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Marine Reservoir Variation in the Bismarck Region: An Evaluation of Spatial and Temporal Change in ΔR and R Over the Last 3000 Years

Published online by Cambridge University Press:  18 July 2016

Fiona Petchey  and
Sean Ulm
Fiona Petchey*
Affiliation:
Radiocarbon Dating Laboratory, University of Waikato, Hamilton, New Zealand
Sean Ulm
Affiliation:
Department of Anthropology, Archaeology and Sociology, School of Arts and Social Sciences, James Cook University, Cairns, Australia
*
Corresponding author. Email: fpetchey@waikato.ac.nz
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Abstract

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Interactions between islands, ocean currents, and winds cause large-scale eddies and upwelling in the lee of islands that can result in spatial variation in the marine radiocarbon reservoir. For waters around New Ireland and the Bismarck Sea, ΔR values ranging from 365 to −320 14C yr have been reported (Kirch 2001; Petchey et al. 2004). Petchey et al. (2004) proposed that some of this variation was caused by seasonal reversals in the South Equatorial Current and North Equatorial Counter Current system, combined with Ekman upwelling from the Equator. McGregor et al. (2008) suggested additional complexity within this region caused by a change in the reservoir value over time in response to changing climatic conditions. We present a series of 14 new and extant published ΔR and R values on historic shells, combined with 8 values from archaeological terrestrial/marine pairs and U-Th dated coral, that support observations of localized variability caused by a complex interplay between seasonal currents, riverine input, and ocean eddies. On the basis of these values and oceanographic data, we divide the Bismarck Sea surface marine 14C reservoir into 6 tentative subregions. In particular, our results support significant variation within channels at the southwest and southeast ends of New Britain and towards the equatorial boundary of the sea. Our results indicate that within the Bismarck Sea geographical variation appears to be more extreme than temporal over the last 3000 yr.

Information

Type
Articles
Information
Radiocarbon , Volume 54 , Issue 1 , 2012 , pp. 45 - 58
Copyright
Copyright © 2012 by the Arizona Board of Regents on behalf of the University of Arizona 

