Hostname: page-component-78c5997874-mlc7c Total loading time: 0 Render date: 2024-11-02T20:34:07.509Z Has data issue: false hasContentIssue false

Revisiting late Holocene sea-level change from the Gilbert Islands, Kiribati, west-central Pacific Ocean

Published online by Cambridge University Press:  18 September 2017

Hiroya Yamano*
Affiliation:
Center for Environmental Biology and Ecosystem Studies, National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki 305-8506, Japan
Hajime Kayanne
Affiliation:
Department of Earth and Planetary Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo 113-0033, Japan
Toru Yamaguchi
Affiliation:
Department of Ethnology and Archaeology, Keio University, 2-15-45 Mita, Minato, Tokyo 108-8345, Japan
Tomomi Inoue
Affiliation:
Center for Environmental Biology and Ecosystem Studies, National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki 305-8506, Japan
Yukira Mochida
Affiliation:
Kanagawa Study Center, The Open University of Japan, 2-31-1 O-oka, Minami, Yokohama 232-8510, Japan Makino Herbarium (MAK), Tokyo Metropolitan University, 1-1 Minami-osawa, Hachioji, Tokyo 192-0397, Japan
Shigeyuki Baba
Affiliation:
International Society for Mangrove Ecosystems, c/o Faculty of Agriculture, University of the Ryukyus, Nishihara, Okinawa 903-0219, Japan
*
*Corresponding author at: Center for Environmental Biology and Ecosystem Studies, National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki 305-8506, Japan. E-mail address: [email protected] (H. Yamano).

Abstract

New coral microatoll data allow presenting an updated late Holocene sea-level curve for the Gilbert Islands of Kiribati. Examination of build-up elevation and spatial distribution of microatolls, along with radiocarbon age data from coral samples, suggest an approximately 1 m sea-level high stand, possibly lasting from ~3500 to 1900 cal yr BP. Our sea-level curve, which is similar to the one reported from the Marshall Islands, is a baseline to reconstruct the evolution of reef flats and reef islands. In addition, it provides important contextual data to infer human settlement on islands in the west-central Pacific.

