The Silurian rocks of the Tortworth Inlier,Gloucestershire     

M.L.K. Curtis 《Proceedings of the Geologists' Association. Geologists' Association》1972,83(1):1-35

The Silurian succession in the Tortworth Inlier includes strata belonging to the three main divisions of the System. The Upper Llandovery, which rests unconformably on Tremadoc beds, consists of about 700 ft. (213 m.) of fine-grained sandstones, mudstones and shales with two igneous bands. The Wenlock Series is represented by some 800 ft. (244 m.) of mudstones, siltstones and calcareous sandstones with impersistent limestone bands at various horizons. The Ludlow succession is incomplete, but at least 300 ft. (91 m.) of mudstones, siltstones and fine-grained sandstones are present, and they pass up conformably into the Downtonian.  相似文献   

Oil/source rock correlations in the Polish Flysch Carpathians and Mesozoic basement and organic facies of the Oligocene Menilite Shales: insights from hydrous pyrolysis experiments     

John B. Curtis  Maciej J. Kotarba  Michael D. Lewan  Dariusz Wi&#x;c&#x;aw 《Organic Geochemistry》2004,35(11-12):1573

The Oligocene Menilite Shales in the study area in the Polish Flysch Carpathians are organic-rich and contain varying mixtures of Type-II, Type-IIS and Type-III kerogen. The kerogens are thermally immature to marginally mature based on atomic H/C ratios and Rock-Eval data. This study defined three organic facies, i.e., sedimentary strata with differing hydrocarbon-generation potentials due to varying types and concentrations of organic matter. These facies correspond to the Silesian Unit and the eastern and western portions of the Skole Unit. Analysis of oils generated by hydrous pyrolysis of outcrop samples of Menilite Shales demonstrates that natural crude oils reservoired in the flysch sediments appear to have been generated from the Menilite Shales. Natural oils reservoired in the Mesozoic basement of the Carpathian Foredeep appear to be predominantly derived and migrated from Menilite Shales, with a minor contribution from at least one other source rock most probably within Middle Jurassic strata. Definition of organic facies may have been influenced by the heterogeneous distribution of suitable Menilite Shales outcrops and producing wells, and subsequent sample selection during the analytical phases of the study.  相似文献   

Estimating forest biomass using small footprint LiDAR data: An individual tree-based approach that incorporates training data   总被引：1，自引：0，他引：1  

Zachary J. Bortolot  Randolph H. Wynne   《ISPRS Journal of Photogrammetry and Remote Sensing》2005,59(6):824

A new individual tree-based algorithm for determining forest biomass using small footprint LiDAR data was developed and tested. This algorithm combines computer vision and optimization techniques to become the first training data-based algorithm specifically designed for processing forest LiDAR data. The computer vision portion of the algorithm uses generic properties of trees in small footprint LiDAR canopy height models (CHMs) to locate trees and find their crown boundaries and heights. The ways in which these generic properties are used for a specific scene and image type is dependent on 11 parameters, nine of which are set using training data and the Nelder–Mead simplex optimization procedure. Training data consist of small sections of the LiDAR data and corresponding ground data. After training, the biomass present in areas without ground measurements is determined by developing a regression equation between properties derived from the LiDAR data of the training stands and biomass, and then applying the equation to the new areas. A first test of this technique was performed using 25 plots (radius = 15 m) in a loblolly pine plantation in central Virginia, USA (37.42N, 78.68W) that was not intensively managed, together with corresponding data from a LiDAR canopy height model (resolution = 0.5 m). Results show correlations (r) between actual and predicted aboveground biomass ranging between 0.59 and 0.82, and RMSEs between 13.6 and 140.4 t/ha depending on the selection of training and testing plots, and the minimum diameter at breast height (7 or 10 cm) of trees included in the biomass estimate. Correlations between LiDAR-derived plot density estimates were low (0.22 ≤ r ≤ 0.56) but generally significant (at a 95% confidence level in most cases, based on a one tailed test), suggesting that the program is able to properly identify trees. Based on the results it is concluded that the validation of the first training data-based algorithm for determining forest biomass using small footprint LiDAR data was a success, and future refinement and testing are merited.  相似文献   

The significance of European high mountain lakes in critical load distributions at the EMEP grid scale     

Chris J. Curtis  Max Posch  Pilar Casals-Carrasco  Jordi Catalan  Mike Hughes  Martin Kernan  Marc Ventura 《Aquatic Sciences - Research Across Boundaries》2005,67(3):252-262

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Web-based service of a visualization package “Amira” for the geosciences     

Yunsong Wang  Gordon Erlebacher  Zachary A. Garbow  David A. Yuen 《Visual Geosciences》2005,10(1):43

Amira is a powerful three-dimensional visualization package that has been employed recently by the science and engineering communities to gain insight into their data. We discuss a new paradigm for the use of Amira in the Earth sciences that relies on the client-server paradigm. We have developed a module called WEB-IS2, which provides web-based access to Amira. This tool allows Earth scientists to manipulate Amira controls remotely and to analyze, render and view large datasets through the Internet without regard for time or location. This could have important ramifications for GRID computing.  相似文献   

Geochemical and biological consequences of groundwater augmentation in lakes of west-central Florida (USA)     

Mark Brenner  Thomas J. Whitmore  Melanie A. Riedinger-Whitmore  Brandy DeArmond  Douglas A. Leeper  William F. Kenney  Jason H. Curtis  Byron Shumate 《Journal of Paleolimnology》2006,36(4):371-383