References

Australian Institute of Marine Science (AIMS). 1998. Coral Sea region billfish atlas: currents. AIMS Research, Australian Institute of Marine Science. Available at http://www.aims.gov.au/pages/reflib/billfish/pages/bf_05.html. Accessed 25 August 2003.Google Scholar
Allen, MS. 2006. New ideas about late Holocene climate variability in the central Pacific. Current Anthropology 47(3):521–35.Google Scholar
Allen, MS, Wallace, R. 2007. New evidence from the East Polynesian gateway: substantive and methodological results from Aitutaki, southern Cook Islands. Radiocarbon 49(3):1–17.Google Scholar
Ambrose, WR. 1988. An early bronze artefact from Papua New Guinea. Antiquity 62(236):483–91.Google Scholar
Ambrose, W, Petchey, F, Swadling, P, Beran, H, Bonshek, L, Szabo, K, Bickler, S, Summerhayes, G. In press. Engraved prehistoric Conus shell artifacts from southeastern Papua New Guinea: their antiquity, motifs and distribution. Australian Archaeometry.Google Scholar
Anderson, A, Higham, T, Wallace, R. 2001. The radiocarbon chronology of the Norfolk Island archaeological sites. Records of the Australian Museum, Supplement 27:33–42.Google Scholar
Anderson, A, Chappell, J, Gagan, M, Grove, R. 2006. Prehistoric maritime migration in the Pacific islands: an hypothesis of ENSO forcing. The Holocene 16(1):1–6.Google Scholar
Bard, E. 1988. Correction of accelerator mass spectrometry 14C ages measured in planktonic foraminifera: paleoceanographic implications. Paleoceanography 3(6):635–45.Google Scholar
Beesley, PL, Ross, GJB, Wells, A, editors. 1998. Mollusca: The Southern Synthesis. Fauna of Australia. Volume 5. Melbourne: CSIRO Publishing.Google Scholar
Burr, GS, Beck, JW, Corrège, T, Cabioch, G, Taylor, FW, Donahue, DJ. 2009. Modern and Pleistocene reservoir ages inferred from South Pacific corals. Radiocarbon 51(1):319–35.Google Scholar
Chappell, J, Polach, HA. 1976. Holocene sea-level change and coral-reef growth at Huon Peninsula, Papua New Guinea. Geological Society of America Bulletin 87:235–40.Google Scholar
Clark, C, Reepmeyer, C. 2012. Last millennium climate change in the occupation and abandonment of Palau's Rock Islands. Archaeology in Oceania 47(1):29–38.Google Scholar
Cook, GT, MacKenzie, AB, Muir, GKP, Mackie, G, Gulliver, P. 2004. Sellafield-derived anthropogenic 14C in the marine intertidal environment of the NE Irish Sea. Radiocarbon 46(2):877–83.Google Scholar
Cresswell, GR. 2000. Coastal currents of northern Papua New Guinea, and the Sepik River outflow. Marine Freshwater Research 51:553–64.Google Scholar
Dye, T. 1994. Apparent ages of marine shells: implications for archaeological dating in Hawaii. Radiocarbon 36(1):51–7.Google Scholar
Edwards, RL, Beck, JW, Burr, GS, Donahue, DJ, Chappell, JMA, Bloom, AL, Druffel, ERM, Taylor, FW. 1993. A large drop in atmospheric 14C/12C and reduced melting in the younger Dryas, documented with 230Th ages of corals. Science 260(5110):962–8.Google Scholar
Green, RC, Anson, D. 2000. Excavations at Kainapirina (SAC), Watom Island, Papua New Guinea. New Zealand Journal of Archaeology 20(1998):29–94.Google Scholar
Guilderson, TP, Schrag, DP, Kashgarian, M, Southon, J. 1998. Radiocarbon variability in the western equatorial Pacific inferred from a high-resolution coral record from Nauru Island. Journal of Geophysical Research 103(C11):24,641–50.Google Scholar
Haberle, SG, David, B. 2004. Climates of change: human dimensions of Holocene environmental change in low latitudes of the PEPII transect. Quaternary International 118–119:165–79.Google Scholar
Hamel, JF, Mercier, A. 1996. The secret of the giant clam. Freshwater and Marine Aquarium 19(5):112.Google Scholar
Hogg, A, Higham, TFG, Dahm, J. 1998. Radiocarbon dating of modern marine and estuarine shellfish. Radiocarbon 40(2):975–84.Google Scholar
Hua, Q, Barbetti, M, Jacobsen, GE, Zoppi, U, Lawson, EM. 2000. Bomb radiocarbon in annual tree rings from Thailand and Australia. Nuclear Instruments and Methods in Physics Research B 172(1–4):359–65.Google Scholar
