Chronostratigraphy of sediment core CRP-2/2A (Table 1), supplement to: Wilson, Gary S; Bohaty, Steven M; Fielding, Christopher R; Florindo, Fabio; Hannah, Mike J; Harwood, David M; McIntosh, W C; Naish, Tim R; Roberts, Andrew P; Sagnotti, Leonardo; Scherer, Reed P; Strong, C Percy; Versub, K L; Villa, Giuliana; Watkins, David K; Webb, Peter-Noel; Woolfe, Ken (2000): Chronostratigraphy of CRP-2/2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(4), 647-654

Gary S Wilson, Steven M Bohaty, Christopher R Fielding, Fabio Florindo, Mike J Hannah, David M Harwood, W C McIntosh, Tim R Naish, Andrew P Roberts, Leonardo Sagnotti, Reed P Scherer, C Percy Strong, K L Versub, Giuliana Villa, David K Watkins, Peter-Noel Webb & Ken Woolfe
The 624.15 m glaciomarine sedimentary succession recovered in the CRP-2/2A drillcore comprises lower Oligocene (1000 m/m.y.). Between 306.65 mbsf and the bottom of the drillcore (624.15 mbsf), fewer datums are available to constrain the age model and unique correlation with the MPTS is not possible, although high average sediment accumulation rates are likely. A significant unconformity is identified at 306.65 mbsf, which may represent as much as 5 m.y. of missing time. Additional unconformities at...
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