Hādhā kitāb Ḥusn al-muḥāḍarah fī akhbār Miṣr wa-al-Qāhirah / lil-Imām al-Mujtahid al-Ḥafīẓ Jalāl al-Dīn ʻAbd al-Raḥmān al-Asyūṭī : manuscript, 1844

Vol. 1 of a multi-volume set.

Kitāb Mufarriḥ al-nafs / taṣnīf al-Imām al-ʻālim al-fāḍil Sharaf al-Dīn Abī Naṣr Muḥammad ibn ʻUmar ibn Abī al-Futūḥ al-Baghdādī thumma al-Māridīnī al-maʻrūf bi-Ibn al-Marah : manuscript, [ca. 1530]

The author's name appears as ابن المره in title page (f. 1r) and ابن المراه at the beginning of the book (f. 1v).

Kitāb al-Barāhīn al-jalīyah fī ʻilm al-kalām / li-jāmiʻihā al-ʻabd al-ḥaqīr Muḥammad Rashīd Qazīhā al-shahīr bi-Ibn Sinān : manuscript, 1896

Paginated 1-32.

(Table 1) I, Br, B, d11B and Mn concentrations in ODP Site 131-808

This study of the interstitial water concentration-depth distributions of iodide, bromide, boron, d11B, and dissolved organic carbon, as represented by absorbance at 325 nm (yellow substance: YS) and laser-induced fluorescence (LIF), is a follow-up of the extensive shipboard program of interstitial water analysis during ODP Leg 131. Most of the components studied are associated with processes involving the diagenesis of organic matter in these sediments. Three zones of the sediment column are discussed separately because of the different processes involved in causing concentration changes: 1. The upper few hundreds of meters: In this zone, characterized by very high sedimentation rates (>1200 m/m.y.), interstitial waters show very sharp increases in alkalinity, ammonia, iodide, bromide, YS, and LIF, mainly as a result of the diagenesis of organic carbon; 2. Whereas below 200 mbsf concentration gradients all show a decreasing trend, the zone at ~ 365 mbsf is characterized by concentration reversals, mainly due to the recent emplacement of deeper sediments above this depth as a result of thrust-faulting; 3. The décollement zone (945-964 mbsf) is characterized by concentration anomalies in various constituents (bromide, boron, d11B, manganese, LIF). These data are interpreted as resulting from an advective input of fluids along the zone of décollement as recent as ~ 200 ka. Possibly periodic inputs of anomalous fluids still seem to occur along this décollement zone.

Dinoflagellate cyst abundances at DSDP Site 94-607 from the North Atlantic (Appendix B)

The climatic deterioration related to the onset of Northern Hemisphere glaciations (circa 2.52 Ma BP) must have lead to reorganization and relocation of species associations and may have enhanced species turnover. The present study investigates how this deterioration affects the dinoflagellate cyst and acritarch assemblages from two locations, DSDP Site 607 (North Atlantic) and the Singa section (southern Italy). The records from these locations cover the interval from 2.8 to 2.2 Ma with at least a 5 ka resolution and they have been correlated to the Milankovitch periodicities on a cycle to cycle basis by means of integrated high resolution stable isotope, calcium carbonate, foraminiferal, palynological and magnetostratigraphical datasets. In the present study this high resolution stratigraphic framework is used for a detailed correlation of events occurring in each of the depositional sequences. It also enables further assessment of the palaeoenvironmental preferences of some dinoflagellate cyst forms. Comparison of the two palynological records reveals a close correspondence in the timing of major assemblage changes and extinction events, confirming their Milankovitch cycle based correlation. A close link between periods of Northern Hemisphere cooling (at oxygen isotope stages 110, 104 and 100-96) and increased dinoflagellate cyst turnover appears to be present for both DSDP Site 607 and the Singa section. The turnover events can also be recognized in the records of planktic foraminifera and calcamous nannoplankton. Comparison of the Singa section with Site 607 and with other time equivalent marine palynological data sets, shows that some oceanic taxa respond similarly over a large area. The biostratigraphical implications are discussed. Notably the last occurrence of Invertocystu lucrymosa appears to be a valuable marker for isotope stage 110 in the Mediterranean and North Atlantic.

Amphora, Side B, Dionysus with Hunters

Amasis Painter; H: 1 ft. 4 17/32 in.; black figure; terracotta

Final report to Congress, The Streambank Erosion Control Evaluation and Demonstration Act of 1974, Section 32, Public Law 93-251 : Main report, supplemented by appendices A-H in separate volumes /

Main report -- Appendix A. Literature survey -- Appendix B. Hydraulic research -- Appendix C. Geotechnical research -- Appendix D. Ohio River demonstration projects -- Appendix F. Missouri River demonstration projects (2 v.) -- Appendix F. Yazoo River Basin demonstration projects -- Appendix G. Demonstration projects on other streams, nationwide (2 v.) -- Appendix H. Evaluation of existing projects (2 v.).

Tsurukame ; Mekari ; Ōyashiro ; Tōbōsaku ; Shun'ei /

"Meiji 32-nen... shuppan ontodokezumi"--Colophon.

Sacra plausible diadema, vistosamente texida de las mas selectas flores del pensil ameno del Parnaso ... con la que, ... la religion de Clerigos Reglares, ministros de los enfermos agonizantes ... corona a su patriarcha y fundador el B. Camilo de Lelis en ... su beatificacion ... /

Mode of access: Internet.

Prodigiosa vida del muy ilustre varón y extático heroe comunmente conocido por el P. de la Caridad y por el Predicador del Amor de Dios, el B.P. Francisco Caraciolo, fundador de la sagrada orden de los Clérigos Menores /

Mode of access: Internet.

TDP : a two-dimensional perturbation calculation code based on TDC, for IBM-7090, Deck B 516 /

Work performed at CANEL.

The voyages of Captain Luke Foxe of Hull and Captain Thomas James of Bristol in search of a Northwest Passage in 1631-32, with narratives of the earlier northwest voyages of Frobisher, David, Weymouth, Hall, Knight, Hudson, Button, Gibbons, Bylot, Baffin, Hawkridge, and others,

Mode of access: Internet.