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Garry Trompf 《Oceania; a journal devoted to the study of the native peoples of Australia, New Guinea, and the Islands of the Pacific》1984,55(2):148-153
Theologische Beiträge aus Papua Neuguinea. Edited by Horst Bürkle (Erlanger Taschenbücher 43). Erlangen: Evangelische - Lutheranische Mission, 1978. Pp. 345. Traditionen und Christentum in Chimbu-Gebiet Neuguineas; Beobachtungen in der Lutherischen Gemeinde Pare. By Friedegard Tomasetti. (Arbeiten aus dem Seminar für Völkerkunde der Johann Wolfgang Goethe-Universität Frankfurt an Main 6). Wiesbaden: Franz Steiner. 1976. Pp. 200. Papuan Belief and Ritual. John Parratt. New York, Washington, Atlanta and Hollywood: Vantage. 1976. Pp. xvi + 101. 相似文献
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During recent reinvestigations in the Great Cave of Niah in Borneo, the ‘Hell Trench’ sedimentary sequence seen by earlier excavators was re-exposed. Early excavations here yielded the earliest anatomically-modern human remains in island Southeast Asia. Calibrated radiocarbon dates, pollen, algal microfossils, palynofacies, granulometry and geochemistry of the ‘Hell Trench’ sequence provide information about environmental and vegetational changes, elements of geomorphic history and information about human activity. The ‘Hell’ sediments were laid down episodically in an ephemeral stream or pool. The pollen suggests cyclically changing vegetation with forest habitats alternating with more open environments; indicating that phases with both temperatures and precipitation reduced compared with the present. These events can be correlated with global climate change sequences to produce a provisional dating framework. During some forest phases, high counts of Justicia, a plant which today colonises recently burnt forest areas, point to fire in the landscape. This may be evidence for biomass burning by humans, presumably to maintain forest-edge habitats. There is evidence from palynofacies for fire on the cave floor in the ‘Hell’ area. Since the area sampled is beyond the limit of plant growth, this is evidence for human activity. The first such evidence is during an episode with significant grassland indicators, suggesting that people may have reached the site during a climatic phase characterised by relatively open habitats ∼50 ka. Thereafter, people were able to maintain a relatively consistent presence at Niah. The human use of the ‘Hell’ area seems to have intensified through time, probably because changes in the local hydrological regime made the area dryer and more suitable for human use. 相似文献
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Carry Momber 《International Journal of Nautical Archaeology》1991,20(2):95-109
Aerial reconnaissance in 1989 revealed a semicircular structure lying just off the coast at Clynnog Fawr in Caernarfon Bay, North Wales. The similarity in shape of the structure to other coastal fish-traps in the area promoted further study. Several avenues of research were followed. Historical sources were scrutinized in an attempt to find a date for the construction of the structure. A hydrographic survey was used to obtain the exact position and shape of the anomaly. A survey of the cliff and beach directly inland of the site was also made.
The anomaly was seen to lie further out to sea today than would have been the case at the time of its construction, indicating an area of coastal erosion. In an attempt to understand this process, the marine and atmospheric forces acting on the area were examined. In association with the processes of coastal erosion, soil tests were undertaken to assess the nature of the material being eroded.
Using both historical and physiological evidence it was concluded that the anomaly was indeed a fish-trap, constructed at about the beginning of the 13th century. The results from the different avenues of study have shown a sea-level rise of about 2.84 m and a cliff recession of about 118 m since its construction. 相似文献
The anomaly was seen to lie further out to sea today than would have been the case at the time of its construction, indicating an area of coastal erosion. In an attempt to understand this process, the marine and atmospheric forces acting on the area were examined. In association with the processes of coastal erosion, soil tests were undertaken to assess the nature of the material being eroded.
Using both historical and physiological evidence it was concluded that the anomaly was indeed a fish-trap, constructed at about the beginning of the 13th century. The results from the different avenues of study have shown a sea-level rise of about 2.84 m and a cliff recession of about 118 m since its construction. 相似文献
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J. Garry Clifford 《The Historian; a journal of history》2014,76(2):439-440
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