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Late Pleistocene sea-level oscillations (MIS 10–2) recorded in shallow marine and coastal plain sediments of the southern Wanganui Basin, New Zealand

Published online by Cambridge University Press:  20 January 2017

Glenn R. Hughes  and
David M. Kennedy
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Abstract

The northern Wanganui Basin, New Zealand, is one of the key global sites for understanding marine cyclic sedimentation during the Quaternary. This paper presents the first evidence of marine cyclic sedimentation from its central-southern parts. Sedimentological, micropalaeontological and palynological analyses on a 280-m-deep borehole encountered units dating back to MIS 10. The sequence includes four marine cycles spanning MIS 9–5, which are overlain by terrestrial fluvial aggradation surfaces dating from MIS 4–2. Each marine unit represents a progressively shallowing depositional environment from the mid-shelf to coastal plain. This is overlain by a terrestrial sequence of lowstand fluvial terraces. Localized fault movements appear to have influenced the sedimentary character of the sequence during MIS 7a and 5e producing basement highs which provided protection to the shoreline. The cyclothems described in this paper now extend the already extensive, previously described record from MIS 17–10 to produce a combined eustatic record of Quaternary sea level change within the basin to MIS 5. They also provide an excellent example of the sedimentary response of a coastal basin to a progressive loss of sedimentation accommodation space.

Keywords

Late PleistoceneMarine isotope stageSea levelShallow marineSedimentary cycleWanganui basinCoastal plainGlacio-eustasy
Type
Articles
Information
Quaternary Research , Volume 71 , Issue 3 , May 2009 , pp. 477 - 489
Copyright
University of Washington

