Mottl, Michael J; Lawrence, James R; Keigwin, Lloyd D (1983): (Table 3) Composition of sediment pore water at DSDP Hole 69-505 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.816376, In supplement to: Mottl, MJ et al. (1983): Elemental and stable-isotope composition of pore waters and carbonate sediments from Deep Sea Drilling Project Sites 501/504 and 505. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 461-473, https://doi.org/10.2973/dsdp.proc.69.121.1983
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 1.913300 * Longitude: -83.790000
Date/Time Start: 1979-09-29T00:00:00 * Date/Time End: 1979-09-29T00:00:00
Minimum DEPTH, sediment/rock: 2.0 m * Maximum DEPTH, sediment/rock: 231.5 m
Event(s):
69-505 * Latitude: 1.913300 * Longitude: -83.790000 * Date/Time: 1979-09-29T00:00:00 * Elevation: -3537.0 m * Penetration: 242 m * Recovery: 187.1 m * Location: North Pacific/GRABEN * Campaign: Leg69 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 26 cores; 223 m cored; 0 m drilled; 83.9 % recovery
Comment:
Sediment depth is given in mbsf. All samples squeezed from sediment were at 6.8 to 10.5 °C except water sample 69-505-35 (which was at 14°C).
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
358 data points
Data
1 Sample label | 2 Depth sed [m] | 3 ID | 4 Comment | 5 pH | 6 Sal | 7 cl [mmol/l] | 8 AT [mmol(eq)/l] | 9 [SO4]2- [mmol/l] | 10 Na [mmol/l] | 11 K [mmol/l] | 12 Ca [mmol/l] | 13 Mg [mmol/l] | 14 Sr [µmol/l] | 15 Li [µmol/l] | 16 Fe [µmol/l] | 17 Mn [µmol/l] | 18 NH3 [µmol/l] | 19 Si [µmol/l] | 20 δ18O H2O [‰ SMOW] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
69-505-2-1,144-150 | 2.0 | 20 | 7.71 | 34.6 | 552.8 | 3.04 | 28.50 | 474.3 | 12.26 | 10.23 | 52.67 | 85.4 | 28.0 | 5.30 | 105.00 | <50 | 548 | ||
69-505-2-3,144-150 | 5.0 | 21 | 7.64 | 34.6 | 557.4 | 4.27 | 27.86 | 478.6 | 12.37 | 9.88 | 53.02 | 83.9 | 26.7 | 1.20 | 103.00 | 203 | 687 | ||
69-505-2-5,144-150 | 8.0 | 22 | 7.53 | 34.4 | 558.3 | 3.98 | 27.93 | 479.6 | 12.12 | 9.91 | 52.99 | 89.2 | 26.5 | 1.96 | 92.90 | 186 | 674 | 0.0 | |
69-505-3-3,140-150 | 14.5 | 23 | 7.40 | 34.6 | 561.1 | 6.85 | 25.99 | 481.2 | 12.11 | 8.40 | 54.44 | 88.8 | 27.9 | 3.95 | 80.50 | 496 | 704 | 0.2 | |
69-505-4-6,140-150 | 28.5 | 24 | 7.29 | 34.4 | 562.9 | 8.93 | 23.35 | 484.2 | 12.20 | 6.20 | 54.32 | 87.2 | 26.5 | 1.71 | 39.70 | 786 | 758 | 0.3 | |
69-505-5-3,140-150 | 33.5 | 25 | 7.29 | 34.6 | 561.1 | 9.41 | 22.83 | 482.9 | 12.41 | 5.95 | 53.90 | 86.6 | 27.4 | 2.22 | 36.60 | 842 | 746 | 0.0 | |
69-505-6-3,0-10 | 41.6 | 26 | 7.27 | 34.4 | 562.0 | 8.38 | 23.72 | 484.2 | 12.09 | 6.21 | 54.00 | 89.3 | 26.9 | 2.65 | 39.80 | 805 | 755 | -0.2 | |
69-505-9-2,140-150 | 70.0 | 27 | 7.29 | 34.2 | 562.9 | 13.26 | 18.96 | 484.0 | 11.91 | 3.74 | 54.57 | 83.8 | 24.2 | 1.98 | 17.70 | 1371 | 784 | ||
