998 resultados para Busseto (Italy)


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The proposed third volume was never published, although copyright claim is printed on back of t.-p. ("The Reminiscences copyright 1881 by Henry Stevens of Vermont." The records of the Copyright office do not bear out this statement) The material was later published in Transactions and proceedings of the Library association of the United Kingdom at their seventh annual meeting...1884. London, 1890 (p. 117-124: Twenty years reminiscences of Panizzi and the British museum, 1845-1865)

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Translation of "Reisebriefe...aus den jahren 1830 bis 1832", edited by Paul Mendelssohn Bartholdy (Leipzig, 1862)

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Vital Subjects: Race and Biopolitics in Italy is an interdisciplinary study of how racial and colonial discourses shaped the “making” of Italians as modern political subjects in the years between its administrative unification (1861-1870) and the end of the First World War (1919)

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Includes bibliographical references.

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Mode of access: Internet.

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Special t.p.: Posthuma fragmenta poematum Georgii Coryati Sarisburiensis, sacrae theologiae baccalaurei, quondem e sociis Novi collegii in inclyta academia Oxoniensi, as postea ecclesiae Odcombiensis in agro Somersetensi ministri, ubi tandem anno 1606, extremum vitae diem clausit. Londini, anno domini 1611: vol.II, p. [377-408]

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The age structure and, stable isotope composition of a stalagmite (CC I) from an upland cave in central-western Italy were studied to investigate regional response to global climatic changes. Four growth phases are constrained by 28 thermal ionization and multi-collector inductively coupled plasma mass spectrometry Th-U ages and reveal intermittent deposition through the period between Marine isotope Stage (MIS) 11 and 3 (similar to380 and similar to43 kyr). Most of the growth took place between similar to380 and similar to280 kyr, a period punctuated briefly by a hiatus in deposition through the glacial maximum of MIS 10. Growth was terminated abruptly at 280 kyr just prior to the MIS 8 glacial maximum. With a present-day chamber temperature of 7.5 degreesC, the timing of hiatuses close to these glacial maxima point to freezing conditions at the time. No deposition was recorded through the entirety of MIS 7 and most of MIS 6, whilst two minor growth phases occurred at similar to141-125 and similar to43 kyr. Growth at 141 kyr indicates temperatures >0 degreesC at a time when MIS 6 ice volumes were close to their maximum. High stable carbon isotope (delta(13)C) values (similar to2.8parts per thousand to +3.1parts per thousand) throughout the stalagmite's growth reflect a persistently low input of biogenic CO2, indicating that the steep, barren and alpine-like recharge area of today ha's been in existence for at least the last similar to380 kyr. During MIS 9, the lowest delta(13)C values occur well after maximum interglacial conditions, suggesting a lag in the development of post-glacial soils in this high-altitude karst. The stable oxygen isotope (delta(18)O) trends match the main structural features of the major climate proxy records (SPECMAP, Vostok and Devils Hole), suggesting that the delta(18)O of CC1 has responded to global-scale climate changes, whilst remarkable similarity exists between CC1 delta(18)O and regional sea-surface temperature reconstructions from North Atlantic core ODP980 and southwest Pacific marine core MD97-2120 through the most detailed part of the CC1 record, MIS 9-8. The results suggest that CC1 and other stalagmites from the cave have the potential to capture a long record of regional temperature trends, particularly in regards to the relative severity of Pleistocene glacial stages. (C) 2004 Elsevier B.V. All rights reserved.