Pacific Society (pacific + society)

Distribution by Scientific Domains


Selected Abstracts


11TH BIENNIAL MEETING OF THE ASIA PACIFIC SOCIETY FOR SEXUAL MEDICINE OCTOBER 6-10, 2007, JEJU, KOREA

THE JOURNAL OF SEXUAL MEDICINE, Issue 2008
Article first published online: 5 DEC 200
First page of article [source]


Consequences of Contact: Language Ideologies and Sociocultural Transformations in Pacific Societies edited by Miki Makihara and Bambi B. Schieffelin

AMERICAN ANTHROPOLOGIST, Issue 4 2009
PAUL V. KROSKRITY
No abstract is available for this article. [source]


8th Asian Pacific Society of Respirology Congress MESSAGE FROM THE ORGANIZING CHAIRMAN

RESPIROLOGY, Issue 1 2003
Professor Chong-Kin Liam
No abstract is available for this article. [source]


Toward Unification of Asian Pacific Countries for Circulatory Support: Founding of the Asian Pacific Society for Circulatory Support

ARTIFICIAL ORGANS, Issue 7 2005
D.MSc., Setsuo Takatani Ph.D.
No abstract is available for this article. [source]


THE A.D. 1300 EVENT IN THE PACIFIC BASIN,

GEOGRAPHICAL REVIEW, Issue 1 2007
Patrick D. Nunn
ABSTRACT. Around a.d. 1300 the entire Pacific Basin (continental Pacific Rim and oceanic Pacific Islands) was affected by comparatively rapid cooling and sea-level fall, and possibly increased storminess, that caused massive and enduring changes to Pacific environments and societies. For most Pacific societies, adapted to the warmer, drier, and more stable climates of the preceding Medieval Climate Anomaly (a.d. 750,1250), the effects of this A.D. 1300 Event were profoundly disruptive, largely because of the reduction in food resources available in coastal zones attributable to the 70,80-centimeter sea-level fall. This disruption was manifested by the outbreak of persistent conflict, shifts in settlements from coasts to refugia inland or on unoccupied offshore islands, changes in subsistence strategies, and an abrupt end to long-distance cross-ocean interaction during the ensuing Little Ice Age (a.d. 1350,1800). The A.D. 1300 Event provides a good example of the disruptive potential for human societies of abrupt, short-lived climate changes. [source]