al- Jawhar al-munaḍḍad fī maʻná Qul huwa Allāhu aḥad / li-muʼallifihā Aḥmad ibn Aḥmad ibn Aḥmad al-Biqāʻī al-Dimashqī al-Ṣūfī : manuscript, 1641

A Sufi commentary on Chapter 112 of the Qur'an.

Risālah fī al-īmān wa-al-islām : manuscript, 1743

Title supplied by cataloger.

Namāz : manuscript, 1858-1865

Ritual Prayer in Arabic with instructions on number of prostration cycles (rakaʻahs) to be performed during each of the five prayer times.

ejī:harī:nāme:harī:jāṇī:e : manuscript, 1829?

Title provided by cataloger.

[ Ghaṭpāṭjī dhoā]

Prayers to be recited during the ghaṭpāṭ ceremony; prayer includes recitation of the name of Ismāʻīlī Imāms as well as those of Pīrs.

[ Four ginān books

Pīr Imām Shāh ... [et al.]].

[ Three ginān books

Pīr Imām Shāh ... [et al.]].

How much did China’s WTO accession increase economic growth in resource-rich countries? CEPS Working Document No. 384, 3 October 2013

This Working Document provides an estimate of China’s impact on the growth rate of resource-rich countries since its WTO accession in December 2001. The authors’ empirical approach follows the logic of the differences-in-differences estimator. In addition to temporal variation arising from the WTO accession, which they argue was exogenous to other countries’ growth trajectories, the authors exploit spatial variation arising from differences in natural resource wealth. In this way they can compare changes in economic growth in the pre- and post-accession periods between countries that benefited from the surge in demand for industrial commodities brought about by China’s WTO accession and countries that were less able to do so. They find that that roughly one-tenth of the average annual post-accession growth in resource-rich countries was due to China’s increased appetite for commodities. The authors use this finding to inform the debate about what will happen to economic growth in resource-rich countries as China rebalances and its demand for commodities weakens.

(Tab. XIII.1) TOC content, carbonate content, carbonate mineralogy, percentage of total carbonate, aragonite, low magnesium calcium, and high magnesium calcium, and grain-size contents from samples from the Golfe d'Arguin and from the Western Sahara

Modern carbonate sedimentation takes place on the northern Mauritanian shelf (20°N), where typical tropical components (e.g. hermatypic reefs, calcareous green algae) are absent. Such deposits are reminiscent of extratropical sediment in the geological record. The tropical open shelf of Mauritania is influenced by large siliciclastic dust input and upwelling, highly fertilizing the ocean, as well as strongly limiting the light penetration. In this context, temperature does not appear to be the steering factor of carbonate production. This thesis describes the depositional system of the Golfe d'Arguin off Mauritania and focuses on environmental conditions that control the depositional pattern, in particular carbonate production. The description of this modern analogue provides a tool for paleoenvironmental interpretation of ancient counterparts. The Golfe d'Arguin is a broad shallow shelf comprising extensive shoals (<10 m water depth; i.e. the Banc d'Arguin) on the inner shelf where waters warm up. The sediments collected in water depths between 4 and 600 m are characterized by mixed carbonate and siliciclastic (dust) deposits. They vary from clean coarse-grained, almost pure carbonate loose sediments to siliciclastic-dominated fine-grained sediments. The carbonate content and sediment grain size show a north-south decreasing pattern through the Golfe d'Arguin and are controlled by the hydraulic regime influenced by wind-driven surface currents, swell, and tidal currents. The carbonate grain association is heterozoan. Components include abundant molluscs, foraminifers, and worm tubes, as well as barnacles and echinoderms, elements that are also abundant in extratropical sediments. The spatial distribution of the sedimentary facies of the Golfe d'Arguin does not display a depth zonation but rather a mosaic (i.e. patchy distribution). The depth and climatic signatures of the different sedimentary facies are determined by taxonomic and ecological investigations of the carbonate-secreting biota (molluscs and foraminifers). While certain planktonic foraminifers and molluscs represent upwelling elements, other components (e.g. mollusc and benthic foraminifer taxa) demonstrate the tropical origin of the sediment. The nutrient-rich (and thus also low light-penetration) conditions are reflected in the fact that symbiotic and photosynthetic carbonate-producing organisms (e.g. hermatypic corals) are absent. The Mauritanian deposits represent an environment that is rare in the modern world but might have been more common in the geological past when global temperatures were higher. Taxonomic and ecological studies allow for distinguishing carbonate sediments formed under either tropical high-nutrient or extratropical conditions, thus improving paleoclimate reconstruction.