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References

Abbott, S.T. Mid-cycle condensed shell beds from mid-Pleistocene cyclothems, New Zealand: implications for sequence architecture. Sedimentology 44, (1997). 805–824.CrossRefGoogle Scholar
Abbott, S.T., and Carter, R.M. The sequence architecture of mid-Pleistocene (c. 1.1–0.4 Ma) cyclothems from New Zealand: facies development during a period of orbital control on sea-level cyclicity. De Boer, P.L., Smith, D.G. Orbital Forcing and Cyclic Sequences 19, (1994). Special Publication of the International Association of Sedimentologists, 367–394.CrossRefGoogle Scholar
Aharoni, E., (1991). Seismic reflection study across the Horowhenua coastal plain, North Island, New Zealand. Unpublished MSc Thesis. Victoria University of Wellington, Wellington., 169 pp.Google Scholar
Anderton, P.W. Structure and evolution of the South Wanganui Basin. New Zealand: New Zealand Journal of Geology and Geophysics 24, (1981). 39–63.Google Scholar
Barnett, R., (1994). Upper Quaternary stratigraphy in the Otaki Distric. Unpublished BSc (Hons) Thesis. Victoria University of Wellington, Wellington., 82 pp.Google Scholar
Begg, J.G., and Johnston, M.R. Geology of the Wellington Area. Geological map 10. Institute of Geological and Nuclear Sciences. (2000). Lower Hutt, 64 Google Scholar
Berryman, K.R., and Hull, A. Tectonic controls on Late Quaternary shorelines: a review and prospects for future research. Goff, J.R., Nichol, S.L., and Rouse, H.L. The New Zealand Coast. (2003). Dunmore Press, Palmerston North. 25–58.Google Scholar
Beu, A.G., and Edwards, A.R. New Zealand Pleistocene and late Pliocene glacio-eustatic cycles. Palaeogeography, Palaeoclimatology, Palaeoecology 46, (1984). 119–142.CrossRefGoogle Scholar
Beu, A.G., and Maxwell, P.A. Cenozoic Molluscs of New Zealand. New Zealand Geological Survey Paleontological Bulletin 58, (1990). 518 Google Scholar
Bryant, V.M., Holloway, R.G., Jones, J.G., and Carlson, D.L. Pollen preservation in alkaline soils of the American Southwest. Traverse, A. Sedimentation of Organic Particles. (1994). Cambridge University Press, Cambridge. 47–58.Google Scholar
Bussell, M.R. Palynological evidence for upper Putikian (middle Pleistocene) interglacial and glacial climates at Rangitawa Stream, South Wanganui Basin, New Zealand. New Zealand Journal of Geology and Geophysics 29, (1986). 471–479.CrossRefGoogle Scholar
Bussell, M.R., and Pillans, B. Vegetational and climatic history during oxygen isotope stage 7 and early stage 6, Taranaki, New Zealand. Journal of the Royal Society of New Zealand 27, (1997). 419–438.CrossRefGoogle Scholar
Carter, R.M., and Naish, T.R. A Review of Wanganui Basin, New Zealand: global reference section for shallow marine, Plio-Pleistocene (2.5–0Ma) Cyclostratigraphy. Sedimentary Geology 122, (1998). 37–52.CrossRefGoogle Scholar
Carter, R.M., Abbott, S.T., Fulthorpe, C.S., Haywick, D.W., and Henderson, R.A. Application of global sea-level and sequence-stratigraphy models in Southern Hemisphere Neogene strata from New Zealand. Special Publication of the International Association of Sedimentologists 12, (1991). 41–65.Google Scholar
Chappell, J., Omura, A., Esat, T., McCulloch, M., Pandolfi, J., Ota, Y., and Pillans, B. Reconciliation of late Quaternary sea levels derived from coral terraces at Huon Peninsula with deep sea oxygen isotope records. Earth and Planetary Science Letters 141, (1996). 227–236.CrossRefGoogle Scholar
Clifton, H.E., Hunter, R.E., and Gardner, J.V. Analysis of eustatic, tectonic and sedimentologic influences on transgressive and regressive cycles in the Upper Cenozoic Merced Formation, San Francisco, California. Kleinspehn, K.L., and Paola, C. New Perspectives In Basin Analysis. (1988). Springer-Verlag, New York. 109–128.Google Scholar
Cowie, J.D. Dune-building phases in the Manawatu District: New Zealand. Journal of Geology and Geophysics 6, (1963). 268–280.CrossRefGoogle Scholar
Cranwell, L.M. New Zealand Pollen Studies: The Monocotyledons. Bulletin of the Auckland Institute and Museum. (1953). Harvard University Press, Cambridge. 19–29.Google Scholar
Dunbar, G.B., and Barrett, P.J. Estimating paleobathymetry of wave-graded continental shelves using sediment texture. Sedimentology 52, (2005). 253–269.CrossRefGoogle Scholar
Fleming, C.A. The geology of Wanganui subdivision. New Zealand Geological Survey Bulletin 52, (1953). 361 Google Scholar
Fleming, C.A. The contribution of C14 dates to the Quaternary geology of the ‘golden coast', western Wellington. Tuatara 19, (1972). 61–69.Google Scholar
Froggatt, P.C. Toward a comprehensive Upper Quaternary tephra and ignimbrite stratigraphy in New Zealand using electron microprobe analysis of glass shards. Quaternary Research 19, (1983). 188–200.CrossRefGoogle Scholar
Hayward, B.W., and Hollis, C.J. Brackish Foraminifera in New Zealand: a taxonomic and ecologic review. Micropaleontology 40, (1994). 185–222.CrossRefGoogle Scholar
Hayward, B.W., Grenfell, H.R., Reid, C.M., and Hayward, K.A. Recent New Zealand shallow-water benthic Foraminifera: taxonomy, ecological distribution, biogeography, and use in paleoenvironmental assessment. Institute of Geological and Nuclear Sciences monograph 21, (1999). 1–264.Google Scholar
Hesp, P.A., and Shepherd, M.J. Some aspects of the late Quaternary geomorphology of the lower Manawatu Valley, New Zealand. New Zealand Journal of Geology and Geophysics 21, (1978). 403–412.CrossRefGoogle Scholar
