Vanuatu environments from the Holocene to the present day: A state of knowledge
Identifieur interne : 000275 ( Hal/Curation ); précédent : 000274; suivant : 000276Vanuatu environments from the Holocene to the present day: A state of knowledge
Auteurs : Claire Combettes [France]Source :
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Abstract
The first Vanuatu archaeological site discovery dates back to the 1960s, then the scientific and archaeological knowledge of this archipelago have increased. Nevertheless, the human activities–palaeoenvironmental changes relation in Vanuatu is still a matter of debate. In order to better determine this relation, reviewing the literature on past and actual environment is needed. This paper presents here a state of knowledge on Vanuatu geology, climate, biodiversity and archaeology, from the mid-Holocene to our present-day. The young archipelago results from strong volcanic and tectonic activity, due to the active subduction zone between Australian and Pacific plates. The atmosphere–ocean interactions determine the wet and dry seasons. Fauna and flora are principally derived from Southeast Asia. The occurrence of several species and subspecies endemic to the archipelago, if not to some islands, is probably due to the Vanuatu isolated location, the size of the islands and the climatic gradient between north and south. The first human populations reached the archipelago around 3200 yr BP. The Lapita culture, characterized by decorated potteries, is shared across the whole Vanuatu between 3200 and 2900 yr BP. After 2900 yr BP, cultures differ from one island to another. After 600 yr BP, the Polynesian culture dominates in Vanuatu.
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DOI: 10.1016/j.anthro.2016.03.003
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<front><div type="abstract" xml:lang="en">The first Vanuatu archaeological site discovery dates back to the 1960s, then the scientific and archaeological knowledge of this archipelago have increased. Nevertheless, the human activities–palaeoenvironmental changes relation in Vanuatu is still a matter of debate. In order to better determine this relation, reviewing the literature on past and actual environment is needed. This paper presents here a state of knowledge on Vanuatu geology, climate, biodiversity and archaeology, from the mid-Holocene to our present-day. The young archipelago results from strong volcanic and tectonic activity, due to the active subduction zone between Australian and Pacific plates. The atmosphere–ocean interactions determine the wet and dry seasons. Fauna and flora are principally derived from Southeast Asia. The occurrence of several species and subspecies endemic to the archipelago, if not to some islands, is probably due to the Vanuatu isolated location, the size of the islands and the climatic gradient between north and south. The first human populations reached the archipelago around 3200 yr BP. The Lapita culture, characterized by decorated potteries, is shared across the whole Vanuatu between 3200 and 2900 yr BP. After 2900 yr BP, cultures differ from one island to another. After 600 yr BP, the Polynesian culture dominates in Vanuatu.</div>
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<abstract xml:lang="en">The first Vanuatu archaeological site discovery dates back to the 1960s, then the scientific and archaeological knowledge of this archipelago have increased. Nevertheless, the human activities–palaeoenvironmental changes relation in Vanuatu is still a matter of debate. In order to better determine this relation, reviewing the literature on past and actual environment is needed. This paper presents here a state of knowledge on Vanuatu geology, climate, biodiversity and archaeology, from the mid-Holocene to our present-day. The young archipelago results from strong volcanic and tectonic activity, due to the active subduction zone between Australian and Pacific plates. The atmosphere–ocean interactions determine the wet and dry seasons. Fauna and flora are principally derived from Southeast Asia. The occurrence of several species and subspecies endemic to the archipelago, if not to some islands, is probably due to the Vanuatu isolated location, the size of the islands and the climatic gradient between north and south. The first human populations reached the archipelago around 3200 yr BP. The Lapita culture, characterized by decorated potteries, is shared across the whole Vanuatu between 3200 and 2900 yr BP. After 2900 yr BP, cultures differ from one island to another. After 600 yr BP, the Polynesian culture dominates in Vanuatu.</abstract>
<abstract xml:lang="fr">La découverte des premiers sites archéologiques du Vanuatu remonte aux années 1960. Depuis, les connaissances scientifiques et archéologiques sur cet archipel ont grandement augmenté. Cependant, les relations entre l’Homme et les différents changements paléoenvironnementaux du Vanuatu restent un sujet débattu. Afin de mieux décrire ces relations, il est important de faire un point sur ce que nous savons des environnements passés et présents. Cet article présente donc un état des lieux des connaissances sur la géologie, le climat, la biodiversité et l’archéologie du Vanuatu, de l’Holocène moyen jusqu’à nos jours. L’archipel du Vanuatu est relativement jeune et issu d’une forte activité volcanique et tectonique de la zone de subduction entre la plaque Pacifique et la plaque Australie. Le climat est majoritairement influencé par les relations atmosphère–océan Pacifique, déterminant les saisons humides et sèches. La faune et la flore sont principalement originaires d’Asie du Sud-Est mais l’isolement de l’archipel, la taille des îles et le gradient climatique entre le nord et le sud sont à l’origine de la présence de certaines espèces et sous-espèces endémiques à l’archipel, voire à quelques îles. Les premières populations humaines n’ont atteint l’archipel qu’autour de 3200 ans BP. Entre 3200 et 2900 ans BP, la culture Lapita, caractérisée par des poteries très décorées, est commune à tout le Vanuatu. Après 2900 ans BP, les cultures divergent et diffèrent d’une île à une autre. À partir de 600 ans BP, la culture polynésienne domine au Vanuatu dans les îles du centre et du sud.</abstract>
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