972 resultados para John II Comnenus, Emperor of the East, 1088-1143.
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Includes index.
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En el t.II: "A table of weights, measures and coins used in several parts of the East Indies" (10 p.)
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Mode of access: Internet.
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"An introduction to the geography of the New Testament ... by Lant Carpenter. Philadelphia : J. Anderson, printer, 1822" has special t.p. and separate paging.
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The mitochondrial DNA cytochrome b gene was sequenced from 8 bagrid catfishes in China. Aligned with cytochrome b sequences from 9 bagrid catfishes in Japan, Korea and Russia retrieved from GenBank, and selected Silurus meridionalis, Liobagrus anguillicauda, Liobagrus reini and Phenacogrammus interruptus as outgroups, we constructed a matrix of 21 DNA sequences. The Kimura's two-parameter distances were calculated and molecule phylogenetic trees were constructed by using the maximum parsimony (MP) and neighbor-joining (NJ) methods. The results show that (i) there exist 3-bp deletions of mitochondrial cytochrome b gene compared with cypriniforms and characiforms; (ii) the molecular phylogenetic tree suggests that bagrid catfishes form a monophyletic group, and the genus Mystus is the earliest divergent in the East Asian bagrid catfishes, as well as the genus Pseudobagrus is a monophyletic group but the genus Pelteobagrus and Leiocassis are complicated; and 60 the evolution rate of the East Asian bagrids mitochondrial cytochrome b gene is about 0.18%-0.30% sequence divergence per million years.
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Chemical analyses have been carried out on 40 samples from the sediment surface and 210 samples from cores that were taken from the edge of the African continental block at the Arabian Sea (coasts of Somalia and Kenya, from Cape Guardafui to Mombasa) on the occasion of the Indian Ocean Expedition of the German research vessel "Meteor" during the years 1964/65. The carbonate content shows its maximum on the northern part of the continental shelf of Africa, where fossil reef debris furnish the detritic portion of carbonate. In the southern part of the continental shelf of Africa the portion of carbonate is low, as it is heavily diluted by the non-carbonatic detritus. It is also in the deep-sea that a lower carbonate content is encountered below the calcite compensation depth. Trace elements in the carbonates: On the shelf and in its vicinity Sr and Mg are enriched. The enrichment has been brought about by the portion of reef debris, as this latter contains aragonite (enrichment of Sr) as well as high-magnesium calcite. The greatest part of the slope contains carbonates that are poor in trace elements and mainly made up of foraminifera (and of coccoliths). Below the carbonate compensation depth another enrichment of Mg takes place in the carbonates, which is probably due to a selective dissolution of calcite in comparison to dolomite. The iron and manganese contents of the carbonates are high (iron higher in coast proximity, manganese higher in the depth), but not genuine, as they come about in the course of the extraction of the carbonates as a result of the dissolution of authigenic Mn-Fe-minerals. Non-carbonatic portion of the sediments: In coast proximity an enrichment of quartz comes about. Within the quartz-rich zone it is the elements V, Cr, Fe, Ti, and B that have been enriched in the non-carbonatic components. This enrichment must be attributed to an elevated content of heavy minerals. In the case of Ti and Fe the preliminary enrichment brought about by processes of lateritisation on the continent plays a certain role. Toward the deep-sea an enrichment of the elements Mn Ni, Cu, and Zn takes place; these enrichments must be explained by authigenic Mn-Fe-minerals. Within the Mn-rich zone a belt running parallel to the coast stands out that shows an increased Mn-enrichment. However, this increase in enrichment does not apply to the elements Ni, Cu, and Zn. It is probable that this latter increased enrichment comes about as a result of the migration of manganese to the sediment surface. (Within the sediments there prevail reductive conditions, in the presence of which Mn is capable of migration, whereas at the sediment surface its precipitation comes about under oxidizing conditions). The quantity of organic matter mainly is dependent on grain size and on the rate of sedimentation. On the shelf an impoverishment of organic matter is to be encountered, as the sediments are coarse-grained. In the depth the impoverishment must be explained on the strength of a small rate of sedimentation. Between those two ranges organic substance is enriched. P and N show an enrichment in comparison to Corg with this applying all the more the smaller the absolute quantity of Corg is. In this particular case one has to do with an enrichment coming about during the diagenetic processes of organic matter. A comparison with the sediments from the Indian and Pakistani continental border in Arabian Sea shows as follows: on the African continental border the coarse detrital material has been transported farther out to deep-sea, which has something to do with the greater inclination of the surface of sedimentation. Carbonate is found in greater abundance on the African side. Its chemical composition is influenced by reef-debris which is missing by Indian-Pakistani side. The content of organic matter is lower on the African side. Contrary to that, the enrichments of N and P compared to organic matter are of an equal order of magnitude on both sides of the Arabian Sea.
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by John Cary.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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I. The life of John Flavel. The fountain of life.--II. The method of in the gospel-redemption. Pneumatologia; a treatise of the soul of man.--III. Pneumatologia (cont.) A practical treatise of fear. The righteous man's refuge. A blow at the root; or, The causes and cure of mental errors. Vindiciarum vindex. The second appendix; of Antinomianism. A sermon on gospel-unity.--England's duty. Mount Pisgah. Divine conduct; or, The mystery of Providence. Wonderful sea-deliverances. Antipharmacum saluberrimum. Tidings from Rome; or, England's alarm.-- V. Husbandry spiritualized; or, The heavenly use of earthly things. Navigation spiritualized; or, A new compass for seamen. [Miscellaneous tracts and sermons]--VI. Preparations for sufferings. The balm of the covenant. An exposition of the Assembly's Shorter catechism. A reply to Mr. Philip Cary's Solemn call. Sacramental meditations. [Miscellaneous tracts and sermons].
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Mode of access: Internet.
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Tâoism. The sacred books of China. The texts of Tâoism. In vol. 39, 4âry-Upanishads. In vol. I, 15.--Vedânta-Sûtras. With the commentary by Saṅkarâkaarya. In vol. 34, 38, 48.--Vedic hymns. In vol. 32, 46.--Vinaya text. Translated from the Pâli.l In vol. 13, 17, 20.--Vishnu. The institutes of Vishnu. In vol. 7.--Zend-Avesta. In vol. 4, 23, 31.--A general index to the names and subject-matter, comiled by M. Winternitz. In vol. 50.
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Mode of access: Internet.