998 resultados para Pausanias, fl. ca. 150-175


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A treatise on washing and wiping feet in ritual ablution.

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With this is bound: Itḥāf al-murīdīn li-ʻaqīdat Umm al-burhān / Aḥmad ibn ʻAbd Allāh ibn Abī Bakr al-Ghadāmisī (ff. 29v-128r) -- Ḥāshiyah ʻalā al-ʻAqīdah al-Sanūsīyah / Muḥammad ibn Abī al-Qāsim ibn Naṣr al-Thawrī (ff. 129v-164r) -- al-Durrah al-mushayyadah fī sharḥ al-Murshidah / Muḥammad ibn ʻAbbād al-Tilimsānī (ff. 165v-199v) -- Ightinām al-fawāʼid bi-sharḥ Qawāʻid al-ʻaqāʼid / Aḥmad ibn Aḥmad Zarrūq (ff. 200v-229v).

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Bound with: Sharḥ al-ʻAqīdah al-Sanūsīyah / Muḥammad al-Maʼmūn ibn Muḥammad al-Ḥafṣī (ff. 1v-28v).

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Bound with: al-Maqṣūd al-maḥmūd fī talkhīṣ al-wathāʼiq wa-al-ʻuqūd / ʻAlī ibn Yaḥyá al-Jazīrī.

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Bound with: Sharḥ al-ʻAqīdah al-Sanūsīyah / Muḥammad al-Maʼmūn ibn Muḥammad al-Ḥafṣī (ff. 1v-28v).

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Title supplied by cataloger.

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Marriage ritual in Arabic, the Story of the fast of Satī Mā also known as the fast of Maulā ʻAlī, a Prayer to be recited during ceremony for the forgiveness of sin on the Great Day (the Day of Judgement), the short kalimah or testimony of faith and the long kalimah.

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Local paper. Pages slightly discolored.

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We compare a new mid-Pleistocene sea surface temperature (SST) record from the eastern tropical Atlantic to changes in continental ice volume, orbital insolation, Atlantic deepwater ventilation, and Southern Ocean front positions to resolve forcing mechanisms of tropical Atlantic SST during the mid-Pleistocene transition (MPT). At the onset of the MPT, a strong tropical cooling occurred. The change from a obliquity- to a eccentricity-dominated cyclicity in the tropical SST took place at about 650 kyr BP. In orbital cycles, tropical SST changes significantly preceded continental ice-volume changes but were in phase with movements of Southern Ocean fronts. After the onset of large-amplitude 100-kyr variations, additional late glacial warming in the eastern tropical Atlantic was caused by enhanced return flow of warm waters from the western Atlantic driven by strong trade winds. Pronounced 80-kyr variations in tropical SST occurred during the MPT, in phase with and likely directly forced by transitional continental ice-volume variations. During the MPT, a prominent anomalous long-term tropical warming occurred, likely generated by extremely northward displaced Southern Ocean fronts. While the overall pattern of global climate variability during the MPT was determined by changes in mean state and frequency of continental ice volume variations, tropical Atlantic SST variations were primarily driven by early changes in Subantarctic sea-ice extent and coupled Southern Ocean frontal positions.

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Mg/Ca, Sr/Ca, and stable isotope measurements have been performed on tests from the planktonic foraminifers Globigerinoides ruber (white), Globigerina bulloides, and Neogloboquadrina pachyderma (right coiling) in samples from Ocean Drilling Program site 977A in the Alboran Sea (Western Mediterranean). The evolution of different water masses between 250 and 150 ka is described. Warm substages were characterized by strong seasonality and thermal stratification of the water column. By contrast, less pronounced seasonality and basin stratification seem to prevail during cold substages. Several periods of stratification due to the low salinity of the upper water mass occurred during the formation of organic-rich layers and also during a possible Heinrich-like event at 220 ka. The three foraminifer species studied show a common and large shell Sr/Ca variability in short timescales, suggesting changes in the global ocean Sr/Ca ratio as one of the main causes of variations in shell composition.