Hua, Q, Barbetti, M, Zoppi, U, Chapman, DM, Thomson, B. 2003. Bomb radiocarbon in tree rings from New South Wales, Australia: implications for dendrochronology, atmospheric transport, and air-sea exchange of CO2 . Radiocarbon 45(3):431–47.Google Scholar
Keith, ML, Anderson, GM, Eichler, R. 1964. Carbon and oxygen isotopic composition of mollusk shells from marine and fresh-water environments. Geochimica et Cosmochimica Acta 28(10–11):1757–86.Google Scholar
Kirch, PV. 2001. A radiocarbon chronology for the Mussau Islands. In: Kirch, PV, editor. Lapita and Its Transformations in Near Oceania: Archaeological Investigations in the Mussau Islands, Papua New Guinea, 1985–88. Volume 1 Introduction, Excavations, Chronology. Contribution No. 59. Archaeological Research Facility, University of California at Berkeley. p 196–222.Google Scholar
Kuroda, Y. 2000. Variability of currents of the northern coast of New Guinea. Journal of Oceanography 56(1):103–16.Google Scholar
Lindstrom, E, Butt, J, Lukas, R, Godfrey, S. 1990. The flow through Vitiaz Str. and St George's Channel, Papua New Guinea. In: Pratt, L, editor. The Physical Oceanography of Sea Straits. Dordtrecht: Kluwer Academic. p 171–89.Google Scholar
Mangerud, J, Bondevik, S, Gulliksen, S, Hufthammer, AK, Høisæter, T. 2006. Marine 14C reservoir ages for 19th century whales and molluscs from the North Atlantic. Quaternary Science Reviews 25(23–24):3228–45.Google Scholar
McCormac, FG, Hogg, AG, Blackwell, PG, Buck, CE, Higham, TFG, Reimer, PJ. 2004. SHCal04 Southern Hemisphere calibration, 0–11.0 cal kyr BP. Radiocarbon 46(3):1087–92.Google Scholar
McFadgen, BG. 1982. Dating New Zealand archaeology by radiocarbon. New Zealand Journal of Science 25:379–92.Google Scholar
McGregor, HV, Gagan, MK, McCulloch, MT, Hodge, E, Mortimer, G. 2008. Mid-Holocene variability in the marine 14C reservoir age for northern coastal Papua New Guinea. Quaternary Geochronology 3(3):213–25.Google Scholar
Nunn, PD. 2007. Climate, Environment and Society in the Pacific during the Last Millennium. Amsterdam: Elsevier.Google Scholar
Ortlieb, L, Vargas, G, Saliège, J-F. 2011. Marine radiocarbon reservoir effect along the northern Chile-southern Peru coast (14–24°S) throughout the Holocene. Quaternary Research 75(1):91–103.Google Scholar
Paterne, M, Ayliffe, LK, Arnold, M, Caioch, G, Tisnérat-Laborde, N, Hatté, C, Douville, E, Bard, E. 2004. Paired 14C and 230Th/U dating of surface corals from the Marquesas and Vanuatu (subequatorial Pacific) in the 3000 to 15,000 cal yr interval. Radiocarbon 46(2):551–6.Google Scholar
Petchey, F. 2009. Dating marine shell in Oceania: issues and prospects. In: Fairbairn, A, O'Connor, S, Marwick, B, editors. New Directions in Archaeological Science. Terra Austral is, 28. Canberra: Pandanus Books, Research School of Pacific and Asian Studies, ANU. p 157–72.Google Scholar
Petchey, F, Clark, G. 2010. A ΔR for the Palau Islands: an evaluation of extant and new ΔR values and their application to archaeological deposits at Ulong. Journal of Island Archaeology 5:236–52.Google Scholar
Petchey, F, Clark, G. 2011. Tongatapu hardwater: investigation into the 14C marine reservoir offset in lagoon, reef and open ocean environments of a limestone island. Quaternary Geochronology 6(6):539–49.Google Scholar
Petchey, F, Phelan, M, White, P. 2004. New ΔR values for the southwest Pacific Ocean. Radiocarbon 46(2):1005–14.Google Scholar
Petchey, F, Green, R, Jones, M, Phelan, M. 2005. A local marine reservoir correction value (ΔR) for Watom Island, Papua New Guinea. New Zealand Journal of Archaeology 26:29–40.Google Scholar
Petchey, F, Anderson, A, Zondervan, A, Ulm, S, Hogg, A. 2008. New marine ΔR values for the South Pacific Subtropical Gyre region. Radiocarbon 50(3):373–97.Google Scholar
Petchey, F, Allen, MS, Addison, D, Anderson, A. 2009. Stability in the South Pacific surface marine 14C reservoir over the last 750 years: evidence from American Samoa, the southern Cook Islands and the Marquesas. Journal of Archaeological Science 36(10):2234–43.Google Scholar
