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81.
Jakob Heyman Arjen P. Stroeven Marc W. Caffee Clas Hättestrand Jonathan M. Harbor Yingkui Li Helena Alexanderson Liping Zhou Alun Hubbard 《Quaternary Science Reviews》2011,30(15-16):1988-2001
The Bayan Har Shan, a prominent upland area in the northeastern sector of the Tibetan Plateau, hosts an extensive glacial geological record. To reconstruct its palaeoglaciology we have determined 10Be exposure ages based on 67 samples from boulders, surface pebbles, and sediment sections in conjunction with studies of the glacial geology (remote sensing and field studies) and numerical glacier modelling. Exposure ages from moraines and glacial sediments in Bayan Har Shan range from 3 ka to 129 ka, with a large disparity in exposure ages for individual sites and within the recognised four morphostratigraphical groups. The exposure age disparity cannot be explained by differences in inheritance without using unrealistic assumptions but it can be explained by differences in post-depositional shielding which produces exposure ages younger than the deglaciation age. We present a palaeoglaciological time-slice reconstruction in which the most restricted glaciation, with glaciers less than 10 km long, occurred before 40–65 ka. More extensive glaciations occurred before 60–100 ka and 95–165 ka. Maximum glaciation is poorly constrained but probably even older. The Bayan Har Shan exposure age dataset indicates that glaciers on the northeastern Tibetan Plateau have remained surprisingly restricted for at least 40 ka, including the global last glacial maximum (LGM). This case of a missing LGM is further supported by high-resolution glacier modelling experiments. 相似文献
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84.
Phytoplankton seasonal and interannual variability in the Guadiana upper estuary was analyzed during 1996–2005, a period that
encompassed a climatic controlled reduction in river flow that was superimposed on the construction of a dam. Phytoplankton
seasonal patterns revealed an alternation between a persistent light limitation and episodic nutrient limitation. Phytoplankton
succession, with early spring diatom blooms and summer–early fall cyanobacterial blooms, was apparently driven by changes
in nutrients, water temperature, and turbulence, clearly demonstrating the role of river flow and climate variability. Light
intensity in the mixed layer was a prevalent driver of phytoplankton interannual variability, and the increased turbidity
caused by the Alqueva dam construction was linked to pronounced decreases in chlorophyll a concentration, particularly at the start and end of the phytoplankton growing period. Decreases in annual maximum and average
abundances of diatoms, green algae, and cyanobacteria were also detected. Furthermore, chlorophyll a decreases after dam filling and a decrease in turbidity may point to a shift from light limitation towards a more nutrient-limited
mode in the near future. 相似文献
85.
The sedimentary record from the Ugleelv Valley on central Jameson Land, East Greenland, adds new information about terrestrial palaeoenvironments and glaciations to the glacial history of the Scoresby Sund fjord area. A western extension of a coastal ice cap on Liverpool Land reached eastern Jameson Land during the early Scoresby Sund glaciation (≈the Saalian). During the following glacial maximum the Greenland Ice Sheet inundated the Jameson Land plateau from the west. The Weichselian also starts with an early phase of glacial advance from the Liverpool Land ice cap, while polar desert and ice‐free conditions characterised the subsequent part of the Weichselian on the Jameson Land plateau. The two glaciation cycles show a repeated pattern of interaction between the Greenland Ice Sheet in the west and an ice cap on Liverpool Land in the east. Each cycle starts with extensive glacier growth in the coastal mountains followed by a decline of the coastal glaciation, a change to cold and arid climate and a late stage of maximum extent of the Greenland Ice Sheet. Copyright © 2005 John Wiley & Sons, Ltd. 相似文献
86.
