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  • Greg A. Ludvigson, Luis A. González, Ronald A. Metzger, Brian J. Witzke, Robert L. Brenner, Angela P. Murillo +1 other
  • 1998
Pedogenic carbonates from vadose soils form in areas of net water deficit, have δ 18 O values that are highly correlated with that of local meteoric water, and have been widely used as paleoclimate proxy records (Cerling and Quade, 1993). Paleo-climatic and paleohydrologic studies in humid continental settings, however, have been limited by the lack of(More)
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