2169-1038D-4R 34.20-43.80 mbsf 2% recoveryoveryyyyScientific party of Leg 169October 1, 19966661҆$HHG(HHP'`@??GzG d?  (X*>n)Y+?o*Z,@p+[-Aq,\.Br-]/Cs.^0Dt/_1Eu0`2Fv1a3Gw2b4Hx3c5Iy4d6Jz5e7K{6f8L|7g 9M}8h :N~ 9i ;O :j <P ;k =Q <l>R =m?S>n@T?oAU@pBVAqCWBrDXCsEYDtFZEuG[FvH\GwI]HxJ^IyK_JzL`K{MaL|NbM}OcN~ PdO!Qe P"Rf!Q#Sg"R$Th#S%Ui$T&Vj%U'Wk&V(Xl'W)Ym !#650/$%&'(,-;<=>?@ABCDEFGHIJ8@@3333333@@3333333HwҀ xHҀ`ҁ  xHҀ,x72~`/<xP҂  " "<ҁ R4P҂ IW Interstitial Water҇ R4҂p   PAL Micropaleontologyҋ 2 13 FINE SANDSTONE and SILTY CLAYSTONE Major lithologies: In this core 10 cm of weakly indurated, olive gray (5Y 5/1), noncalcareous, FINE SANDSTONE overlies 10 cm of weakly indurated, gray (N 5), noncalareous, but highly altered SILTY CLAYSTONE. Black carbon "soot" is present on the water in the core voids.