Type
Research Article
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2017 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Andréfouët, S., Muller-Karger, F.E., Robinson, J.A., Kranenburg, C.J., Torres-Pulliza, D., Spraggins, S.A., Murch, B., 2006. Global assessment of modern coral reef extent and diversity for regional science and management applications: A view from space. In: Suzuki, Y., Nakamori, T., Hidaka, M., Kayanne, H., Casareto, B.E., Nadaoka, K., Yamano, H., Tsuchiya, M. (Eds.), Proceedings of the 10th International Coral Reef Symposium, 28 June to 2 July 2004. Japanese Coral Reef Society, Tokyo, pp. 17321745.Google Scholar
Australian Bureau of Meteorology. 2010. Pacific country report on sea level & climate: their present state, Kiribati. Available at http://www.bom.gov.au/oceanography/projects/spslcmp/country_report.shtml.Google Scholar
Baker, R.G.V., Haworth, R.J., 2000. Smooth or oscillating late Holocene sea-level curve? Evidence from the palaeo-zoology of fixed biological indicators in east Australia and beyond. Marine Geology 163, 367386.Google Scholar
Chappell, J., Polach, H.A., 1976. Holocene sea-level change and coral-reef growth at Huon Peninsula, Papua New Guinea. Geological Society of America Bulletin 87, 235240.Google Scholar
David, T.W.E., Sweet, G., 1904. The geology of Funafuti. In: Coral Reef Committee of the Royal Society (Ed.), The Atoll of Funafuti. Boring into a Coral Reef and the Results. The Royal Society of London, London, pp. 61124.Google Scholar
Dawson, J.L., Smithers, S.G., Hua, Q., 2014. The importance of large benthic foraminifera to reef island sediment budget and dynamics at Raine Island, northern Great Barrier Reef. Geomorphology 222, 6881.Google Scholar
Di Piazza, A., 1999. Te Bakoa site. Two old earth ovens from Nikunau Island (Republic of Kiribati). Archaeology in Oceania 34, 4042.Google Scholar
Dickinson, W.R., 1999. Holocene sea-level record on Funafuti and potential impact of global warming on central Pacific atolls. Quaternary Research 51, 124132.Google Scholar
Dickinson, W.R., 2003. Impact of mid-Holocene hydro-isostatic highstand in regional sea level on habitability of islands in Pacific Oceania. Journal of Coastal Research 19, 489502.Google Scholar
Environment and Conservation Division of Kiribati, 2011. Mangrove activities report 2010. Environment and Conservation Division, Tarawa, Kiribati.Google Scholar
Falkland, A.C., Woodroffe, C.D., 1997. Geology and hydrogeology of Tarawa and Christmas Island, Kiribati. In: Vacher H.I., Quinn, T. (Eds.), Geology and Hydrogeology of Carbonate Islands (Developments in Sedimentology 54. Elsevier, Amsterdam, pp. 577610.Google Scholar
Flora, C.J., Ely, P.S., Flora, A.R., 2009. Microatoll edge to ENSO annulus growth suggests sea level change. Atoll Research Bulletin 571, 110.Google Scholar
Grossman, E.E., Fletcher, C.H. III, Richmond, B.M., 1998. The Holocene sea-level highstand in the equatorial Pacific: analysis of the insular paleosea-level database. Coral Reefs 17, 309327.CrossRefGoogle Scholar
Harii, S, Kayanne, H., 2003. Larval dispersal, recruitment, and adult distribution of the brooding stony octocoral Heliopora coerulea on Ishigaki Island, southwest Japan. Coral Reefs 22, 188196.CrossRefGoogle Scholar
Kaplin, P.A., 1981. Relief, age and types of Oceanic islands. New Zealand Geographer 36, 312.Google Scholar
Kayanne, H., Suzuki, A., Saito, H., 1995. Diurnal changes in the partial pressure of carbon dioxide in coral reef water. Science 269, 214216.Google Scholar
Kayanne, H., Yasukochi, T., Yamaguchi, T., Yamano, H., Yoneda, M., 2011. Rapid settlement of Majuro Atoll, central Pacific, following its emergence at 2000 years CalBP. Geophysical Research Letters 38, L20405. http://dx.doi.org/10.1029/2011GL049163.CrossRefGoogle Scholar
Kench, P.S., McLean, R.F., Nichol, S.L., 2005. New model of reef-island evolution: Maldives, Indian Ocean. Geology 33, 145148.Google Scholar
Kench, P.S., Owen, S.D., Ford, M.R., 2014. Evidence for coral island formation during rising sea level in the central Pacific Ocean. Geophysical Research Letters 41, 820827.CrossRefGoogle Scholar
Kench, P.S., Smithers, S.G., McLean, L.F., 2012. Rapid reef island formation and stability over and emerging reef flat: Bewick Cay, northern Great Barrier Reef, Australia. Geology 40, 347350.CrossRefGoogle Scholar
Kench, P.S., Smithers, S.G., McLean, L.F., Nichol, S.L., 2009. Holocene reef growth in the Maldives: evidence of a mid-Holocene sea-level highstand in the central Indian Ocean. Geology 37, 455458.CrossRefGoogle Scholar
Kench, P.S., Thompson, D., Ford, M.R., Ogawa, H., McLean, R.F., 2015. Coral islands defy sea-level rise over the past century: records from a central Pacific atoll. Geology 43, 515518.Google Scholar
Kinsey, D.W., 1972. Preliminary observations on community metabolism and primary productivity of the pseudo-atoll reef at One Tree Island, Great Barrier Reef. In: Mukundan, C., Gopinadha Pillai, C.S. (Eds.), Proceedings of the 1st International Symposium on Corals and Coral Reefs, 12 to 16 January 1969. Marine Biological Association of India, Cochin, pp. 1332.Google Scholar
Lambeck, K., Rouby, H., Purcell, A., Sun, Y., Sambridge, M., 2014. Sea level and global ice volumes from the Last Glacial Maximum to the Holocene. Proceedings of the National Academy of Sciences of the United States of America 111, 1529615303.CrossRefGoogle ScholarPubMed
Lewis, S.E., Wüst, R.A.J., Webster, J.M., Shields, G.A., 2008. Mid-late Holocene sea-level variability in eastern Australia. Terra Nova 20, 7481.CrossRefGoogle Scholar
