India & South Asia, 1850 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Hindoostan. It was published by Thomas, Cowperthwait & Co. in 1850. Scale [ca. 1:9,500,000]. Covers India, Sri Lanka, Bangladesh, Nepal, and portions of Maldives, Afghanistan, Pakistan, China, and Bhutan. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Kalianpur 1975 India Zone III projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, territorial and colonial boundaries, shoreline features, and more. Relief shown by hachures. Includes also inset: Delta of the Ganges.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Chemical and isotopic compositions of pore fluids from ODP Sites 169-1034 and 169-1037

We have analysed the concentrations of Li, K, Rb, Cs, and B, and the isotopic ratios of Li and B of a suite of pore fluids recovered from ODP Sites 1037 (Leg 169; Escanaba Trough) and 1034 (Leg 169S; Saanich Inlet). In addition, we have analysed dissolved K, Rb, and Cs concentrations for estuarine mixing of the Ganges-Brahmaputra river system. Together, these data sets have been used to assess the role of sediments in the marine geochemical cycles of the alkali elements and boron. Uptake onto clay minerals during estuarine mixing removes 20-30% of the riverine input of dissolved Cs and Rb to the oceans. Prior to this study, the only other recognised sink of Rb and Cs was uptake during low-temperature alteration of the oceanic crust. Even with this additional sink there is an excess of inputs over outputs in their modern oceanic mass balance. Pore fluid data show that Li and Rb are transferred into marine sediments during early diagenesis. However, modeling of the Li isotope systematics of the pore fluids from Site 1037 shows that seawater Li taken up during marine sedimentation can be readily returned to solution in the presence of less hydrated cations, such as NH4+. This process also appears to result in high concentrations of pore fluid Cs (relative to local seawater) due to expulsion of adsorbed Cs from cation exchange sites. Flux calculations based on pore fluid data for a series of ODP sites indicate that early diagenesis of clay sediments removes around 8% of the modern riverine input of dissolved Li. Although NH4+-rich fluids do result in a flux of Cs to the oceans, on the global scale this input only augments the modern riverine Cs flux by ~3%. Nevertheless, this may have implications for the fate of radioactive Cs in the natural environment and waste repositories.

Crimes célèbres,

t. 1. Les Cenci. La marquise de Brinvilliers. Karl Ludwig Sand. Marie Stuart [1. ptie.]--t. 2. Marie Stuart [2. ptie.] La marquise de Ganges (1. Ptie.)--t. 3. La marquise de Ganges (2. ptie.) Murat. Les Borgia (1. ptie.)--t. 4. Les Borgia (suite) Urbain Grandier. Vaninka.--t. 5. Massacres du Midi (1. ptie.)--t. 6. Massacres du Midi (2. ptie.) La comtesse de Saint-Géran. Jeanne de Naples. Nisida [1. ptie.]--t. 7. Nisida (2. ptie.) Derues. Martin Guerre. Ali-Pacha (1. ptie.)--t. 8. Ali-Pacha (2. ptie.) La Constantin. L'homme au masque de fer.

Geschichte des Alterthums.

cont. 6. Bd. Das neue Fürstenthum und die unteren Stände. Die Befestigung der Aristokratie in Sparta und die Entwickelung der Demokratie in Athen. 3.5. Aufl. 1882.--7. Bd. Die Angriffe der Perser und der Karthager. 3.-5. Aufl. 1882.--8. Bd. (n. f. 1. Bd.) Die Gründung der Macht Athens und der erste Krieg mit den Peloponnesiern. 1884.--9. Bd. (n. f. 2. Bd.) Die Staatsleitung des Perikles. 1886.

Manuel et son temps; Étude sur l'opposition parlementaire sous la restauration.

Mode of access: Internet.

The crimes of the Marquise de Brinvilliers and others;

Introduction.--The Marquise de Brinvilliers.--Martin Guerre.--The Marquise de Ganges.--Mary Stuart.--Vaninka.

