Petrology and geochemistry of REE-rich Mafé banded iron formations (Bafia group,Cameroon)     

Charles Nkoumbou  Fuh Calistus Gentry  Jacqueline Tchakounte Numbem  Yolande Vanessa Belle Ekwe Lobé  Christin Steve Nwagoum Keyamfé 《Comptes Rendus Geoscience》2017,349(4):165-174

Archaean–Paleoproterozoic foliated amphibole-gneisses and migmatites interstratified with amphibolites, pyroxeno-amphibolites and REE-rich banded-iron formations outcrop at Mafé, Ndikinimeki area. The foliation is nearly vertical due to tight folds. Flat-lying quartz-rich mica schists and quartzites, likely of Pan-African age, partly cover the formations. Among the Mafé BIFs, the oxide BIF facies shows white layers of quartz and black layers of magnetite and accessory hematite, whereas the silicate BIF facies is made up of thin discontinuous quartz layers alternating with larger garnet (almandine–spessartine) + chamosite + ilmenite ± Fe-talc layers. REE-rich oxide BIFs compositions are close to the East Pacific Rise (EPR) hydrothermal deposit; silicate BIFs plot midway between EPR and the associated amphibolite, accounting for a contamination by volcanic materials, in addition to the hydrothermal influence during their oceanic deposition. The association of an oceanic setting with alkaline and tholeiitic magmatism is typical of the Algoma-type BIF deposit. The REE-rich BIFs indices recorded at Mafé are interpreted as resulting from an Archaean–Paleoproterozoic mineralization.  相似文献   

Temporal and spatial changes in grain size on a macro-tidal channel-flat complex: results from Kingsport,Nova Scotia,Bay of Fundy     

Law  Brent A.  Hill  Paul S.  Milligan  Timmothy G.  Zions  Vanessa 《Ocean Dynamics》2019,69(2):239-252

Ocean Dynamics - Understanding the processes that lead to seasonal changes in grain size on muddy macro-tidal flat and channel complexes will assist efforts to predict future changes caused by...  相似文献   

“Convoluted Journeys”: Integrating Nonprofit Organizations and University Science     

Vanessa Crossgrove Fry  Jen Schneider  Sally Sargeant-Hu  Carl Anderson  Erik Olson 《社会与自然资源》2019,32(3):239-254

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Late Miocene paleoenvironment of the Lambert Graben embayment, East Antarctica, evident from: Mollusc paleontology, sedimentology and geochemistry     

Jason M. Whitehead  Werner Ehrmann  David M. Harwood  Claus-Dieter Hillenbrand  Patrick G. Quilty  Charles Hart  Marco Taviani  Vanessa Thorn  Andrew McMinn 《Global and Planetary Change》2006,50(3-4):127-147

The Upper Miocene (10.7–9.0 Ma) Battye Glacier Formation was deposited 250 km inland from the modern Amery Ice Shelf edge in Prydz Bay, East Antarctica. The composition of clay minerals distinguishes a Lower Member, which reflects regional erosion of Precambrian metamorphic basement, from an Upper Member, which records increased erosion of local Permian–Triassic Amery Group strata. The Upper Member was deposited in an ice-proximal environment akin to the modern fjords of East Greenland, with substantial diamict deposition resulting from melting iceberg discharge. The Lower Member was deposited in an ice-distal environment and included the accumulation of the fossil-bearing McLeod Beds. The McLeod Beds contain much siliceous biogenic sediment (≤ 15% opal), which is rare to absent in the predominantly hemipelagic mud of modern East Greenland fjords. The McLeod Beds also contain largely monospecific in situ Hiatella sp. mollusc assemblages suggestive of environmental stress, potentially caused by low salinity melt-water and a high input of terrigenous sediment, which excluded most other benthic taxa. Geochemical results from primary aragonite in Hiatella shells imply large freshwater input into the marine environment during mollusc growth, causing low δ¹⁸O, Na, Mg and high Fe values. The present study indicates that iceberg melt-water influence entering the marine environment was greater during the Late Miocene than today around Antarctica, and documents the paleoenvironment associated with a discrete period of ice margin retreat and marine incursion into the Lambert embayment.  相似文献   

