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181.
D. S. Ormerod N. W. Rogers C. J. Hawkesworth 《Contributions to Mineralogy and Petrology》1991,108(3):305-317
The variations in trace element abundances of a suite of alkali-olivine basalts from the Big Pine volcanic field, California,
have been ‘inverted’ following the method of Hofmann and co-workers to obtain source concentration and distribution coefficient
data. The high Mg-numbers and ne-normative mineralogy of these lavas allow a simple correction to be made for fractional crystallisation,
and together with a limited range in 87Sr/86Sr (0.7056–0.7064), suggest derivation from a relatively homogeneous source region. Negative correlations between SiO2 and P2O5, and SiO2 and Rb in the calculated primary magmas imply that both major and trace elements vary in a coherent fashion as a function
of the degree of partial melting. The Big Pine lavas are characterised by high ratios of large-ion lithophile to high-field
strength elements (Ba/Nb>60), and the inverse procedure demonstrates that this reflects source concentrations, as opposed
to a mineralogical control. The calculated mantle source is further characterised by generally high abundances of Sr, Ba,
K, and Th relative to Nb and Ta which imply that incompatible element enrichment of the source occurred above a subduction
zone. A model Sm/Nd age of 1.8 Ga for this enrichment coincides with the regional crustal formation age. Such features imply
that both the major and trace element components of the Big Pine lavas are derived from within lithospheric mantle, perhaps
mobilised by the high geothermal gradients which characterise the extensional environment of the Basin and Range Province.
A comparison with other Cenozoic mafic lavas throughout the western United States suggests that a substantial proportion of
the mantle lithosphere in this area has similar chemical characteristics to the source of the Big Pine lavas. If this is the
case, then it implies that convergent margins represent an important tectonic environment for the formation of lithospheric
mantle. 相似文献
182.
183.
Restructuring the kiosk trade in St. Petersburg: A new retail trade model for the post-Soviet period
This study explores the commercial kiosk phenomenon as a reflection of the socio-spatial reordering of St. Petersburg following the introduction of market forces. In this article we interpret empirical evidence on the restructuring of commercial opportunity in post-Soviet St. Petersburg as a result of the emergence of the kiosk phenomenon. Kiosk trade and processes that contribute to it have emerged as tools for mass socioeconomic and psychological adaptation, following the dismantling of the communist regime. In our opinion, the emergence and continuing mutation of St. Petersburg kiosks constitutes the backbone of a process of middle-class formation. An extensive field research of 1989, 1994 and 1995 made it possible to study the dynamics of spatial structures of kiosk phenomenon. It is our final conclusion that kiosks will remain an important feature of St. Petersburgs commercial geography in the foreseeable future. 相似文献
184.
185.
Jason L. Howard Alex Perez Christian C. Lopes James W. Fourqurean 《Estuaries and Coasts》2016,39(5):1422-1434
Seagrass ecosystems are attracting attention as potentially important tools for carbon (C) sequestration, comparable to those terrestrial and aquatic ecosystems already incorporated into climate change mitigation frameworks. Despite the relatively low C stocks in living biomass, the soil organic carbon pools beneath seagrass meadows can be substantial. We tested the relationship between soil C storage and seagrass community biomass, productivity, and species composition by revisiting meadows experimentally altered by 30 years of consistent nutrient fertilization provided by roosting birds. While the benthos beneath experimental perches has maintained dense, Halodule wrightii-dominated communities compared to the sparse Thalassia testudinum-dominated communities at control sites, there were no significant differences in soil organic carbon stocks in the top 15 cm. Although there were differences in δ13C of the dominant seagrass species at control and treatment sites, there was no difference in soil δ13C between treatments. Averages for soil organic carbon content (2.57?±?0.08 %) and δ13C (?12.0?±?0.3?‰) were comparable to global averages for seagrass ecosystems; however, our findings question the relevance of local-scale seagrass species composition or density to soil organic carbon pools in some environmental contexts. 相似文献
186.
