Polynesian voyaging driven by resource shortages

 A lot of the research into Polynesian voyaging looks at how it was accomplished and when, but less work has been done on why.

Why would groups of individuals, living in Pacific paradise islands, expend enormous treasure and energy to build great canoes and outfit massive voyaging missions?

The answers are coming.

This blog first looked into the issue in 2007.

That article reviewed a paper that suggested that sea level changes between 4,000 and 6,000 years ago, which created resource shortages, could have launched the Polynesians eastward into the Pacific from the islands near Asia.

And now, there’s new research that suggests a second period of resource shortages 1,000 years ago drove the final exploration phase—the one that led to the inhabitation of Hawai’i, Tahiti, the Marquesas, the Cooks, and eventually Rapa Nui and Aotearoa.

The suggestion is that a huge, multi-century central Pacific drought, from about AD 900 to 1200 drove settled populations out of the central Pacific and led them to locate new homelands that could feed expanding populations.

A team of Hawai’i, United Kingdom and New Zealand researchers in 2020 published a paper saying the signs of that drought can still be located in lake sediments in the Pacific Islands.

Their work answers that nagging question about Pacific voyaging: Why? Why would islanders in rich environments expend vast resources to build and provision voyaging canoes, and then sail into the uncharted ocean?

The paper’s authors are David A. Sear, Melinda S. Allen, Jonathan D. Hassall, Ashley E. Maloney, Peter G. Langdon, Alex E. Morrison, Andrew C. G. Henderson, Helen Mackay, Ian W. Croudace, Charlotte Clarke, Julian P. Sachs, Georgiana Macdonald, Richard C. Chiverrell, Melanie J. Leng, L. M. Cisneros-Dozal, Thierry Fonville, and Emma Pearson. Morrison is a senior archaeologist with Honolulu’s International Archaeology, LLC.

Their research paper, “Human settlement of East Polynesia earlier, incremental, and coincident with prolonged South Pacific drought,” was published in 2020 in the Proceedings of the National Academy of Sciences.

That prolonged drought was detected in sediments in Efate in Vanuatu, ‘Upolu in Samoa, and Atiu in the Southern Cook Islands. Other data from Tahiti and Kiribati also supports the drought hypothesis. It lasted from about AD 900 to AD 1200.

Their suggestion is that exploratory voyagers sailed out initially around 900, that they located islands and brought that information home, but that actual colonization took place generations later.

But once again, the message is that Polynesians voyaged because they had do.

© Jan TenBruggencate 2024