Holgate, G.P., (1985). Aspects of upper Quaternary stratigraphy of the Wanganui. Unpublished MSc (Hons) Thesis. Victoria University of Wellington, Wellington., 181 pp.Google Scholar
Kohn, B.P., Pillans, B., and McGlone, M.S. Zircon fission track ages for middle Pleistocene Rangitawa Tephra, New Zealand: stratigraphic and paleoclimate significance. Paleogeography, Paleoclimatology, Paleoecology 95, (1992). 73–94.CrossRefGoogle Scholar
Kummel, B., and Raup, D.M. Handbook of Paleontological Techniques. (1965). W H Freeman, San Francisco. 852 Google Scholar
Macphail, M.K., and McQueen, D.R. The value of New Zealand pollen and spores as indicators of Cenozoic vegetation and climates. Tuatara 26, (1983). 37–59.Google Scholar
McGlone, M.S. A late Quaternary pollen record from marine core P69, southeastern North Island, New Zealand. New Zealand Journal of Geology and Geophysics 44, (2001). 69–77.CrossRefGoogle Scholar
Moar, N.T. Pollen Grains Of New Zealand Dicotyledonous Plants. (1993). Manaaki Whenua Press, Lincoln. 200 Google Scholar
Moore, P.D., Webb, J.A., and Collinson, M.E. Pollen Analysis Second Edition. (1991). Blackwell Scientific Publications, Boston. 216 Google Scholar
Murray-Wallace, C. Pleistocene coastal stratigraphy, sea-level highstands and neotectonism of the southern Australian passive continental margin — a review. Journal of Quaternary Science 17, (2002). 469–489.CrossRefGoogle Scholar
Naish, T., and Kamp, P.J.J. Sequence stratigraphy of sixth-order (41 k.y.) Pliocene–Pleistocene cyclothems, Wanganui basin, New Zealand: a case for the regressive systems tract. Geological Society of America Bulletin 109, (1997). 978–999.2.3.CO;2>CrossRefGoogle Scholar
Naish, T., and Kamp, P.J.J. Foraminiferal depth paleoecology of Late Pliocene shelf sequences and systems tracts, Wanganui Basin, New Zealand. Sedimentary Geology 110, (1997). 237–255.CrossRefGoogle Scholar
Naish, T.R. New Zealand's shallow-marine record of Pliocene-Pleistocene global sea-level and climate change. Journal of the Royal Society of New Zealand 35, (2005). 1–8.CrossRefGoogle Scholar
Naish, T.R., Abbott, S.T., Alloway, B.V., Beu, A.G., Carter, R.M., Edwards, A.R., Journeaux, T.D., Kamp, P.J.J., Pillans, B.J., Saul, G., and Woolfe, K.J. Astronomical calibration of a southern hemisphere plio-pleistocene reference section, Wanganui Basin, New Zealand. Quaternary Science Reviews 17, (1998). 695–710.CrossRefGoogle Scholar
Perrett, T.L., (1990). Variations in sediment texture and biota off a wave dominated coastline, Peka Peka Beach, New Zealand. Unpublished MSc (Hons) Thesis. Victoria University of Wellington, Wellington., 135 pp.Google Scholar
Pillans, B. Upper Quaternary marine terrace chronology and deformation, South Tarakani, New Zealand. Geology 11, (1983). 292–297.2.0.CO;2>CrossRefGoogle Scholar
Pillans, B. Loess chronology in Wanganui Basin, New Zealand. Eden, D.N., and Furkert, R.J. Loess, its Distribution, Geology, and Soils. (1988). Balkema, Rotterdam. 175–191.Google Scholar
Pillans, B. Direct marine-terrestrial correlations, Wanganui Basin, New Zealand: the last 1 million years. Quaternary Science Reviews 13, (1994). 189–200.CrossRefGoogle Scholar
Pillans, B., Holgate, G., and McGlone, M. Climate and sea level during oxygen isotope stage 7b: on-land evidence from New Zealand. Quaternary Research 29, (1988). 176–185.CrossRefGoogle Scholar
Pocknall, D.T. Pollen morphology of New Zealand species of Dacrydium (Solander), Podocarps (Heriter) and Dacrydioides (Endlicher). New Zealand Journal of Botany 19, (1981). 67–94.CrossRefGoogle Scholar
Posamentier, H.W., and Vail, P.R. Eustatic controls on clastic deposition 2. Wilgus, C.K. Sea Level Changes: An Integrated Approach 42, (1988). SEPM Special Publication, 124–154.Google Scholar
Reinson, G.E. Transgressive barrier island and estuarine systems. Walker, R.G., and James, N.P. Facies Models: Response to Sea Level Change. (1992). Geological Association of Canada, 179–194.Google Scholar
Saul, G., Naish, T.R., Abbott, S.T., and Carter, R.M. Sedimentary cyclicity in the marine Pliocene–Pleistocene of the Wanganui Basin (New Zealand): sequence stratigraphy motifs characteristic of the past 2.5m.y. GSA Bulletin 111, (1999). 524–537.2.3.CO;2>CrossRefGoogle Scholar
Seward, D. Tephrostratigraphy of the marine sediments in the Wanganui Basin, New Zealand. New Zealand Journal of Geology and Geophysics 19, (1976). 9–20.CrossRefGoogle Scholar
Shackleton, N.J. Oxygen isotopes, ice volume and sea level. Quaternary Science Reviews 6, (1987). 183–190.CrossRefGoogle Scholar
Shackleton, N.J., Berger, A., and Peltier, W.R. An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677. Transactions of the Royal Society of Edinburgh 81, (1990). 251–261.CrossRefGoogle Scholar
Shepherd, M.J. Holocene alluviation and transgressive dune activity in the lower Manawatu Valley, New Zealand. New Zealand Journal of Geology and Geophysics 30, (1987). 175–187.CrossRefGoogle Scholar
Tokuhashi, S., and Kondo, Y. Sedimentary cycles and environments in the middle-late Pleistocene Shimosa Group, Boso Peninsula, central Japan. Journal of the Geological Society of Japan 95, (1989). 933–951.Google Scholar
Thom, B.G. Transgressive and regressive stratigraphies of coastal sand barriers in southeast Australia. Marine Geology 56, (1983). 137–158.CrossRefGoogle Scholar