Rome sous Trajan /

Cover imprint: Paris, A. Degorce-Cadot.

History of the later Roman commonwealth, from the end of the second Punic war to the death of Julius Caesar; and of the reign of Augustus; with a life of Trajan.

M. Ulpius Trajanus Crinitus from A.D. 98 to 117: vol. II, p. [409]-476.

History of the later Roman commonwealth : from the end of the second Punic war to the death of Julius Cæsar; and of the reign of Augustus: with a life of Trajan /

Republished from the "Encyclopædia Metropolitana."

Trajan's dakische Kriege : nach dem Säulenrelief /

Includes bibliographical references.

Zur Geschichte Trajan's und seiner Zeitgenossen /

Includes inscriptions in Latin.

Zur Geschichte Trajan's und seiner Zeitgenossen /

Includes inscriptions in Latin.

Der judische Krieg : unter den Kaiser Trajan und Hadrian.

Mode of access: Internet.

Kaiser Trajanus. Eine festrede zum 27. Januar 1898.

Beilage zum osterprogramm des Königlichen Friedrich-Wilhelms-gymnasiums zu Köln, 1898.

Le fonti per la storia dell'imperatore Traiano.

"Estratto dal periodico Studi e documenti di storia e diritto, anno xvi, 1895."

C. Plinii Caecilii Secundi Epistolae et Panegyricus Trajano dictus ... /

Includes index of recipients of the letters.

I reclami del Foro Trajano eposti al pubblico e giustificati

Mode of access: Internet.

The communings with himself of Marcus Aurelius Antoninus, emperor of Rome, together with his speeches and saying;

Bibliography: p. xxxix-xxxi.

Nero, Emperor of Rome. : A tragedy, acted at the Theatre-Royal by His Majesty's Servants. /

Head- and tail-pieces; initials; title vignette.

Planktonic foraminifera of ODP Site 117-722

Quantitative analysis of the late Cenozoic planktonic foraminiferal record from western Arabian Sea Site 722 revealed long term trends in the history of oceanography and climate. The modern western Arabian Sea surface waters are highly influenced by the monsoonal wind system. Summer upwelling, a result of southwestern winds, occurs along the coast of Somalia which produces distinct foraminiferal assemblages which are dominated by G. bulloides d'Orbigny. Consequently, variations in the distribution record of G. bulloides through time monitor the upwelling history associated with monsoonal activities. G. bulloides was a minor constituent of the foraminiferal fauna from the bottom of the hole (~14.5 Ma) until about 8.6 Ma ago. Then a rapid shift occurred toward higher values, up to 53% at 7.4 Ma. We interpret this rapid increase as a major step in the evolution of the monsoonal history. It is either the establishment of the system or at least a strong intensification of the monsoonal winds. At 5.5 Ma a significant drop of the G. bulloides relative abundance occurred which may indicate less upwelling, or alternatively other biota may have been favored in this period. From 5.0 Ma to Recent the G. bulloides record indicates that upwelling has occurred with minor fluctuations.