756 resultados para Gh
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taʼlīf ʻAbd al-Qādir al-Shafshāwanī.
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Foliated 1-442. Missing f. 441.
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Commentary on the Īsāghūjī [Isagoge], "Introduction to logic", by al-Abharī.
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Bound with: Ghāyat al-ghawr fī dirāyat al-dawr (ff. 1r-7r).
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Copy completed in Jumādá al-Ākhirah 1192 [June 26-July 24, 1778] in the hand of Muḥammad Amīn ibn ʻAlī ibn Ḥusayn ibn Muḥammad Qāsim.
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According to colophon, Manṣūr Handal al-ʻAdawī al-Mālikī copied the book for himself.
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Copy completed 13 Ramaḍān 1108 [April 5, 1697] in the hand of Muḥammad ibn Ibrāhīm al-Najāḥī al-Shāfiʻī.
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1. Tarih-i Al-i Osman bin Ertuğrul (dates of Ottoman Sultans) (f. 1r) -- 2. Suret-i arzname (ff. 1v--2v) -- 3. Arabic poem, awāʼil Muḥarram 804 [August 11-20, 1401] (copied by Ḥājjī Aḥmad ibn ... al-B.f.l.ghānī) (ff. 3r-11r) -- 4. Taʻrīfāt ʻilm usūl fiqh, Shawwāl 804 [May 1402] (ff. 11v-16v) -- 5. Arabic glossary (explanations in Arabic and Persian), 804 [1402] (copied by Idrīs b. Ḥasan b. Bayram) (ff. 17r-52r) -- 6. Sharḥ al-Farāʼiḍ al-Sirājīyah / ʻAbd al-Karīm b. Muḥammad b. al-Ḥasan al-Hamadānī al-Tabrīzī, awāsiṭ Dhī al-Ḥijja 804 [July 1402] (copied by Idrīs b. Ḥasan b. Bayram) (ff. 52v-94r) -- 7. Lughat-i ḥurūf (ff. 94v-95r) -- 8. Mufradāt-i Pārsī (A list of Persian verbs) (ff. 95v-97v).
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Recent observations on postglacial emergence and past glacier extent for one of the least accessible areas in the Arctic, northern Novaya Zemlya are here united. The postglacial marine limit formed 5 to 6 ka is registered on the east and west coasts of the north island at 10 ± 1 and 18 ± 2 m aht, respectively. This modest and late isostatic response along with deglacial ages of >9.2 ka on adjacent marine cores from the northern Barents Sea indicate either early (>13 ka) deglaciation or modest ice sheet loading (<1500 m thick ice sheet) of Novaya Zemlya. Older and higher (up to 50 m aht) raised beaches were identified beneath a discontinuous glacial drift. Shells from the drift and underlying sublittoral sediments yield minimum limiting 14C ages of 26 to 30 ka on an earlier deglacial event(s). The only moraines identified are within 4 km of present glacier margins and reflect at least three neoglacial advances in the past 2.4 ka.
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Reflecting the natural biology of mass spawning fish aquaculture production of fish larvae is often hampered by high and unpredictable mortality rates. The present study aimed to enhance larval performance and immunity via the oral administration of an immunomodulator, beta-glucan (MacroGard®) in turbot (Scophthalmus maximus). Rotifers (Brachionus plicatilis) were incubated with or without yeast beta-1,3/1,6-glucan in form of MacroGard® at a concentration of 0.5 g/L. Rotifers were fed to first feeding turbot larvae once a day. From day 13 dph onwards all tanks were additionally fed untreated Artemia sp. nauplii (1 nauplius ml/L). Daily mortality was monitored and larvae were sampled at 11 and 24 dph for expression of 30 genes, trypsin activity and size measurements. Along with the feeding of beta-glucan daily mortality was significantly reduced by ca. 15% and an alteration of the larval microbiota was observed. At 11 dph gene expression of trypsin and chymotrypsin was elevated in the MacroGard® fed fish, which resulted in heightened tryptic enzyme activity. No effect on genes encoding antioxidative proteins was observed, whilst the immune response was clearly modulated by beta-glucan. At 11 dph complement component c3 was elevated whilst cytokines, antimicrobial peptides, toll like receptor 3 and heat shock protein 70 were not affected. At the later time point (24 dph) an anti-inflammatory effect in form of a down-regulation of hsp 70, tnf-alpha and il-1beta was observed. We conclude that the administration of beta-glucan induced an immunomodulatory response and could be used as an effective measure to increase survival in rearing of turbot.
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Molecular and isotopic measurements of gas and water obtained from a gas hydrate at Site 570, DSDP Leg 84, are reported. The hydrate appeared to be Structure I and was composed of a solid framework of water molecules enclosing methane and small amounts of ethane and carbon dioxide. Carbon isotopic values for the hydrate-bound methane, ethane, and carbon dioxide were -41 to about -44, -27, and -2.9 per mil, respectively. The d13C-C1 values are consistent with void gas values that were determined to have a biogenic source. A significant thermogenic source was discounted because of high C1/C2 ratios and because the d13C-CO2 values in these sections were also anomalously heavy (or more positive) isotopically, suggesting that the methane was formed biogenically by reduction of heavy CO2 . The isotopically heavy hydrate d13C-C2 is also similar to void gas isotopic compositions and is either a result of low-temperature diagenesis producing heavy C2 in these immature sediment sections or upward migration of deeper thermogenic gas. The salinity of the hydrate water was 2.6 per mil with dDH2O and d18OH2O values of +1 and +2.2 per mil, respectively.