988 resultados para Sierra Engarcerán-Grabado
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Panktonic foraminiferal tests of the spinose species Orbulina universa, of the non-spinose Globorotalia tumida-menardii complex, and of a mixed species assemblage (grain size fraction 200-400 µm) were isolated from Sierra Leone Rise core GIK13519-2 and analyzed for free, total, and bound (by difference) amino acids to study the isoleucine epimerization mechanism in fossil foraminiferal tests and to define empirical calibration curves for dating deep-sea sediments over the past 900,000 years. Total isoleucine epimerization curves typically separate into three "linear" segments of decreasing apparents rates with increasing time and exhibit a pronounced "species effect". The degree of epimerization attained at time is considerably lower in O. universa than in G. tumida-menardii while the mixed species results scatter between the limits delineated by the two monospecific curves. Total allo/iso ratios are closely related to the proportion of free to total isoleucine accumulating in the tests indicating that the rate of hydrolysis of matrix proteins and peptides controls the overall epimerization reaction. The results are consistent with experimental evidenve where upon isoleucine epimerizes at a rapid rate in terminal positions but at slow rates in interior positions as well as in the free state. Notwithstanding free isoleucine exhibits the highest degree of epimerized terminal isoleucine. Species-specific hydrolysis and epimerization rates are maintained until about 50 % of bound isoleucine have been hydrolyzed to the free state corresponding to a total allo/iso ratio of about 0.5. Remaining peptide units appear to be more resistent against hydrolysis and separate species then show the same apparent epimerization rate dominantly controlled by the slow conversion rate in the free state until equilibrium is achieved in Miocene samples under deep-ocean temperature conditions. The degree of epimerization attained at comparable time in separate species will, however, remain different due to different initial rates of hydrolysis.
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We have integrated Oligocene to lower upper Miocene planktonic foraminifer biostratigraphy with benthic foraminifer (Cibicidoides spp.) stable isotope records for two sites drilled on opposite sides of the Sierra Leone Rise in the eastern equatorial Atlantic Ocean. Deep Sea Drilling Project Site 366 (2853 m present water depth; 2200-2800 m paleodepth) recovered an Oligocene to upper Miocene record with a minor unconformity in the "middle" Oligocene and a condensed middle Miocene section. Ocean Drilling Program Site 667 (3529 m present depth; 3000-3500 m paleodepth) recovered an apparently continuous "middle" Oligocene to lower middle Miocene record and a similar condensed middle Miocene section. The Oligocene to lower Miocene sections were deposited at similar sedimentation rates (~11-16 m/m.y.). Stable isotope stratigraphy proved to be useful in establishing intra- and interbasinal correlations. In addition to the well-known earliest Oligocene and middle Miocene S180 increases, a distinct d18O increase occurred near the Oligocene/Miocene boundary. Carbon isotope variations provide similar potential for improving correlations; for example, a d13C increase occurred near the Oligocene/Miocene boundary in concert with increased d18O values. There was little d13C difference between the western Atlantic and eastern Atlantic basins during the late Oligocene and most of the middle Miocene; in contrast, eastern basin d13C values were slightly lower than those in the western basins during the earliest Oligocene (about 35-33 Ma) and early Miocene (about 22-18 Ma).
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Mode of access: Internet.
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"Organo de la Asociación Universitaria."
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Poems.
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Mode of access: Internet.
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Mode of access: Internet.
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Thesis (Ph.D.)--Univ. of California, May 1920.
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Contiene: Premiere partie, Livre cinquiéme, Voyages en différentes parties de l'Afrique & dans les isles adjacentes, avec la description des pays & des habitants. - Premiere partie, Livre sixiéme, Voyages au long de la cote occidentale d'Afrique, depuis le Cap Blanco jusqu'à Sierra Leona, contenant la description de plusieus pays & de leurs habitants. [Incluye los relatos de: Roberts en 1721-24 a Cabo Verde, Jannequin en 1637 a Libya, Senegal y rio Niger y Brue en 1697 a la costa occidental de Africa]
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Premiere partie, Livre sixiéme, Voyages au long de la cote occidentale d'Afrique, depuis le Cap Blanco jusqu'à Sierra Leona, contenant la description de plusieus pays & de leurs habitants. - Table des chapitres & paragraphes contenus dans [volumes V, VI, VII, VIII]. - Avis au relier, pour placer les cartes géographiques... les figures. - [Viajes de Brue desde 1697 a 1715].
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Advertissement p.i-vj. - Lettre de M. Bellin...a M.l'abbé Prevost p. vij-xij. - Approbation p.xij. - Premiere partie, Livre septiéme, Voyages au long de la cote occidentale d'Afrique, depuis le Cap Blanco jusqu'à Sierra Leona, contenant l'établissement du commerce des anglois sur la riviere de Gambra, vulgairemente la Gambie. - [Se incluyen los relatos de: Jobson en 1620-21, Stibbs en 1723-24, Moore en 1730-35, Job Ben Salomon en 1731-35, Broek en 1605, Le Maire (a las Canarias y otros sitios) en 1682; observaciones sobre los Jalofs, Foulis y Mandingos].
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Premiere partie, Livre septiéme, Voyages au long de la cote occidentale d'Afrique, depuis le Cap Blanco jusqu'à Sierra Leona, contenant l'établissement du commerce des anglois sur la riviere de Gambra, vulgairemente la Gambie. - [Se incluyen, entre otros, los relatos sobre Sierra Leona de Finch en 1607, Villault en 1666, Barbot en 1678 y Atkins en 1678 y 1721].
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.