1000 resultados para Townshend, Charles, 1725-1767.
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The bound notebook contains academic texts copied by Harvard student James Varney in the early 1720s. The texts are written tête-bêche (where both ends of the volume are used to begin writing). The front paste-down endpaper reads 'James Varney his book 1724,' and the rear paste-down endpaper reads 'Joseph Lovett' [AB 1728].
Voyage autour du monde par la frégate la Boudeuse et la flûte l'Étoile : en 1766, 1767, 1768 & 1769.
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Vocabulaire de l?ile Taiti: p. 389-402.
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Mode of access: Internet.
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ICCU,
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Concerning the claim of Archibald Douglas as heir of tailzie to his uncle, Archibald, duke of Douglas.
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Appendix: The sentiments of Charles Alphonse Du Fresnoy, on the works of the principal and best painters of the two last ages. The preface of Mr. Dryden to his translation, containing a parallel between poetry and painting. Epistle of Mr. Pope to Mr. Jervas. A chronological list of painters from the revival of the art to the beginning of the present century: p. [127]-213.
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Includes bibliographical references and index.
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"Errata",p.35.
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Verso of t.p. (p. [2] at front) a blank.
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Mode of access: Internet.
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Mode of access: Internet.
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"List of the works of Linnæus": p. 319-378.
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Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.