Celebrated crimes,

Plates accompanied by guard sheets with descriptive letterpress.

Mineralogy of northern Indian Ocean surface sediments and of suspended sediments of Indian rivers (Table 2 and 5)

The solid phases from surface sediments, atmospheric dusts, and rivers of the Indian Ocean environment have been analyzed for their clay minerals and quartz. Such data have been used to delimit the transport paths and sources of the detrital minerals in the oceanic deposits. Diagnostic in distinguishing fluvial and eolian inputs to the northern Indian Ocean is a combination of the clay mineral assemblages and of their geographic distributions. River borne solids are the primary components of the Bay of Bengal deposits. The eastern part receives its continental input through the Ganges-Brahmaputra river system, while drainage of the Indian Peninsula by rivers introduces solids to the western part. The former materials are characterized by high illite and chlorite in the clay mineral assemblages; the latter by montmorillonite. The winds over the Bay bear distinctive dust burdens based upon their directions. However, their contributions to the sediments are insignificant. The eastern sector of the Arabian Sea receives major contributions of continental debris from the rivers and the high montmorillonite levels clearly indicate a source in the Indian Peninsula. The rest of the Sea appears to receive most of its land-derived materials from the north, perhaps the desert regions of northern India and West Pakistan, and they are wind-borne. These materials are also transported to the equatorial regions of the Indian Ocean. A gradient in attapulgite, just north of the equator, may indicate an eolian contribution to the Arabian Sea from the African continent. The halogenated hydrocarbon pesticides were assayed in the southwest monsoon winds and enter the Bay of Bengal at levels of a half ton per month, an amount comparable to those introduced by other wind and river systems to the marine environment.

Bulk and amino acid parameters of core SO188-342KL from the Northern Bay of Bengal for the last 18 ka

The Northern Bay of Bengal (NBoB) is a globally important region for deep-sea organic matter (OM) deposition due to massive fluvial discharge from the Ganges-Brahmaputra-Meghna (G-B-M) rivers and moderate to high surface productivity. Previous studies have focused on carbon burial in turbiditic sediments of the Bengal Fan. However, little is known about the storage of carbon in pelagic and hemipelagic sediments of the Bay of Bengal over millennial time scales. This study presents a comprehensive history of OM origin and fate as well as a quantification of carbon sediment storage in the Eastern Bengal Slope (EBS) during the last 18 ka. Bulk organic proxies (TOC, TIC, TN, d13CTOC, d15NTN) and content and composition of total hydrolysable amino acids (THAA) in a sediment core (SO188-342KL) from the EBS were analyzed. Three periods of high OM accumulation were identified: the Late Glacial (LG), the Bölling/Alleröd (B/A), and the Early Holocene Climatic Optimum (EHCO). Lower eustatic sea level before 15 ka BP allowed a closer connection between the EBS and the fluvial debouch, favoring high terrestrial OM input to the core site. This connection was progressively lost between 15 and 7 ka BP as sea level rose to its present height and terrestrial OM input decreased considerably. Export and preservation of marine OM was stimulated during periods of summer monsoon intensification (B/A and EHCO) as a consequence of higher surface productivity enhanced by cyclonic-eddy nutrient pumping and fluvial nutrient delivery into the photic zone. Changes in the THAA composition indicate that the marine plankton community structure shifted from calcareous-dominated before 13 ka BP to siliceous-dominated afterwards. They also indicate that the relative proportion of marine versus terrestrial OM deposited at site 342KL was primarily driven by relative sea level and enlarged during the Holocene. The ballasting effect of lithogenic particles during periods of high coastal proximity and/or enhanced fluvial discharge promoted the export and preservation of OM. The high organic carbon accumulation rates in the EBS during the LG (18-17 ka BP) were 5-fold higher than at present and comparable to those of glacial upwelling areas. Despite the differences in sediment and OM transport and storage among the Western and Eastern sectors of the NBoB, this region remains important for global carbon sequestration during sea level low-stands. In addition, the summer monsoon was a key promotor of terrestrial and marine OM export to the deep-ocean, highlighting its relevance as regulator of the global carbon budget.

