954 resultados para Eusebius, Bishop of Emesa, ca. 300-ca. 359.


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One-leaf undated handwritten fragment from the College customs signed "A true copy Attest Edward Wigglesworth" with the postscript "Thomas Leonards penison."

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Four pieces of paper containing notes and figures related to colleges in the University of Cambridge including calculations of the number of fellows, scholars, and masters. The verso of one leaf contains a February 21, 1800 request for the creation of a pamphlet with eulogies for George Washington.

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Small notebook containing handwritten entries of actions for the years 1718-1799 recorded in Volumes I-IV of the Harvard Board of Overseers formal meeting minutes. The entries note the appointment of Committees of inquiry and votes related to salary increases and allowances.

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Shapleigh's notes are written on the verso of a Harvard commencement theses broadside from 1792. Additional commencement theses broadsides from 1792 are available in the Harvard University Commencement theses, quaestiones, and orders of exercises collection (HUC 6642).

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A map of estimated calcification temperatures of the planktic foraminifer Neogloboquadrina pachyderma sinistral (TNps) for the Nordic Seas and the northern North Atlantic for the Last Glacial Maximum was produced from oxygen isotopes with support of Mg/Ca ratios. To arrive at the reconstruction, several constraints concerning the plausible salinity and ?18O-fields were employed. The reconstruction indicates inflow of temperate waters in a wedge along the eastern border of the Nordic Seas and at least seasonally ice-free waters. The reconstruction from oxygen isotopes shows similarities with Mg/Ca based paleotemperatures in the southern and southeastern sector, while unrealistically high Mg/Ca values in the central Nordic Seas prevent the application of the method in this area. The oxygen isotope based reconstruction shows some agreement with temperature reconstructions based on the modern analogue technique, but with somewhat lower temperatures and a stronger internal gradient inside the Nordic Seas. All told, our results suggest a much more ice-free and dynamic high latitude ocean than the CLIMAP reconstruction.

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Includes index.

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Students in tennis attire sitting on grass, ca. 1905 (Daybook image)

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