Table T4. Summary of Leg 202 geochemistry.
Region
Site
Water
depth
(m)
Sulfate
concentration
minimum
(mM)
Depth
(mcd)
Alkalinity
concentration
maximum
(mM)
Depth
(mcd)
Phosphate
concentration
maximum
(µM)
Depth
(mcd)
Ammonium
concentration
maximum
(mM)
Depth
(mcd)
Methane
concentration
maximum
(ppmv)
Shallowest
depth
(mcd)
Calcium
concentration
minimum
(mM)
Depth (mcd)
Limited to no sulfate reduction













Nazca Ridge 1236 1323 <26 170-191 2.2 2 3 <0.005 BDL
Increases with depth

1237 3212 <26 5-63 >5 9-20 9 5 >0.25 9-33 8 42-63 Increases with depth
Cocos Rise 1241 2027 Little depletion >5 63-95 5 3 >0.4 53-106 13 189 Increases with depth
Intermediate sulfate reduction













Carnegie Ridge 1238 2203 <10 75 >17 83-93 >15 10-64 3 82-386 <100
6.1 54
Panama Basin* 1240 2921 <15 135-200 >17 147-190 >30 147-190 >2 147-200 57 147 <3.5 104-179
Complete sulfate reduction













Chile Basin 1232 4072 <2 26 >30 26-159 >50 Throughout >2 37 >10,000 >60 <6 27













<4 93-105
Chile margin 1233 838 BDL 21 >60 21-44 >210 11-55 >5 11-77 High 23 <2 5-11

1234 1015 BDL 10 >63 18-52 >120 10-52 >11 40-88 High 9 <2 10-112

1235 489 BDL 20 >60 31-42 >200 20-42 >8 31-42 High 20 <2 20-109
Carnegie Ridge 1239 1414 BDL 71 >28 92-123 >20 61-113 >6 133-378 Moderate-high 100 5.5 71-82
Cocos Rise 1242 1364 BDL 23 >25 23-94 60 34 >7.5 94-170 High 35 2.5 34

Notes: * = Site 1240 is influenced by fluid flow in the underlying basalt, and its geochemistry is discussed separately in the text as a consequence. BDL = below detection limit. Sulfate detection limit was typically 1 mM or lower.