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Late Pleistocene Sea Level History of Bermuda

Published online by Cambridge University Press:  20 January 2017

Russell S. Harmon ,
Henry P. Schwarcz  and
Derek C. Ford
Russell S. Harmon
Affiliation:
Department of Geology, Michigan State University, East Lansing, Michigan 48824, U.S.A.
Henry P. Schwarcz
Affiliation:
Department of Geology, McMaster University, Hamilton, Ontario L8S 4MI, Canada
Derek C. Ford
Affiliation:
Department of Geography, McMaster University, Hamilton, Ontario L8S 4MI, Canada
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Abstract

The timing of eustatic sea level fluctuations over the vertical range + 15 to −11 m has been deduced from 230Th/234U dating of Bermudan corals and speleothems. On this tectonically stable carbonate island, interglacial periods are characterized by platform submergence, development of patch reefs, and the deposition of littoral and eolian carbonates, whereas glacial periods are times of platform emergence, carbonate diagenesis, soil development, and the deposition of speleothems in caves extending below present sea level. Interglacial periods are observed at about 200,000, 130,000 to 90,000, and 10,000 yr BP to present. The sea level history of the last interglacial period (130,000 to 90,000 yr BP) is complex, consisting of at least two short, distinct episodes of high sea stand (at 125,000 and 97,000 yr BP) superimposed on a longer period of general platform submergence. The sea level data derived from this study are compatible with those from other stable areas such as the Bahamas, but in addition suggest that eustatic sea level changes can be rapid, on the order of 5 to 10 m/1000 yr.

Type
Original Articles
Information
Quaternary Research , Volume 9 , Issue 2 , March 1978 , pp. 205 - 218
Copyright
University of Washington

