Carved and painted rock images in the Marquesas Islands, French Polynesia

1997 ◽  
Vol 32 (3) ◽  
pp. 181-196 ◽  
Author(s):  
Sidsel N. Millerstrom
2010 ◽  
Vol 19 (1) ◽  
pp. 11-14
Author(s):  
Hanna Margońska

A new variety of Habenaria (Orchidaceae, Habenariinae) from French Polynesia A new variety of Habenaria tahitensis (Orchidaceae, Habenariinae) from Tahiti and the Marquesas Islands (French Polynesia) is described, illustrated and compared to its closest relatives.


Zootaxa ◽  
2012 ◽  
Vol 3550 (1) ◽  
pp. 43 ◽  
Author(s):  
JOSEPH POUPIN ◽  
LAURE CORBARI ◽  
THIERRY PÉREZ ◽  
PIERRE CHEVALDONNÉ

Decapod crustaceans were studied in the Marquesas Islands, French Polynesia, between 50–550 m by using a remotelyoperated vehicle (ROV) equipped with high resolution cameras and an articulated arm. Careful examination of videos andphotographs combined with previous inventories made in the area with conventional gears allowed the identification of30 species, including 20 species-level determinations. Species identified belong to shrimps (Penaeoidea, Stenopodidea,and Caridea), lobsters (Astacidea and Achelata), anomurans (Galatheoidea and Paguroidea), and brachyuran crabs(Dromioidea, Homolodromioidea, Raninoidea, Leucosioidea, Majoidea, Parthenopoidea, Portunoidea, and Trapezioidea).Most of these species were observed and photographed in situ for the first time. A discussion is given on the geographic distribution, density, ecology, and behavior.


2007 ◽  
Vol 155 (4) ◽  
pp. 581-597 ◽  
Author(s):  
DAVID H. LORENCE ◽  
WARREN L. WAGNER ◽  
ARNAUD MOULY ◽  
JACQUES FLORENCE

2002 ◽  
Vol 173 (4) ◽  
pp. 359-367 ◽  
Author(s):  
Emile A. Okal ◽  
Gerard J. Fryer ◽  
José C. Borrero ◽  
Christophe Ruscher

Abstract On 13 September 1999, a local tsunami, comprising two waves separated by a few minutes, hit the village of Omoa, on the island of Fatu Hiva, French Polynesia. It inflicted serious damages to structures built close to the seashore, in particular to the local elementary school. The tsunami was generated by the collapse of a basaltic cliff, located 3 km to the southeast of Omoa, along the coastline. The volume of the landslide is estimated to range from 2 to 5 million m3, of which 60 % fell into the sea. A preliminary simulation of the tsunami provides an acceptable explanation of wave amplitudes, as well as an estimate of the origin time of landslide.


Author(s):  
Xénia Jost ◽  
Jean-Luc Ansel ◽  
Gaël Lecellier ◽  
Phila Raharivelomanana ◽  
Jean-François Butaud

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