Analysis of Plant Microfossils in Archaeological

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Analysis of Plant Microfossils in Archaeological Analysis of Plant Microfossils in Archaeological Deposits from Two Remote Archipelagos: The Marshall Islands, Eastern Micronesia, and the Pitcairn Group, Southeast Polynesia1 Mark Horrocks2,3,5 and Marshall I. Weisler4 Abstract: Pollen and starch residue analyses were conducted on 24 sediment samples from archaeological sites on Maloelap and Ebon Atolls in the Marshall Islands, eastern Micronesia, and Henderson and Pitcairn Islands in the Pitcairn Group, Southeast Polynesia. The sampled islands, two of which are ‘‘mystery islands’’ (Henderson and Pitcairn), previously occupied and abandoned before European contact, comprise three types of Pacific islands: low coral atolls, raised atolls, and volcanic islands. Pollen, starch grains, calcium oxylate crystals, and xylem cells of introduced non-Colocasia Araceae (aroids) were identified in the Marshalls and Henderson (ca. 1,900 yr B.P. and 1,200 yr B.P. at the earliest, re- spectively). The data provide direct evidence of prehistoric horticulture in those islands and initial fossil pollen sequences from Pitcairn Island. Combined with previous studies, the data also indicate a horticultural system on Henderson comprising both field and tree crops, with seven different cultigens, including at least two species of the Araceae. Starch grains and xylem cells of Ipomoea sp., possibly introduced I. batatas, were identified in Pitcairn Island deposits dated to the last few centuries before European contact in 1790. During the late Holocene settlement of This involved starch staples produced the eastern Pacific, agricultural practices com- through a variety of ‘‘wet’’ and ‘‘dry’’ field- bining tropical Asian-Pacific and American cropping methods (Kirch 1994) and tree crops were adapted to a diversity of island cropping (Yen 1973). The extension of these environments (Yen 1973, Spriggs 1982, Ayres practices to remote islands of often very small and Haun 1990, Kirch 1994, Bellwood 2005). area with barren soil, unreliable groundwater supply, unpredictable rainfall, and frequent marine inundation was one of the most chal- 1 The Marsden Fund administered by the Royal Soci- lenging accomplishments of this diaspora. ety of New Zealand provided support for M.H. Funding from the Wenner Gren Foundation for Anthropological The starch staples include four species of Research, the United Nations, the U.S. National Park the Araceae, Colocasia esculenta (taro), Alocasia Service, the Australian South Pacific Cultures Fund, and macrorrhiza (elephant ear taro), Cyrtosperma the Historic Preservation Office (Republic of the Mar- merkusii (syn. chamissonis, giant swamp taro), shall Islands) provided support for M.I.W. Manuscript accepted 2 June 2005. and Amorphophallus paeoniifolius (elephant 2 Microfossil Research Ltd., 31 Mont Le Grand Road, yam); and Dioscorea spp. (yams), Musa spp. Mount Eden, Auckland 1003, New Zealand (e-mail: (bananas), Artocarpus altilis (breadfruit), and www.microfossilresearch.com). Ipomoea batatas (sweet potato). In total, there 3 School of Geography and Environmental Science, are approximately 30 species of subsistence University of Auckland, Private Bag 92-019, Auckland, New Zealand. plants listed (see, e.g., Kirch 1989, Loy et al. 4 School of Social Science, University of Queensland, 1992, Matthews 1996). Many of these origi- St. Lucia 4072, Queensland, Australia. nated in Asia and, recent research suggests, 5 Corresponding author. also in the Sahul continental region (Haberle 1995, Lebot 1999, Denham et al. 2003, Mat- Pacific Science (2006), vol. 60, no. 2:261–280 thews 2003, Bellwood 2005). They were in- : 2006 by University of Hawai‘i Press troduced throughout the Pacific by early All rights reserved human colonizers. Ipomoea batatas (sweet 261 262 PACIFIC SCIENCE . April 2006 potato) and Lagenaria siceraria (bottle gourd) this growing body of evidence, however, ma- originated in South America, their introduc- jor gaps in the Pacific record remain. In addi- tions a result of Polynesian contact (Hather tion, human settlement of atolls is extremely and Kirch 1991, Green 2000). underresearched (Weisler 1999). Research on the age, development, and di- Although ethnographic accounts are valu- versity of early agriculture in the Pacific has able sources of information, we would like to been hindered by transformation of tradi- know which species were introduced where tional cropping systems after European con- and when. The so-called ‘‘mystery islands’’ tact and archaeological scarcity of crop are particularly problematic in this respect fossils. However, recent advances have been because they were uninhabited at the time made with regard to the latter at sites across of Western contact. There are more than a the Pacific by the identification of plant mac- score of these, typically small targets at some rofossils and especially by the application of a distance from their nearest neighbors (Irwin range of microfossil techniques, namely pol- 1992). Given the isolation, small size, and len, starch residues, and phytoliths. In Micro- especially resource-poor nature of these