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References

Bender, M.L., Taylor, F.T., Matthews, R.K., 1973. Helium-uranium dating of corals from Middle Pleistocene Barbados reef tracts. Quaternary Research. 3, 142 146.Google Scholar
Blackburn, G., Taylor, R.M., 1969. Limestones and red soils of Bermuda. Geological Society of America Bulletin. 80, 1595 1598.Google Scholar
Bloom, A.L., 1971. Glacial eustatic and isostatic controls of sea level since the last glaciation. Turekian, K.K., Late Cenozoic Glacial Ages. Yale University Press, New Haven, 355 379.Google Scholar
Bloom, A.L., Broecker, W.S., Chappell, J.M.A., Matthews, R.K., Mesolella, K.J., 1974. Quaternary sea level fluctuations on a tectonic coast: New 230Th/234U dates from the Huon Peninsula, New Guinea. Quaternary Research. 4, 184 205.Google Scholar
Bretz, J.H., 1960. Bermuda: A partially drowned late-mature Pleistocene karst. Geological Society of America Bulletin. 71, 1729 1754.Google Scholar
Bricker, O.P., Mackenzie, F.T., 1970. Limestones and red soils of Bermuda: Discussion. Geological Society of America Bulletin. 81, 2523 2524.Google Scholar
Chappell, J.M.A., 1974. Geology of coral terraces, Huon Peninsula, New Guinea: A study of the Quaternary tectonic movements and sea level changes. Geological Society of America Bulletin. 85, 553 570.Google Scholar
Dreimanis, A., Goldthwait, R.P., 1973. Wisconsin glaciation in the Huron, Erie, and Ontario lobes. Geological Society of America Memoir. 136, 71 105.Google Scholar
Emiliani, C., 1971. The last interglacial paleotemperatures and chronology. Science. 171, 571 573.CrossRefGoogle ScholarPubMed
Fairbridge, R.W., 1961. Eustatic changes in sea level. Physics and Chemistry of the Earth. 4, 99 185.CrossRefGoogle Scholar
Frye, J.C., Willman, H.B., 1973. Wisconsinan climatic history interpreted from Lake Michigan lobe deposits and soils. Geological Society of America Memoir. 136, 135 152.CrossRefGoogle Scholar
Gees, R.A., 1969. The age of the Bermuda seamount. Maritime Sediments. 5, 56 57.Google Scholar
Ginsburg, R.N., Schroeder, J.H., Shinn, E.A., 1971. Recent synsedimentary cementation in subtidal Bermuda reefs. Bricker, O.P., Carbonate Cements. John Hopkins Press, Baltimore, 54 58.Google Scholar
Goldberg, E.D., Bruland, K., 1974. Radioactive geochronologies. Goldberg, E.D., The Sea. Vol. 5, Wiley-Interscience, New York, 451 489.Google Scholar
Kaufman, A., Broecker, W.S., Ku, T.-L., Thurber, D.L., 1971. The status of U-series methods of mollusc dating. Geochimica et Cosmochimica Acta. 35, 1155 1183.CrossRefGoogle Scholar
Knox, A.S., 1940. The peat deposits of Bermuda and evidence of postglacial changes in sea level. Journal of Geology. 48, 767 780.Google Scholar
Ku, T.-L., Kimmel, M.A., Easton, W.H., O'Neill, T.J., 1974. Eustatic sea level 120,000 years ago on Oahu, Hawaii. Science. 183, 959 962.Google Scholar
Land, L.S., Mackenzie, F.T., Gould, S.J., 1967. Pleistocene history of Bermuda. Geological Society of America Bulletin. 78, 993 1006.CrossRefGoogle Scholar
Mesolella, K.J., Matthews, R.K., Broecker, W.S., Thurber, D.L., 1969. The astronomical theory of climatic change: Barbados Data. Journal of Geology. 77, 250 274.CrossRefGoogle Scholar
Neumann, A.C., 1969. Quaternary sea level data from Bermuda (Abstr.). 8th International Quaternary Congress Abstracts. 228 229.Google Scholar
Neumann, A.C., Moore, W.S., 1975. Sea level events and Pleistocene coral ages in the northern Bahamas. Quaternary Research. 5, 215 224.CrossRefGoogle Scholar
Plummer, L.N., Vacher, H.L., Mackenzie, F.T., Bricker, O.P., Land, L.S., 1976. Hydrogeochemistry of Bermuda: A case history of ground-water diagenesis of biocalcarenites. Geological Society of America Bulletin. 87, 1301 1316.2.0.CO;2>CrossRefGoogle Scholar
Ristvet, B.L., 1971. The progressive diagenetic history of Bermuda. Bermuda Biological Station Special Publication. 9, 118 157.Google Scholar
Ruhe, R.106., Cady, J.G., Gomez, R.S., 1961. Paleosols of Bermuda. Geological Society of America Bulletin. 72, 1121 1142.Google Scholar
Sayles, R.W., 1931. Bermuda during the Ice Age. Proceedings of American Academy of Arts and Science. 66, 381 467.Google Scholar
Shackleton, N.J., 1969. The last interglacial in the marine and terrestrial records. Proceedings of Royal Society of London, Series B. 174, 135 154.Google Scholar
Shackleton, N.J., Opdyke, N.D., 1973. Oxygen isotope and paleomagnetic stratigraphy of equatorial Pacific core V28-238: Oxygen isotope temperatures and ice volumes on a 105 and 106 year scale. Quaternary Research. 3, 39 55.CrossRefGoogle Scholar
Spalding, R.F., Matthews, T.D., 1972. Submerged stalagmites from caves in the Bahamas: Indicators of low sea level stand. Quaternary Research. 2, 470 472.Google Scholar
Spencer, M., 1967. Bahamas deep test. American Association of Petroleum Geologists, Bulletin. 51, 263 268.Google Scholar
Thompson, P., 1973. Procedures for extraction and isotopic analysis of uranium and thorium from speleothem. Department of Geology Technical Memorandum 73-9. McMaster University, Hamilton. Google Scholar
Upchurch, S.B., 1970. Sedimentation on the Bermuda platform. U. S. Lake Survey Reports. 2 12.Google Scholar
Vacher, L., 1973. Coastal dunes of younger Bermuda. Coates, D., Coastal Geomorphology. State University of New York Publications in Geomorphology. 355 391.Google Scholar
Veeh, H.H., Chappell, J.M.A., 1970. Astronomic theory of climatic change support from New Guinea. Science. 167, 862 865.Google Scholar
Verrill, A.E., 1907. The Bermuda Islands. IV. Geology and paleontology. Connecticut Academy of Arts and Sciences Transactions. 12, 45 348.Google Scholar
Walcott, R.I., 1973. Past sea level, eustasy, and deformation of the Earth. Quaternary Research. 2, 1 14.CrossRefGoogle Scholar