Una década de planes de movilidad urbana sostenible en España 2004-2014

Los Planes de Movilidad Urbana Sostenible (PMUS) son una herramienta de reciente implantación en España que en la última década se ha desarrollado en un buen número de municipios. El objetivo es conocer cuál ha sido la dimensión territorial y el impacto que este instrumento de planificación de la movilidad ha tenido en nuestro país entre los años 2004 y 2014. Como resultado se ha logrado describir el panorama de los PMUS en España y su evolución durante esta última década en cada una de las Comunidades Autónomas.

Compositional data analysis of Holocene sediments from the West Bengal Sundarbans, India: Geochemical proxies for grain-size variability in a delta environment

This paper is part of a special issue of Applied Geochemistry focusing on reliable applications of compositional multivariate statistical methods. This study outlines the application of compositional data analysis (CoDa) to calibration of geochemical data and multivariate statistical modelling of geochemistry and grain-size data from a set of Holocene sedimentary cores from the Ganges-Brahmaputra (G-B) delta. Over the last two decades, understanding near-continuous records of sedimentary sequences has required the use of core-scanning X-ray fluorescence (XRF) spectrometry, for both terrestrial and marine sedimentary sequences. Initial XRF data are generally unusable in ‘raw-format’, requiring data processing in order to remove instrument bias, as well as informed sequence interpretation. The applicability of these conventional calibration equations to core-scanning XRF data are further limited by the constraints posed by unknown measurement geometry and specimen homogeneity, as well as matrix effects. Log-ratio based calibration schemes have been developed and applied to clastic sedimentary sequences focusing mainly on energy dispersive-XRF (ED-XRF) core-scanning. This study has applied high resolution core-scanning XRF to Holocene sedimentary sequences from the tidal-dominated Indian Sundarbans, (Ganges-Brahmaputra delta plain). The Log-Ratio Calibration Equation (LRCE) was applied to a sub-set of core-scan and conventional ED-XRF data to quantify elemental composition. This provides a robust calibration scheme using reduced major axis regression of log-ratio transformed geochemical data. Through partial least squares (PLS) modelling of geochemical and grain-size data, it is possible to derive robust proxy information for the Sundarbans depositional environment. The application of these techniques to Holocene sedimentary data offers an improved methodological framework for unravelling Holocene sedimentation patterns.

El pensamiento religioso de Fernando Sánchez Dragó

Fernando Sánchez Dragó pertenece por edad a la generación de 1956, aunque por afinidad está más cerca de la siguiente, la de 1968, una generación iconoclasta, nihilista y anarquista. Hay a su alrededor un grupo de intelectuales muy conocidos situados dentro de la contracultura (Salvador Pániker, Luis Racionero, Antonio Escohotado, Ramiro Calle, Pepa Roma y Fernando Díez), que sufren por primera vez una influencia directa de las religiones orientales al tiempo que experimentan con drogas visionarias. Un día de marzo de 1967 sufre una experiencia de conversión en Benarés mientras contempla el Ganges, que hará que sienta lo sagrado a partir de entonces a la manera oriental. Descubre el mundo de los hippies y se inicia en la “ebriedad sagrada” de las drogas enteogénicas, que le abren las puertas de la percepción. La lectura de de Carl Gustav Jung hace surgir en él la idea de escribir el libro que le hará famoso, Gárgoris y Habidis. Una historia mágica de España, que indaga en el inconsciente colectivo de los españoles mediante la búsqueda de sus arquetipos. Frente a los demás compañeros de la generación de 1968, que rompen con la tradición española, él decide emprender un viaje de signo contrario en dirección al pasado en busca de un sentido religioso del mundo y de la vida en la España antigua, hasta descubrir una tradición que además es esotérica y heterodoxa, pero que con el paso del tiempo terminará por imaginar como una invención suya que nunca existió...