69-505-11-4,140-150 | 101.5 | 28 | 7.42 | 34.2 | 564.8 | 15.92 | 17.13 | 486.4 | 11.52 | 3.62 | 54.02 | 93.5 | 22.7 | 1.78 | 35.60 | 1504 | 822 | ||
69-505-14-4,140-150 | 130.0 | 29 | 7.21 | 34.2 | 562.9 | 13.19 | 17.87 | 482.0 | 11.37 | 3.63 | 54.57 | 98.1 | 21.9 | 2.96 | 16.30 | 1774 | 775 | -0.1 | |
69-505-17-5,140-150 | 169.5 | 30 | 7.19 | 34.2 | 566.6 | 10.31 | 18.77 | 485.2 | 11.44 | 4.21 | 53.92 | 108.0 | 22.3 | 2.71 | 9.60 | 1281 | 837 | ||
69-505-20-5,140-150 | 198.0 | 31 | 7.12 | 34.4 | 560.2 | 7.58 | 21.44 | 480.3 | 11.07 | 5.78 | 53.25 | 113.0 | 19.5 | 1.13 | 7.31 | 886 | 814 | ||
69-505-21-7,140-150 | 210.5 | 32 | 7.26 | 35.0 | 562.0 | 6.19 | 22.36 | 480.2 | 11.15 | 6.51 | 53.79 | 107.0 | 19.2 | 2.16 | 6.55 | 724 | 799 | -0.3 | |
69-505-22-5,140-150 | 217.0 | 33 | 7.25 | 34.5 | 564.8 | 5.06 | 23.80 | 483.0 | 11.60 | 7.14 | 53.87 | 107.0 | 20.4 | 2.09 | 5.18 | 587 | 768 | ||
69-505-23-5,140-150 | 226.5 | 34 | 7.30 | 35.2 | 563.8 | 3.85 | 25.61 | 483.0 | 11.67 | 8.32 | 53.49 | 98.3 | 21.3 | 1.03 | 4.32 | 334 | 786 | ||
69-505-24-2,140-150 | 231.5 | 35 | 7.48 | 34.2 | 553.3 | 1.22 | 26.54 | 471.8 | 12.53 | 8.39 | 53.07 | 83.3 | 22.9 | 1.11 | 9.51 | 142 | 635 | -0.2 | |
95.5 | IS-1, prime | 8.08 | 34.1 | 561.1 | 16.78 | 3.97 | 55.95 | 26.50 | 1250 | ||||||||||
95.5 | IS-1, overflow | Data have been normalized to the chlorinity of the prime aliquot, except for chlorinity and alkalinity (#). Alkalinity was calculated from the difference in Ca between the prime and normalized overflow aliquots | #172.0 | #18.54 | 23.23 | 492.5 | 10.41 | 4.85 | 55.95 | 82.0 | 30.5 | 22.70 | 878 | 250 | |||||
145.5 | IS-2, prime | 8.03 | 34.1 | 556.5 | 13.33 | 4.63 | 54.95 | 22.30 | 1087 | ||||||||||
IS-2, overflow | Data have been normalized to the chlorinity of the prime aliquot, except for chlorinity and alkalinity (#). Alkalinity was calculated from the difference in Ca between the prime and normalized overflow aliquots | 34.2 | #367.0 | #14.13 | 20.64 | 480.2 | 10.27 | 5.03 | 54.95 | 105.0 | 23.8 | 18.70 | 544 | 584 | |||||
145.5 | IS-3e | Data for pH, salinity, chlorinity, alkalinity, Ca, Mg, Mn, and NH3 are from the prime aliquot. Other data are from the overflow aliquot normalized to the chlorinity of the prime aliquot. Mg is identical in both aliquots | 8.10 | 34.2 | 555.5 | 10.68 | 20.93 | 478.0 | 10.25 | 5.99 | 53.29 | 115.0 | 23.7 | 17.50 | 928 | 670 | |||
211.0 | IS-4e | Data for pH, salinity, chlorinity, alkalinity, Ca, Mg, Mn, and NH3 are from the prime aliquot. Other data are from the overflow aliquot normalized to the chlorinity of the prime aliquot. Mg is identical in both aliquots | 7.83 | 556.5 | 6.64 | 24.92 | 478.5 | 10.69 | 8.12 | 53.32 | 114.0 | 22.3 | 11.70 | 603 | 651 |