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Avifaunal extinctions, vegetation change, and Polynesian impacts in prehistoric Hawai'i
Author(s) -
Athens J. Stephen,
Toggle H. David,
Ward Jerome V.,
Welch David J.
Publication year - 2002
Publication title -
archaeology in oceania
Language(s) - English
Resource type - Journals
eISSN - 1834-4453
pISSN - 0728-4896
DOI - 10.1002/j.1834-4453.2002.tb00507.x
Subject(s) - radiocarbon dating , prehistory , geography , archaeology , ecology , vegetation (pathology) , polynesians , coring , wetland , assemblage (archaeology) , habitat , biology , medicine , mechanical engineering , population , demography , pathology , sociology , engineering , drilling
Pre‐contact avifaunal extinctions in Hawai'i generally have been attributed to human predation and/or landscape alteration by colonizing Polynesians. However, until recently there have been insufficient data for evaluating most of the important variables involved in this issue. This situation has changed with recent archaeological, paleontological, and wetland coring research conducted on O'ahu's ‘Ewa Plain, a hot, dry emerged limestone reef characterized by numerous sinkholes. The main evidence obtained from this research includes (1) wetland coring data that stratigraphically demonstrate forest decline before any burning, (2) radiocarbon dating of bones of rats and extinct birds that provides a time frame for their occurrence unavailable from stratified deposits, and (3) the radiocarbon‐based history of human settlement of the 'Ewa Plain. Based on this evidence the argument is made that (1) at least some major avian extinctions occurred within the period immediately following Polynesian colonization, (2) these extinctions were due primarily to the rapid decline of their native lowland forest habitat, (3) human settlement of the 'Ewa Plain occurred after native forest collapse, not coincident with it, and (4) the main source of destruction of the native forests was the introduced Polynesian rat, Rattus exulans , not Hawaiian agricultural clearing and burning. This model also explains the absence of large quantities of bird bone in early sites (in contrast to other places in Polynesia and Micronesia), and the absence in early middens of many plants (notably Kanaloa kahoolawensis ) that were common in the native forest.