PAH transport by sinking particles in the open Mediterranean Sea: a 1 year sediment trap study   总被引：1，自引：0，他引：1  

Bouloubassi I  Méjanelle L  Pete R  Fillaux J  Lorre A  Point V 《Marine pollution bulletin》2006,52(5):560-571

One year time series of sinking particles were collected at two depths in the open Mediterranean Sea and analysed for polycyclic aromatic hydrocarbons (PAH). Average total PAH concentrations were 593+/-284 ng g(-1) at 250 m and 551 +/- 198 ng g(-1) at 2850 m. Total PAH fluxes averaged 73 +/- 58 ng m(-2) d(-1) at 250 m and 53 +/- 39 ng m(-2) d(-1) at 2850 m. Contamination levels and, thus, exposure of marine organisms to PAH are comparable in surface and deep waters. Deep waters appear as a significant, yet overlooked, PAH sink. PAH temporal patterns show noticeable seasonality. This is partly due to varying levels of specific components such as the winter increase of pyrolytic PAH. Downward transport processes and the nature of sinking particles also impact on PAH fluxes, as inferred during periods of increasing productivity. Different phase-associations and interactions with particulate organic carbon for low-MW fossil PAH and high-MW pyrolytic PAH influence their downward transport efficiency.  相似文献   

Using Multiple Methods to Understand the Nature of Relationships in Social Networks     

Vanessa M. Adams  Katie Moon  Jorge G. Álvarez-Romero  Örjan Bodin  Michaela Spencer  Deborah Blackman 《社会与自然资源》2018,31(7):755-772

Effective natural resource management (NRM) often depends on collaboration through formal and informal relationships. Social network analysis (SNA) provides a framework for studying social relationships; however, a deeper understanding of the nature of these relationships is often missing. By integrating multiple analytical methods (including SNA, evidence ratings, and perception matrices), we were able to investigate the nature of relationships in NRM social networks across five service types (e.g., technical advice, on-ground support) in our case study region, Daly catchment Australia. Only one service type was rated as highly associated with free choice in establishing relationships: technical advice/knowledge. Beneficial characteristics of NRM organizations, such as collaborative and transparent, were associated with the presence of freely chosen relationships between organizations. Our results suggest a need to improve our understanding of organizational roles and characteristics, in particular for use in applied NRM contexts, such as network weaving or disseminating information.  相似文献   

Disruption of Routine Behaviors Following the Deepwater Horizon Oil Spill     

Vanessa Parks  Leah Drakeford  Michael R. Cope  Tim Slack 《社会与自然资源》2018,31(3):277-290

This paper frames the unfolding impacts of the Deepwater Horizon oil spill as a process of lifeway disruption, analyzing the degree to which residents of spill affected communities were prevented from undertaking routine behaviors during the disaster. Special attention is paid to the influence of time, natural resource employment, and community sentiment. Drawing on data from the Louisiana Community Oil Spill Survey, the results show that people in the spill impacted region were prevented from engaging in routine behaviors, though this disruption has steadily decreased over time, suggesting a general trend toward recovery. Consistent with the renewable resource community concept, the results also show that those with ties to the fishing industry were more likely to be prevented from undertaking routine behaviors than were nonfishers. Finally, community sentiment is shown to ameliorate routine behavior disruption, thus, promoting resilience. Overall, these results challenge notions of monolithic paths to disaster recovery.  相似文献   

Competing Place Meanings in Complex Landscapes: A Social–Ecological Approach to Unpacking Community Conservation Outcomes on the Wild Coast,South Africa     

