aquatic vegetation in the Bay; and (6) altered interactions among trophic levels, with subtropical fish and shellfish species ultimately being favored in the Bay. The magnitude of these changes is sensitive to the CO₂ emission trajectory, so that actions taken now to reduce CO₂ emissions will reduce climate impacts on the Bay. Research needs include improved precipitation and streamflow projections for the Bay watershed and whole-system monitoring, modeling, and process studies that can capture the likely non-linear responses of the Chesapeake Bay system to climate variability, climate change, and their interaction with other anthropogenic stressors.  相似文献   

Population-level genotyping of coat colour polymorphism in woolly mammoth (Mammuthus primigenius)     

Claire Workman  Love Dalen  Sergey Vartanyan  Beth Shapiro  Pavel Kosintsev  Andrei Sher  Anders Gotherstrom  Ian Barnes 《Quaternary Science Reviews》2011,30(17-18):2304-2308

Patterns in the spatial or temporal distribution of genotypes may be indicative of natural selection. Previous work on the woolly mammoth melanocortin-1 receptor (Mc1r) gene identified three polymorphic positions that suggest Pleistocene populations may have harboured both light- and dark-haired mammoths (Rompler et al., 2006, 313: 62). Here, we extend this work and present the first population-level analysis of a functional gene in an extinct species. We genotyped the Mc1r gene in 47 woolly mammoth samples excavated from sites across the central portion of the woolly mammoths’ former range to examine the extent of variation of this polymorphism through time and across space. Only one individual was found to be heterozygous, indicating that the frequency of the ‘light’ mutant allele was very low. We conclude that light-coloured woolly mammoths would have been very rare, and may even have been non-existent if the ‘light’ mutant allele was strongly selected against in its homozygotic form. With the increasing availability of large-scale sequencing technologies, population-level datasets capable of identifying local adaptation will become increasingly attainable.  相似文献   

Diffusive Disappearance of Immiscible-Phase Organic Liquids in Fractured Geologic Media   总被引：3，自引：0，他引：3  

Beth L. Parker  Robert W. Gillham  John A. Cherry 《Ground water》1994,32(5):805-820

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Landscape disequilibrium on 1000–10,000 year scales Marsyandi River, Nepal, central Himalaya     

Beth Pratt-Sitaula  Douglas W. Burbank  Arjun Heimsath  Tank Ojha 《Geomorphology》2004,58(1-4):223-241

In an actively deforming orogen, maintenance of a topographic steady state requires that hillslope erosion, river incision, and rock uplift rates are balanced over timescales of 10⁵–10⁷ years. Over shorter times, <10⁵ years, hillslope erosion and bedrock river incision rates fluctuate with changes in climate. On 10⁴-year timescales, the Marsyandi River in the central Nepal Himalaya has oscillated between bedrock incision and valley alluviation in response to changes in monsoon intensity and sediment flux. Stratigraphy and ¹⁴C ages of fill terrace deposits reveal a major alluviation, coincident with a monsoonal maximum, ca. 50–35 ky BP. Cosmogenic ¹⁰Be and ²⁶Al exposure ages define an alluviation and reincision event ca. 9–6 ky BP, also at a time of strong South Asian monsoons. The terrace deposits that line the Lesser Himalayan channel are largely composed of debris flows which originate in the Greater Himalayan rocks up to 40 km away. The terrace sequences contain many cubic kilometers of sediment, but probably represent only 2–8% of the sediments which flushed through the Marsyandi during the accumulation period. At 10⁴-year timescales, maximum bedrock incision rates are 7 mm/year in the Greater Himalaya and 1.5 mm/year in the Lesser Himalayan Mahabarat Range. We propose a model in which river channel erosion is temporally out-of-phase with hillslope erosion. Increased monsoonal precipitation causes an increase in hillslope-derived sediment that overwhelms the transport capacity of the river. The resulting aggradation protects the bedrock channel from erosion, allowing the river gradient to steepen as rock uplift continues. When the alluvium is later removed and the bedrock channel re-exposed, bedrock incision rates probably accelerate beyond the long-term mean as the river gradient adjusts downward toward a more “equilibrium” profile. Efforts to document dynamic equilibrium in active orogens require quantification of rates over time intervals significantly exceeding the scale of these millennial fluctuations in rate.  相似文献   

Earthquake recurrence parameters from seismic and geodetic strain rates in the eastern Mediterranean   总被引：8，自引：0，他引：8  

Sarah Jenny  Saskia Goes  Domenico Giardini  Hans-Gert Kahle 《Geophysical Journal International》2004,157(3):1331-1347

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Migration Patterns During a Period of Political and Economic Shocks in the Former Soviet Union: A Case Study of Yaroslavl' Oblast*     

Beth Mitchneck  David Plane 《The Professional geographer》1995,47(1):17-30

This paper examines migration in Russia during the period that preceded the breakup of the former Soviet Union (FSU) and during the current transition period. An unusually rich dataset is used to conceptualize the impact that the political and economic collapse of a world superpower has on a migration system. A regional case study of migration in Yaroslavl' Oblast from 1989 through 1992 is used to examine the relevance of expected outcomes given standard theories of migration, empirical regularities found in capitalist economies, and past trends in the FSU. The data clearly show a migration system undergoing political and economic shocks. A significant decline of the volume of flows and a relative increase in the importance of interrepublic movement indicate disruptions. Increased relative mobility for those in the later years of the working-age population and increased importance of urban-to-rural migration flows are also important changes evident in this migration system undergoing shock.  相似文献   

Report on I.A.G.-S.S.G. 5.97/3.90 International Workshop ETH Zurich     

H. -G. Kahle 《Journal of Geodesy》1986,60(2):174-175

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