Terezinha Cássia de Brito Galvão Aloisio Rodrigues Pereira Arnaldo Teixeira Coelho Paula Rodrigues Pereira Joaquim Fernandes Teixeira Coelho 《Geotechnical and Geological Engineering》2011,29(1):49-55
Soil erosion, transport and deposition of sediments represent invisible threats that along time can affect negatively the
existing infrastructure of roads and dams, and the quality of air and water resources. In the last decades, a great number
of researches were devoted to study erosion and sediments transportation processes. However, they addressed mostly areas of
agriculture, water impoundments for dams, and land conservation. A lack of studies for erosion processes in urban areas is
evident, in special those aiming to diminish the deposition of sediments originated from urban areas into the rivers and air,
in special as airborne particulate. Traditionally, the costs associated in controlling erosion and sediments in urban areas
are high and in some case, out of the range for most developing countries. Factors responsible for those high prices are the
use of heavy equipments for soil grading and transportation, the use of costly building materials, and the need for employing
more specialized personnel. In the case of gullies in urban areas, another concern is to ensure proper equipment access to
the area for remediation operations. Hereby, it is presented a cost-effective method to recover an extensive gully erosion
area of about 11,000 m2 located in urban area. Estimated sediments released from this area to the water resources and air were estimated on about
66,000,000 tons. In this study area, bioengineering works were performed in 60 days, with hardly any sediment generated outside
the work area resulting from bioengineering operations. A combination of bioengineering techniques were chosen for this study
area, which was a mixture of rigid and biological products including biologs, silt fence, biodegradable straw blankets sewn
with plastic threads derived from recycled PET bottles, among others. An efficient drainage system was implemented for preventing
upland flow, sub-seepage and seepage. Biologs were used aiming to fulfill a double role, the first as barrier to soil sediments
flow, and the second as filler for empty spaces, avoiding expensive grading operations. All engineering works were concluded
in about 60 days at a cost of US0.89/m < sup > 2 < /sup > . This price is cost-effective if compared with the traditional engineering cost of approximately US 0.89/m2. This price is cost-effective if compared with the traditional engineering cost of approximately US 2.92/m2 because it includes extensive use of grading and soil transportation. An environmental advantage of the bioengineering method
is the immediate reduction of airborne particulates. Furthermore, the overall visual aesthetics improved shortly after the
implementation of the works because the bare ground was substituted by native vegetation. After 6 months the vegetation in
the gully erosion area was totally established. Monitoring was performed after 12 months and no erosion and sediment transport
was visually noticed. The ease implementation of this technique without the need for specialized workers in combination with
low prices makes this method a model for developing countries. 相似文献
87.
S. Tavares H. OliveiraJ.P. Coelho M.E. PereiraA.C. Duarte M.A. Pardal 《Estuarine, Coastal and Shelf Science》2011,94(4):315-321
Mercury accumulation throughout the lifespan of Liza aurata (Risso, 1810) was analysed in four tissues (muscle, gills, liver and brain) in two southern European coastal ecosystems with distinct mercury contamination. Specimens from four to five age classes were captured in two sampling sites in the Ria de Aveiro (Laranjo bay and Mira), a system historically contaminated by industrial mercury, and in one site in the Mondego estuary, assumed as a mercury-free ecosystem. Mercury concentration in all tissues was found to be significantly higher in the Ria de Aveiro (Laranjo bay) compared to the Mondego, in accordance with the environmental contamination (water, sediments and suspended particulate matter). Significant differences inside the Ria de Aveiro (between the Mira and Laranjo bay) were only detected in the liver. This tissue registered the highest levels of mercury (ranging from 0.11 to 4.2 μg g−1) in all sampling sites, followed by muscle, brain, and gills. In all sampling sites and tissues was denoted a mercury dilution pattern along the lifecycle (except in liver at the Mondego, the reference area where the concentrations are always very low). An exponential trend was found in the metal age variation patterns in Laranjo (the most contaminated area) and a linear trend in the Mira and the Mondego (the least contaminated areas). Organic mercury concentration in muscle generally accounted for over 95% of total mercury concentration, and followed the same accumulation pattern of total mercury. This fish species is of lesser importance in mercury transfer to adjacent coastal areas and although the consumption of fish from Laranjo may present some risk for the humans, this risk decreases with fish age/size. 相似文献
88.
