Oceanography The Official Magazine of
The Oceanography Society
Volume 25 Issue 03

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Volume 25, No. 3
Pages 118 - 119

SIDEBAR • Diving for the Sedimentary Record of Multiyear Sea Ice

Molly Fritz Miller Samuel S. BowserSally E. Walker
First Paragraph

How is sediment transported to the seafloor along coastlines where the sea ice rarely melts? Are there distinctive characteristics of the resulting deposits that label them as accumulating in this setting that is so sensitive to climate change?


Miller, M.F., S.S. Bowser, and S.E. Walker. 2012. Diving for the sedimentary record of multiyear sea ice. Oceanography 25(3):118–119, https://doi.org/10.5670/oceanog.2012.83.


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Broach, K.H., M.F. Miller, and S.S. Bowser. 2011. Rates and styles of bioturbation by the Antarctic scallop Adamussium colbecki and ophiuroid Ophionotus victoriae. P. 547 in 11th International Symposium on Antarctic Earth Sciences Programme and Abstracts. Available online at: http://www.isaes2011.org.uk/programme.html.

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Gooday, A.J., S.S. Bowser, and J.M. Bernhard. 1996. Benthic foraminiferal assemblages in Explorers Cove, Antarctica: A shallow-water site with deep-sea characteristics. Progress in Oceanography 37:117–166, https://doi.org/10.1016/S0079-6611(96)00007-9.

McClintock, J.B., L.B. Tackett, and S.S. Bowser. 2010. Video observations on non-swimming valve claps in the Antarctic scallop Adamussium colbecki. Antarctic Science 22:1–2, https://doi.org/10.1017/S0954102009990757.

Murray, K.T., M.F. Miller, and S.S. Bowser. 2012. Depositional processes beneath coastal multi-year sea ice. Sedimentology, https://doi.org/10.1111/j.1365-3091.2012.01345.x.

Stockton, W.L. 1984. The biology and ecology of the epifaunal scallop Adamussium colbecki on the west side of McMurdo Sound, Antarctica. Marine Biology 78:171–178, https://doi.org/10.1007/BF00394697.

Walker, B.J. 2011. Dissolution of ophiuroid ossicles (Ophionotus victoriae) in Explorers Cove, Antarctica: Implications for the Antarctic fossil record. Unpublished MS thesis, Vanderbilt University, 56 pp.