Maragos, J.E., Baines, G.B.K., Beveridge, P.J., 1973. Tropical cyclone Bebe creates a new land formation on Funafuti Atoll. Science 181, 11611164.Google Scholar
Marshall, J.F., Jacobson, G., 1985. Holocene growth of a mid-Pacific atoll: Tarawa, Kiribati. Coral Reefs 4, 1117.Google Scholar
McLean, R.F., Hosking, P.L., 1991. Geomorphology of reef islands and atoll motu in Tuvalu. South Pacific Journal of Natural Science 11, 167189.Google Scholar
McLean, R.F., Woodroffe, C.D., 1994. Coral atolls. In: Carter, R.W.G., Woodroffe, C.D. (Eds.), Coastal Evolution, Late Quaternary Shoreline Morphodynamics. Cambridge University Press, New York, pp 267302.Google Scholar
Meltzner, A.J., Woodroffe, C.D., 2015. Chapter 8: Coral microatolls. In: Shennan, I, Long, A.J., Horton, B.P. (Eds.), Handbook of Sea Level Research. John Wiley and Sons, Chichester, pp. 125145.Google Scholar
Mitrovica, J.X., Milne, G.A., 2002. On the origin of late Holocene sea-level highstands within equatorial ocean basins. Quaternary Science Reviews 21, 21792190.Google Scholar
Miyata, T., Maeda, Y., Matsumoto, E., Matsushima, Y., Rodda, P., Sugimura, A., Kayanne, H., 1990. Evidence for a Holocene high sea-level stand, Vanua Levu, Fiji. Quaternary Research 33, 352359.Google Scholar
Nakada, M., 1986. Holocene sea levels in oceanic islands: implications for the rheological structure of the Earth’s mantle. Tectonophysics 121, 263276.CrossRefGoogle Scholar
Nunn, P.D., 2000. Significance of emerged Holocene corals around Ovalau and Moturiki islands, Fiji, southwest Pacific. Marine Geology 163, 345351.Google Scholar
Nunn, P.D., 2016. Sea levels, shorelines and settlements on Pacific reef islands. Archaeology in Oceania 51, 9198.Google Scholar
Nunn, P.D., Peltier, W.R., 2001. Far-field test of the ICE-4G Model of global isostatic response to deglaciation using empirical and theoretical Holocene sea-level reconstructions for the Fiji islands, Southwestern Pacific. Quaternary Research 55, 203214.Google Scholar
Paulay, G., Kerr, A., 2001. Patterns of coral reef development on Tarawa Atoll, Kiribati. Bulletin of Marine Science 69, 11911207.Google Scholar
Perry, C.T., Kench, P.S., Smithers, S.G., Riegl, B., Yamano, H., O’Leary, M.J., 2011. Implications of reef ecosystem change for the stability and maintenance of coral reef islands. Global Change Biology 17, 36793696.CrossRefGoogle Scholar
Reimer, P.J., Reimer, R.W., 2001. A marine reservoir correction database and on-line interface. Radiocarbon 43, 461463.Google Scholar
Reimer, P.J., Bard, E., Bayliss, A., Beck, J.W., 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55, 18691887.CrossRefGoogle Scholar
Schofield, J.C., 1977. Late Holocene sea level, Gilbert and Ellice Islands, west central Pacific Ocean. New Zealand Journal of Geology and Geophysics 20, 503529.Google Scholar
Stuiver, M., Pollach, H.A., 1977. Discussion: reporting of 14C data. Radiocarbon 19, 355363.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., 1993. Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, 215230.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., Reimer, R.W., 2017. CALIB 7.1 [WWW program] (accessed August 16, 2017). http://calib.org.Google Scholar
Takayama, J., Takasugi, H., 1988. Archaeology on Makin, Kiribati, Central Pacific. Tezukayama University, Nara, Japan.Google Scholar
Tracey, J.I. Jr., Ladd, H.S., 1974. Quaternary history of Eniwetok and Bikini atolls, Marshall Islands. Proceeding of the Second Coral Reef Symposium 2, 537550.Google Scholar
Webb, A.P., Kench, P.S., 2010. The dynamic response of reef islands to sea-level rise: evidence from multi-decadal analysis of island change in the Central Pacific. Global and Planetary Change 72, 234246.Google Scholar
Weisler, M.I., Yamano, H., Hua, Q., 2012. A multidisciplinary approach for dating human colonization of Pacific atolls. Journal of Island and Coastal Archaeology 7, 102125.Google Scholar
Woodroffe, C.D., Morrison, R.J., 2001. Reef-island accretion and soil development on Makin, Kiribati, central Pacific. Catena 44, 245261.Google Scholar
Woodroffe, C.D., McGregor, H.V., Lambeck, K., Smithers, S.G., Fink, D., 2012. Mid-Pacific microatolls record sea-level stability over the past 5000 yr. Geology 40, 951954.CrossRefGoogle Scholar
Yamano, H., 2002. Sensitivity of reef flats and reef islands to sea-level change. In: Moosa, M.K., Soemodihardjo, S., Soegiarto, A., Romimohtarto, K., Nontji, A. (Eds.), Proceedings of the 9th International Coral Reef Symposium, 23–27 October 2000. International Society for Reef Studies, Honolulu, pp. 11931198.Google Scholar
Yamano, H., Cabioch, G., Chevillon, C., Join, J.-L., 2014. Late Holocene sea-level change and reef-island evolution in New Caledonia. Geomorphology 222, 3945.CrossRefGoogle Scholar
Yamano, H., Kayanne, H., Yamaguchi, T., Kuwahara, Y., Yokoki, H., Shimazaki, H., Chikamori, M., 2007. Atoll island vulnerability to flooding and inundation revealed by historical reconstruction: Fongafale Islet, Funafuti Atoll, Tuvalu. Global and Planetary Change 57, 407416.Google Scholar
Yamano, H., Kayanne, H., Yonekura, N., 2001. Anatomy of a modern coral reef flat: a recorder of storms and uplift in the late Holocene. Journal of Sedimentary Research 71, 295304.Google Scholar
Yasukochi, T., Kayanne, H., Yamaguchi, T., Yamano, H., 2014. Sedimentary facies and Holocene depositional process of Laura Island, Majuro Atoll. Geomorphology 222, 5967.Google Scholar