964 resultados para Ansgar, Saint, Archbishop of Hamburg and Bremen, ca. 801-865.


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"Opus hoc [Vita Rimberti] superstite Adalgario, Rimberti successore, sed certe non ab ipso, sed ab alio quodam, aut ecclesiae bremensis clerico, aut monacho corbeiensi compositum est."--G. H. Pertz, quoted, p. [80]

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This note, likely in the hand of President Willard, directs Mr. [Josiah] Moore and Mr. [John] Walton measure the length, width, and height of the chapel, hall, and library in Harvard Hall. Includes each room's measurements.

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This manuscript grammar notebook, written in Chaldean Aramaic and English, appears to have originally belonged to William Bentley (Harvard A.B. 1777); Bentley's name and a date, "December 1776," appear on the volume but have been struck through, and the handwriting appears to be his. The names of Elisha Parmele and Polly Parmele are also on the volume; presumably it was given to Elisha by Bentley, and upon Elisha's death in 1784 it was passed to Polly.

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Includes bibliographical references and index.

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Mode of access: Internet.

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Mode of access: Internet.

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The late Miocene carbon shift (~6.2 Myr) -a 0.5-1.0 per mil, d13C decrease in benthic and planktonic foraminifera- has been ascribed to changes in global inventory, deep-ocean circulation, and/or productivity. Cadmium, d13C, and nutrients in the ocean are linked; comparison of d13C and Cd/Ca yields circulation and chemical inventory information not available from either alone. We determined Cd/Ca ratios in late Miocene benthic foraminifera from DSDP Site 289. Results include: (1) late Miocene Pacific Cd/Ca values fall between those of late Quaternary Atlantic and Pacific benthic foraminifera; (2) there are no systematic Cd/Ca offsets between Cibicidoides kullenbergi, Cibicidoides wuellerstorfi and Uvigerina spp.; and (3) there is a very slight Cd/Ca change coincident with d13C. Cd/Ca, slightly higher in younger, isotopically lighter samples, exhibits a smaller increase than predicted if circulation were the primary cause of the carbon shift. The carbon shift may have been due to a long-term shift in the steady-state carbon isotope input or to a change in the sedimentation of organic carbon relative to calcium carbonate.