hab- nesia, prehistoric pollen (and macrofossils) of itats (including low-nutrient soils and unpre- the Araceae and Artocarpus altilis has been re- dictable water resources), it is uncertain if ported in the Mariana, Caroline, and Mar- horticulture was practiced at all. shall Islands (Beardsley 1994, Athens et al. During an archaeological expedition to the 1996, Athens and Ward 2002, 2004). In Mel- Pitcairn Group in Southeast Polynesia in anesia, Araceae starch residues have been 1991–1992, sediment samples from deposits identified at Lapita settlements in the Bis- thought to be prehistoric gardening areas marck Archipelago (Crowther 2005) and were collected (Weisler 1995). The project Vanuatu (Horrocks and Bedford 2005). Simi- was investigating the survival of small human larly, Lentfer and Green (2004) identified groups on isolated, marginal landfalls, and an Musa phytoliths at a Lapita site in the Bis- island-wide archaeological survey and exten- marcks. In Polynesia, starch residues, phyto- sive excavations in habitation sites were con- liths, and pollen of a suite of introduced ducted (Weisler 1995, 1997). In another cultivated plants have been identified in New project samples were collected in 1993–1997 Zealand, comprising Ipomoea batatas, Colocasia from the Marshall Islands in eastern Micro- esculenta, Lagenaria siceraria, and Broussonetia nesia (Weisler 1999, 2001a). That project papyrifera (paper mulberry) (Horrocks was investigating the timing and nature of 2004a). In the Society Islands, Parkes (1997) Araceae horticulture across the rainfall gradi- reported pollen of Ipomoea batatas, Colocasia ent in the Marshalls. Extreme remoteness is esculenta, and Cordyline fruticosa (syn. termina- a common feature of these two distant archi- lis, Pacific Island cabbage tree). Athens pelagoes. The sites presented the opportunity and Ward (1997) reported pollen of Colocasia to test different tropical soil types in a range esculenta, Cordyline fruticosa, and Aleurites mo- of environmental settings for preservation luccana (candlenut tree) in Hawai‘i, and Cum- of plant microfossils and to look for direct mings (1998) reported pollen of Ipomoea evidence of prehistoric horticulture near the batatas and starch granules of Colocasia on outer margins of both Polynesia and Micro- Easter Island. Macrofossils identified in Poly- nesia. The outer Pacific archipelagoes were nesia include Ipomoea batatas root (commonly among the last habitable places on Earth to referred to as tuber) from Hawai‘i (Rosendahl be colonized by people. These islands are and Yen 1971), the Cook Islands (Hather and ecologically fragile and often small, providing Kirch 1991), and New Zealand (e.g., Yen microcosms for the study of human adapta- and Head 1993); Aleurites moluccana endocarp tion to diverse, extreme environments. Pre- from the Cooks and Henderson Island (Kirch sented here are results of recent analyses of et al. 1992, Weisler 1995); and Araceae and pollen and starch residues in the sediment Musa leaf also from Henderson (Weisler samples from archaeological sites in these ar- 1997, Hather and Weisler 2000). Despite chipelagoes. Plant Microfossils from the Marshall Islands and Pitcairn Group . Horrocks and Weisler 263 The Study Areas, Sites, and Sample Context stratigraphically below a 1,580 G 80 yr B.P. date (Beta-69516 [Weisler 2001a]). The pit, marshall islands. Situated in eastern 73 cm in diameter, had subparallel sides to a Micronesia, the Marshall Islands comprise depth of 54 cm. Sample 3 is from MLMl-3, 29 atolls and five coral islands without a TP19, 21, and 24, buried A horizon dating central lagoon aligned in two roughly parallel to 1,910 G 70 yr B.P. (Beta-79576 [Weisler alignments. The climate is tropical, with the 1999]). Because the buried A horizon was archipelago traversing a rainfall gradient thin, sediment was taken from the sidewall from @1,000 mm in the north to @4,000 of three contiguous test pits. This sample is mm in the south. Mean annual temperature associated with the construction of an adja- is @27 C. Most of the atolls and islands are cent pit currently used for cultivation of currently inhabited; the two northernmost Cyrtosperma merkusi. and driest atolls, Taongi (Pokak) and Bikar, The Ebon and Enilok islet (Ebon Atoll) are uninhabited but are visited occasionally samples comprise samples 4–8. Samples 4–7 to collect birds and turtles. Samples from are from MLEb-2I, TP2 layers I, II, III, and two atolls were analyzed in this study: Maloe- IV, which correspond to samples 4–7 (Figure lap in the center of the archipelago and Ebon 1A). A 4-m-long trench was excavated in the far south. The 71 islets composing Ma- through the rim of a suspected horticultural loelap Atoll have a total terrestrial area of 9.8 pit, and stratigraphic samples were taken km2. Samples from one of these islets, Kaven from all four layers; layer III was the buried (2.3 km2), were analyzed. The 22 islets of A horizon dated to 1,930 G 40 yr B.P. (Beta- Ebon Atoll total 5.6 km2. Samples from two 92123 [Weisler 2002a]), layer I the near- of these, the largest, Ebon (2.7 km2), and surface A horizon, layer II a prehistoric habi- Enilok (0.4 km2), were analyzed.
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