Vanessa Masterson  Maria Tengö  Marja Spierenburg 《社会与自然资源》2017,30(12):1442-1457

Despite a general awareness of the social–ecological complexities within which conservation interventions are embedded, approaches to understanding a diversity of local perspectives of heterogeneous landscapes and how they matter for the outcomes of these interventions are seldom demonstrated. We apply a social–ecological approach to exploring the multiple place meanings related to key landscape elements around a proposed community conservation intervention on the Wild Coast, South Africa, by identifying and analyzing three narratives about this impending change. These narratives mobilize competing meanings of the landscape to argue for or against the conservation project. By linking place meanings to locally defined landscape units (ecotopes), we engage multiple interpretations of the heterogeneous and changing landscape to gain a holistic and more inclusive picture of social–ecological landscape processes such as increasing woodlands and field abandonment. The obstruction of this particular intervention indicates the importance of engaging with multiple cultural values of nature.  相似文献   

A Chart for Judging Optimal Sample Spacing for Ore Grade Estimation     

Vanessa Cerqueira Koppe  Ricardo Hundelshaussen Rubio  João Felipe Coimbra Leite Costa 《Natural Resources Research》2017,26(2):191-199

Mineral deposit grades are usually estimated using data from samples of rock cores extracted from drill holes. Commonly, mineral deposit grade estimates are required for each block to be mined. Every estimated grade has always a corresponding error when compared against real grades of blocks. The error depends on various factors, among which the most important is the number of correlated samples used for estimation. Samples may be collected on a regular sampling grid and, as the spacing between samples decreases, the error of grade estimated from the data generally decreases. Sampling can be expensive. The maximum distance between samples that provides an acceptable error of grade estimate is useful for deciding how many samples are adequate. The error also depends on the geometry of a block, as lower errors would be expected when estimating the grade of large-volume blocks, and on the variability of the data within the region of the blocks. Local variability is measured in this study using the coefficient of variation (CV). We show charts analyzing error in block grade estimates as a function of sampling grid (obtained by geostatistical simulation), for various block dimensions (volumes) and for a given CV interval. These charts show results for two different attributes (Au and Ni) of two different deposits. The results show that similar errors were found for the two deposits, although they share similar features: sampling grid, block volume, CV, and continuity model. Consequently, the error for other attributes with similar features could be obtained from a single chart.  相似文献   

Reconstructing Phreatic Palaeogroundwater Levels in a Geoarchaeological Context: A Case Study in Flanders,Belgium     

Ann Zwertvaegher  Peter Finke  Jeroen De Reu  Alexander Vandenbohede  Luc Lebbe  Machteld Bats  Wim De Clercq  Philippe De Smedt  Vanessa Gelorini  Joris Sergant  Marc Antrop  Jean Bourgeois  Philippe De Maeyer  Marc Van Meirvenne  Jacques Verniers  Philippe Cromb 《Geoarchaeology》2013,28(2):170-189

The complex debate on prehistoric settlement decisions is no longer tackled from a purely archaeological perspective but from a more landscape‐oriented manner combined with archaeological evidence. Therefore, reconstruction of several components of the former landscape is needed. Here, we focus on the reconstruction of the groundwater table based on modeling. The depth of the phreatic aquifer influences, for example, soil formation processes and vegetation type. Furthermore, it directly influences settlement by the wetness of a site. Palaeogroundwater modeling of the phreatic aquifer was carried out to produce a series of full‐coverage maps of the mean water table depth between 12.7 ka and the middle of the 20th century (1953) in Flanders, Belgium. The research focuses on the reconstruction of the input data and boundary conditions of the model and the model calibration. The model was calibrated for the 1924–1953 time period using drainage class maps. Archaeological site data and podzol occurrence data act as proxies for local drainage conditions over periods in the past. They also served as a control on the simulated phreatic palaeogroundwater levels. Model quality testing on an independent validation data set showed that the model predicts phreatic water table levels at the time of soil mapping well (mean error of 1.8 cm; root mean square error of 65.6 cm). Simulated hydrological conditions were in agreement with the occurrence of archaeological sites of Mesolithic to Roman age at 96% of the validation locations, and also with the occurrence of well‐drained podzols at 97% of the validation locations.  相似文献