Margin architecture reveals the transition to the modern Antarctic ice sheet ca. 3 Ma: Comment

Geology

Volumn 35, Issue 1, 2007, Pages

  Larter, Robert D ^a  

^a BRITISH ANTARCTIC SURVEY   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE VARIATION; ICE FIELD; ICE FLOW; ICE SHEET; LITERATURE REVIEW; TECTONIC SETTING;

EID: 67349102922     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/G23422C.1     Document Type: Note

References (10)

1. Bamber, J.L., Vaughan, D.G., and Joughin, I., 2000, Widespread complex fl ow in the interior of the Antarctic Ice Sheet: Science, v. 287, p. 1248-1250, doi: 10.1126/science.287.5456.1248.
2. Bart, P.J., and Anderson, J.B., 1995, Seismic record of glacial events affecting the northwestern Antarctic Peninsula, in Cooper, A.K., Barker, P.F., and Brancolini, G., eds., Geology and Seismic Stratigraphy of the Antarctic Margin: American Geophysical Union Antarctic Research Series, v. 68, p. 74-95.
3. Bart, P.J., Egan, D., and Warny, S.A., 2005, Direct constraints on Antarctic Peninsula ice sheet grounding events between 5.12 and 7.94 Ma: Journal of Geophysical Research, v. 110, p. F04008, doi: 10.1029/2004JF000254.
4. Hernández-Molina, F.J., Larter, R.D., Maldonado, A., and Rodríguez-Fernández, J., 2006, Evolution of the Antarctic Peninsula Pacifi c margin offshore from Adelaide Island since the Late Miocene: An example of a glacial passive margin: Terra Antarctica Reports, v. 12, p. 81-90.
5. Iwai, M., and Winter, D., 2002. Data report: Taxonomic notes on Neogene diatoms from the western Antarctic Peninsula: Ocean Drilling Program Leg 178, in Barker, P.F., et al., eds., Proceedings of the Ocean Drilling Program, Scientifi c Results, Volume 178: College Station, Texas, Ocean Drilling Program: http://www-odp.tamu.edu/publications/178_SR/chap_35/chap_35.htm (September 2006).
6. Larter, R.D., and Barker, P.F., 1989, Seismic stratigraphy of the Antarctic Peninsula Pacifi c margin: A record of Pliocene-Pleistocene ice volume and paleoclimate: Geology, v. 17, p. 731-734, doi: 10.1130/0091-7613 (1989)017<0731:SSOTAP>2.3.CO;2.
7. Larter, R.D., and Barker, P.F., 1991, Neogene interaction of tectonic and glacial processes at the Pacifi c margin of the Antarctic Peninsula, in Macdonald, D.I.M., ed., Sedimentation, Tectonics and Eustasy: International Association of Sedimentologists Special Publication, v. 12, p. 165-186.
8. Larter, R.D., Rebesco, M., Vanneste, L.E., Gambôa, L.A.P., and Barker, P.F., 1997, Cenozoic tectonic, sedimentary and glacial history of the continental shelf west of Graham Land, Antarctic Peninsula, in Barker, P.F., and Cooper, A.K., eds., Geology and Seismic Stratigraphy of the Antarctic Margin, 2: American Geophysical Union Antarctic Research Series, v. 71, p. 1-27.
9. Lavelle, M., Barker, P.F., and Osterman, L.E., 2002, Data report: Strontium isotope dating of barnacle fragments, Antarctic Peninsula Site 1103, in Barker, P.F. et al., eds., Proceedings of the Ocean Drilling Program, Scientifi c Results, Volume 178: College Station, Texas, Ocean Drilling Program: http://www-odp.tamu.edu/publications/178_SR/chap_27/chap_27.htm (September 2006).
10. Rebesco, M., Camerlenghi, A., Geletti, R., and Canals, M., 2006, Margin architecture reveals the transition to the modern Antarctic ice sheet ca. 3 Ma: Geology, v. 34, p. 301-304, doi: 10.1130/G22000.1.