Reimer, PJ, McCormac, FG, Moore, J, McCormick, F, Murray, EV. 2002. Marine radiocarbon reservoir corrections for the mid- to late Holocene in the eastern subpolar North Atlantic. The Holocene 12(2):129–35.Google Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Buck, CE, Burr, GS, Edwards, RL, Friedrich, M, Grootes, PM, Guilderson, TP, Hajdas, I, Heaton, TJ, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, McCormac, FG, Manning, SW, Reimer, RW, Richards, DA, Southon, JR, Talamo, S, Turney, CSM, van der Plicht, J, Weyhenmeyer, CE. 2009. IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51(4):1111–50.Google Scholar
Rieth, TM, Hunt, TL, Lipo, C, Wilshurst, JM. 2011. The 13th century Polynesian colonization of Hawai'I Island. Journal of Archaeological Science 38(10):2740–9.Google Scholar
Sikes, EL, Samson, CR, Guilderson, TP, Howard, WR. 2000. Old radiocarbon ages in the southwest Pacific Ocean during the last glacial period and deglaciation. Nature 405(6786):555–9.Google Scholar
Specht, J. 2009. The aceramic to ceramic boundary in the Bismarck Archipelago. In: Sheppard, PJ, Thomas, T, Summerhayes, GR, editors. Lapita. Ancestors and Descendants. Auckland: New Zealand Archaeological Association Monograph 28. p 11–34.Google Scholar
Specht, J, Gosden, C. 1997. Dating Lapita Pottery in the Bismarck Archipelago, Papua New Guinea. Asian Perspectives 36(2):175–94.Google Scholar
Specht, J, Summerhayes, G. 2007. The Boduna Island (FEA) Lapita site. Archaeological studies of the Middle and Late Holocene, Papua New Guinea, Part II. Technical Reports of the Australian Museum 20:51–103.Google Scholar
Steinberg, CR, Choukroun, SM, Slivkoff, MM, Mahoney, MV, Brinkman, RM. 2006. Currents in the Bismarck Sea and Kimbe Bay, Papua New Guinea. Australian Institute of Marine Science and The Nature Conservancy. TNC Pacific Island Countries Report No 6/06.Google Scholar
Stuiver, M, Braziunas, TF 1993. Modeling atmospheric 14C influences and 14C ages of marine samples to 10,000 BC. Radiocarbon 35(1):137–89.Google Scholar
Stuiver, M, Pearson, GW, Braziunas, T. 1986. Radiocarbon age calibration of marine samples back to 9000 cal yr BP. Radiocarbon 28(2B):980–1021.Google Scholar
Stuiver, M, Reimer, PJ, Braziunas, TF. 1998. High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon 40(3):1127–51.Google Scholar
Summerhayes, GR. 2007. The rise and transformation of Lapita in the Bismarck Archipelago. In: Chui, S, Sand, C, editors. From Southeast Asia to the Pacific. Archaeological Perspectives on the Austronesian Expansion and the Lapita Cultural Complex. Taipei: Academic Sinica. p 129–72.Google Scholar
Summerhayes, G. 2010. Lapita interaction: an update. In: Gadu, M, Hsiuman, L, editors. 2009 International Symposium on Austronesian Studies. Taitong: National Museum of Prehistory. p 11–40.Google Scholar
Swift, MJ, Heal, OW, Anderson, JM. 1979. Decomposition in Terrestrial Ecosystems. Melbourne: Blackwell Scientific Publications.Google Scholar
Tanaka, N, Monaghan, MC, Rye, DM. 1986. Contribution of metabolic carbon to mollusc and barnacle shell carbonate. Nature 320(6062):520–3.Google Scholar
Ulm, S. 2002. Marine and estuarine reservoir effects in central Queensland, Australia: determination of ΔR values. Geoarchaeology: An International Journal 17(4):3119–48.Google Scholar
Ulm, S, Petchey, F, Ross, A. 2009. Marine reservoir corrections for Moreton Bay, Australia. Archaeology in Oceania 43(2):160–8.Google Scholar
White, JP. 2007. Ceramic sites on the Duke of York Islands. In: Specht, J, Attenbrow, V, editors. Archaeological Studies of the Middle and Late Holocene, Papua New Guinea. Technical Reports of the Australian Museum 20:3–50.Google Scholar
Wilmshurst, JM, Hunt, TL, Lipo, CP, Anderson, AJ. 2010. High-precision radio-carbon dating shows recent and rapid colonization of East Polynesia. Proceedings of the National Academy of Sciences of the USA 108:1815–20.Google Scholar
Yu, K, Hua, Q, Zhao, J-X, Hodge, E, Fink, D, Barbetti, M. 2010. Holocene marine 14C reservoir age variability: evidence from 230Th-dated corals in the South China Sea. Paleoceanography 25: PA3205, doi::10.1029/2009PA001831.Google Scholar