composition of the Laurentide Ice Sheet over Arctic Canada Subglacial carbonates constrain basal conditions and oxygen isotopic

[1]  G. Miller,et al.  Reorganization of ice sheet flow patterns in Arctic Canada and the mid‐Pleistocene transition , 2010 .

[2]  S. J. Birks,et al.  Isotopic evolution of Glacial Lake Agassiz: New insights from cellulose and porewater isotopic archives , 2007 .

[3]  A. Sima,et al.  Modeling the oxygen‐isotopic composition of the North American Ice Sheet and its effect on the isotopic composition of the ocean during the last glacial cycle , 2006 .

[4]  S. Marshall,et al.  Basal temperature evolution of North American ice sheets and implications for the 100‐kyr cycle , 2002 .

[5]  D. Pollard,et al.  Origin of the Middle Pleistocene Transition by ice sheet erosion of regolith , 1998 .

[6]  Sang-Tae Kim,et al.  Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates , 1997 .

[7]  P. Clark.  Unstable Behavior of the Laurentide Ice Sheet over Deforming Sediment and Its Implications for Climate Change , 1994, Quaternary Research.

[8]  R. Souchez,et al.  Subglacial carbonate deposition: An isotopic study of a present-day case , 1985 .

[9]  C. Hillaire-Marcel,et al.  Analyse isotopique de concrétions sous-glaciaires de l'inlandsis laurentidien et teneur en oxygène 18 de la glace , 1979 .

[10]  B. Hallet,et al.  Oxygen Isotope Composition of Subglacially Precipitated Calcite: Possible Paleoclimatic Implications , 1978, Science.

[11]  B. Hallet.  Deposits formed by subglacial precipitation of CaCO3 , 1976 .

[12]  Claes Rooth,et al.  Hydrology and ocean circulation , 1982 .

[13]  R. Lorrain,et al.  Isotopic composition of ice and subglacially precipitated calcite in an alpine area , 1982 .