We studied sediment cores from four Florida (USA) lakes that have received groundwater hydrologic supplements (augmentation) for >30 years to maintain lake stage. Top samples (0–4 cm) from sediment cores taken in Lakes Charles, Saddleback, Little Hobbs, and Crystal had ²²⁶Ra activities of 44.9, 17.5, 7.6, and 8.5 dpm g⁻¹, respectively, about an order of magnitude greater than values in deeper, older deposits. The surface sample from Lake Charles yielded the highest ²²⁶Ra activity yet reported from a Florida lake core. Several lines of evidence suggest that groundwater augmentation is responsible for the high ²²⁶Ra activities in recent sediments: (1) ²²⁶Ra activity in cores increased recently, (2) the Charles, Crystal, and Saddleback cores display ²²⁶Ra/²¹⁰Pb disequilibrium at several shallow depths, suggesting ²²⁶Ra entered the lakes in dissolved form, (3) cores show recent increases in Ca, which, like ²²⁶Ra, is abundant in augmentation groundwater, and (4) greater Sr concentrations are associated with higher ²²⁶Ra activities in recent Charles and Saddleback sediments. Sr concentrations in Eocene limestones of the deep Floridan Aquifer are high relative to Sr concentrations in surficial quartz sands around the lakes. Historical water quality inferences for the lakes were based on diatom assemblages in sediments. Recent alkalization in Lakes Charles, Saddleback, Little Hobbs, and Crystal was inferred from weighted-averaging calibration (WACALIB). The lakes also show recent trophic state increases based on WACALIB-derived estimates for limnetic total P. Although residential and agricultural sources might contribute to increased P loading, P in augmentation waters probably has had significant influence on eutrophication. Dystrophic diatoms were abundant in the early history of Lakes Saddleback, Little Hobbs, and Crystal, which suggests that these lakes contained more tannic waters during the past than at present, perhaps as a consequence of greater inflows from surrounding wetlands. Ionic content of lake waters increased, as indicated by diatom autecological analysis. Recent geochemical and biological changes detected in cores from these lakes probably are a result of deliberate groundwater augmentation, although inputs of groundwater pumped for agricultural and residential development in the watersheds also might have contributed to limnological changes.  相似文献   

A multi-proxy study of Holocene environmental change in the Maya Lowlands of Peten, Guatemala     

Jason H. Curtis  Mark Brenner  David A. Hodell  Richard A. Balser  Gerald A. Islebe  Henry Hooghiemstra 《Journal of Paleolimnology》1998,19(2):139-159

We used multiple variables in a sediment core from Lake Peten-Itza, Peten, Guatemala, to infer Holocene climate change and human influence on the regional environment. Multiple proxies including pollen, stable isotope geochemistry, elemental composition, and magnetic susceptibility in samples from the same core allow differentiation of natural versus anthropogenic environmental changes. Core chronology is based on AMS ¹⁴C measurement of terrestrial wood and charcoal and thus avoids the vagaries of hard-water-lake error. During the earliest Holocene, prior to 9000 ¹⁴C yr BP, the coring site was not covered by water and all proxies suggest that climatic conditions were relatively dry. Water covered the coring site by 9000 ¹⁴C yr BP, coinciding with filling of other lakes in Peten and farther north on the Yucatan Peninsula. During the early Holocene (9000 to 6800 ¹⁴C yr BP), pollen data suggest moist conditions, but high ¹⁸O values are indicative of relatively high E/P. This apparent discrepancy may be due to a greater fractional loss of the lake's water budget to evaporation during the early stages of lake filling. Nonetheless, conditions were moist enough to support semi-deciduous lowland forest. Decrease in ¹⁸O values and associated change in ostracod species at 6800 ¹⁴C yr BP suggest a transition to even moister conditions. Decline in lowland forest taxa beginning 5780 ¹⁴C yr BP may indicate early human disturbance. By 2800 ¹⁴C yr BP, Maya impact on the environment is documented by accelerated forest clearance and associated soil erosion. Multiple proxies indicate forest recovery and soil stabilization beginning 1100 to 1000 ¹⁴C yr BP, following the collapse of Classic Maya civilization.  相似文献   

Age of the Thornton Beach, California, Mammoth Fossil Updated     

Andrei M. Sarna-Wojcicki  Charles E. Meyer  John W. Hillhouse  N. Timothy Hall  Garniss H. Curtis 《Quaternary Research》1996,45(3):327-331

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The Zone Definition Problem in Survey Research: An Empirical Example from New York State*     

Andrew J. Curtis  Alan D. MacPherson 《The Professional geographer》1996,48(3):310-320

This paper examines problems of zonal definition in the context of a recent empirical project on the geography of inter-firm linkages in New York State. It is argued that the results of a spatially structured survey of private companies can change significantly depending on the manner in which the study regions of the analysis are defined. Variations in the composition of study regions are a result of either changes in spatial scale, or spatial zoning at any one scale. This point is illustrated with data from 472 New York State manufacturing firms aggregated into four different zonal systems. The results of the analysis suggest that misleading interpretations of spatial data can emerge, even when logical boundaries are selected from the outset.  相似文献   

Electoral Geography of the Sino-Thai in Thailand's National Elections, 1979–1995     

Curtis N. Thomson 《The Professional geographer》1996,48(4):392-404

Comparison of Thai and Sino-Thai participation and success rates from the seven elections taking place since 1979 show Sino-Thai participation comparable to their proportion in the country's population. Assimilationist government minority policy and electorate acceptance have served to integrate this group into the mainstream political system. There is no pattern of support for a particular political party and there are no indicators of a separate Sino-Thai political element. Their highest success rates, however, occur in regions of the country that have historically had small Sino-Thai populations. This appears to be the result of factional politics and of monetary and organizational resources needed to garner votes at the provincial level.  相似文献