John Kouroutzoglou Helena A. Flocas Ian Simmonds Kevin Keay Maria Hatzaki 《Theoretical and Applied Climatology》2011,105(1-2):263-275
A comparison of two objective climatologies of explosive cyclones in the Mediterranean region is performed. The results are derived from two different mean sea-level pressure reanalysis data resolutions, but from the same assimilation model, in order to quantify the pure impact of higher resolution on the identification and characteristics of explosive cyclones, when the assimilation model is the same. The explosive cyclones were identified with the aid of the Melbourne University automatic cyclone finding and tracking scheme over a 40-year period, using the 6-hourly analyses of ERA-40 mean sea-level pressure (MSLP) on: (a) 2.5?×?2.5 and (b) 1?×?1 latitude–longitude grid. The comparison of the two datasets revealed the significant role of the increase in spatial resolution of MSLP data on the identification and tracking process, and the number of the explosive cyclones in the high-resolution dataset is almost four times greater than the respective one in the lower resolution dataset. However, the comparison of explosive cyclone characteristics, including spatial and temporal variations of explosive deepening, revealed differences in the geographical distribution of the location of the maximum explosive deepening and average explosive cyclone Laplacian of the central pressure. These differences are due to the identification in the higher resolution set of smaller scale and secondary explosives along the strongly baroclinic northern Mediterranean boundaries, south of the Alps and the Pyrenees. Explosive deepening appears a bias to the daytime period from 12 to 18 Coordinated Universal Time (UTC) for both datasets, which is more prominent in the LR dataset. Statistically significant difference of pressure tendency between the two datasets appear for the daytime period from 06 to 12 UTC, accounting for better representation of orographic forcing in the HR dataset. 相似文献
89.
Carlos J. Archanjo Luiz G.F. Viegas Maria Helena B.M. Hollanda Laecio C. Souza Dunyi Liu 《Gondwana Research》2013,23(2):701-714
The Seridó schist belt is a classical domain of the Borborema Province (NE Brazil) recording crustal melting at HT/LP conditions in a tectonic setting dominated by dextral transpressive deformation. A comparable tectonometamorphic setting has been described in the Pan-African Igarra and Ilesha schist belts of south Nigeria (Africa). The HT‐transpression of the Seridó has previously been imprecisely dated by using a range of isotopic methods on a suite of syntectonic granites. We provide new UPb zircon ages of the Acari granite and Santa Luzia migmatite that constrain the HT/LP metamorphism of the Seridó at c. 575 Ma. Anisotropy of magnetic susceptibility of the Santa Luzia migmatite shows that the magnetic fabric records the NE-trending dextral kinematics similar to those previously described in the Acari pluton. On the other hand, the UPb ages of the Totoró pluton provide evidence for an older, mostly mafic to intermediate magmatism intruding the pelitic schist that precedes the HT/LP metamorphism by approximately 15 m.y. In contrast with the Acari pluton and Santa Luzia migmatite, the magnetic fabrics of Totoró show a concentric steep-dipping structure apparently related to magma ascent. Thermobarometric studies in the Seridó, Igarra and Ilesha schist belts indicate that a large domain in the northern Borborema and south of the Nigeria shields was deformed at a high temperature and at relatively shallow depths. Although the tectonic setting for such a post-collision HT event remains an open issue, it allows us nevertheless to refine the across-Atlantic geological correlation between the continents. 相似文献
90.
Despite the fact that the field of GIScience has been around for two decades, there is still little agreement as to the exact contents and boundaries of the field. Many authors have dedicated several publications concerned with defining the field, yet little consensus has been reached. Because of the highly dynamic nature of the discipline, new areas are constantly added and rigid borders may have a constraining influence on the field. On the contrary, one agreed part of the many GIScience definitions is the search for general principles, but principles for what? Can we define one field or discipline or all potential fields using geospatial information? Probably not. Therefore, rather than attempting to demarcate exact boundaries for GIScience as a discipline or a multidisciplinary field in order to prove its respectability, we herein attempt to analyze the contents of such a dynamic field on the basis of scientific literature and to assess the multidisciplinary and multiparadigmatic nature of GIScience. Such a discussion is not purely of academic nature, but also bears implications beyond academic discourse, in terms of external scientific funding and research grants. We question whether there is a “dominant” paradigmatic approach in GIScience and identify a need for adopting a multiparadigmatic view to accommodate the multifaceted nature of space, spatial representations, and the societal implications of geospatial information. 相似文献