Scraping and extirpating: two strategies to induce recovery of diseased Gorgonia ventalina sea fans
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Claudia Patricia Ruiz‐Diaz Carlos Toledo‐Hernández Alex E. Mercado‐Molina Alberto M. Sabat 《Marine Ecology》2016,37(2):336-343
Coral diseases are currently playing a major role in the worldwide decline in coral reef integrity. One of the coral species most afflicted by disease in the Caribbean, and which has been the focus of much research, is the sea fan Gorgonia ventalina. There is, however, very little information regarding the capacity of sea fans to recover after being infected. The aim of this study was to compare the rehabilitation capacity of G. ventalina after diseased‐induced lesions were eliminated either by scraping or extirpating the affected area. Scraping consisted of removing any organisms overgrowing the axial skeleton from the diseased area as well as the purple tissue bordering these overgrowths using metal bristle brushes. Extirpation consisted of cutting the diseased area, including the surrounding purpled tissue, using scissors. The number of scraped colonies that fully or partially rehabilitated after being manipulated and the rates at which the sea fans whose lesions were scrapped grew back healthy tissue were compared among: (i) colonies that inhabited two sites with contrasting environmental conditions; (ii) colonies of different sizes and (iii) colonies with different ratios of area of legions to total colony area (LA/CA). Both strategies proved to be very successful in eliminating lesions from sea fans. In the case of scraping, over 51% of the colonies recovered between 80% and 100% of the lost tissue within 16 months. The number of colonies that recovered from scraping was similar among sites and among colony sizes, but differed significantly depending on the relative amount of lesion to colony area (LA/CA). When lesions were extirpated, lesions did not reappear in any of the colonies. We conclude that lesion scraping is useful for eliminating relatively small lesions (i.e. LA/CA < 10%), as these are likely to recover in a shorter period of time, whereas for relatively large lesions (LA/CA ≥ 10%) it is more appropriate to extirpate the lesion. 相似文献
187.
The paper reports unique high-resolution observations of meteotsunami by a large array of oceanographic instruments deployed on the Atchafalaya Shelf (Louisiana, USA) in 2008 with the primary aim to study wave dissipation in muddy environments. The meteotsunami event on March 7, 2008, was caused by the passage of a cold front which was monitored by the NOAA NEXRAD radar. The observations of water surface elevations on the shelf show a highly detailed textbook picture of an undular bore (solibore) in the process of its disintegration into a train of solitons. The picture has a striking feature never reported before not only for the meteotsunamis but in other contexts of disintegration of a long-wave perturbation into a sequence of solitons as well—the persistent presence of a single soliton, well ahead of the solibore. Data analysis and simulations based on the celebrated variable-coefficient KdV (vKdV) equation first proposed by Ostrovsky and Pelinovsky (Izv Atmos Ocean Phys 11:37–41, 1975) explain the physics of this phenomenon and suggest that the formation of the lone soliton ahead of the solibore is very likely to be the result of the specific interplay of natural meteotsunami forcing and nearshore bathymetry. The analysis strongly suggests that the patterns of coexisting lone solitons and packets of cnoidal waves should be quite common for meteotsunamis. They were not observed before only because of the scarcity of high-resolution observations. The results highlight the effectiveness of the vKdV equation in providing understanding of the fundamental mechanisms of the complex natural phenomenon that would otherwise require computationally very expensive numerical models. 相似文献
188.
Adam Lewis Leo Lymburner Matthew B. J. Purss Brendan Brooke Ben Evans Alex Ip 《International Journal of Digital Earth》2016,9(1):106-111
The effort and cost required to convert satellite Earth Observation (EO) data into meaningful geophysical variables has prevented the systematic analysis of all available observations. To overcome these problems, we utilise an integrated High Performance Computing and Data environment to rapidly process, restructure and analyse the Australian Landsat data archive. In this approach, the EO data are assigned to a common grid framework that spans the full geospatial and temporal extent of the observations – the EO Data Cube. This approach is pixel-based and incorporates geometric and spectral calibration and quality assurance of each Earth surface reflectance measurement. We demonstrate the utility of the approach with rapid time-series mapping of surface water across the entire Australian continent using 27 years of continuous, 25?m resolution observations. Our preliminary analysis of the Landsat archive shows how the EO Data Cube can effectively liberate high-resolution EO data from their complex sensor-specific data structures and revolutionise our ability to measure environmental change. 相似文献
189.
As the number of climatological studies using record-breaking statistics is growing rapidly, understanding the sensitivity of the chosen time period becomes essential. To that end, here we examine the evolving variability of monthly mean temperatures and its dependence on beginning and final year. Specifically, we use an index, α, based on record-breaking statistics and employing reversibility such that 〈α〉=0 indicates no trend in variability. Generally, 〈α〉 has decreased between 1900 and 2013, indicating decreasing variability relative to early decades for stations from the contiguous USA (United States Historical Climatology Network, version 2.5). We find, somewhat surprisingly, that the observed decrease is due to an early excess of records beginning in 1917 (record low value) and 1921 (record high value). While detailed results depend on whether the data is gridded, detrended, etc., the general finding appears remarkably robust and holds globally as well. 相似文献
190.