Table 1. Summary of Leg 164 gas hydrate proxy measurements in sediment cores.
Hole | Core | Section | Interval (cm) |
Depth (mbsf) |
Gas hydrate indicator |
---|---|---|---|---|---|
994C |
4H |
5-7* |
90; 70* |
29.8-32.9 |
S (core photo) |
994C |
22X |
5 |
70-80 |
180.1 |
S (core photo) |
994C |
31X |
7 |
10-50 |
260.1 |
Recovered hydrate 10-cm thick |
994C |
32X |
1 |
0-25 |
261.1 |
S |
994C |
36P |
1 |
0-23 |
300.0 |
S (core photo) |
994D |
8X |
2 |
65-105 |
398.3 |
TA |
994C |
53P |
1 |
0-5 |
434.1 |
S (core photo) |
994C |
63X |
6 |
130-150 |
591.0 |
TA |
995A |
27P |
1 |
0-100 |
225.5 |
PCS gas, S, Cl- |
995A |
29X |
1 |
60-70 |
233.7 |
TA |
995A |
29X |
1 |
135-140 |
234.5 |
TA |
995A |
29X |
2 |
13-17 |
234.7 |
TA |
995A |
30X |
1 |
60-110 |
243.3 |
TA |
995A |
32X |
1 |
133-150 |
263.3 |
TA (frozen sediment, S) |
995A |
36P |
1 |
15-40 |
300.6 |
S (core photo), Cl- |
995B |
10P |
1 |
0-68 |
319.9 |
S (core photo), Cl- |
995A |
45P |
1 |
0-60 |
376.5 |
PCS gas |
995B |
11X |
4 |
15 |
414.5 |
Small wafer of gas hydrate |
995A |
54X |
CC |
0-20 |
444.9 |
TA |
997A |
25P |
1 |
0-78 |
202.9 |
S |
997A |
28X |
CC |
0-26 |
231.3 |
TA |
997A |
29X |
2 |
0-10 |
234.3 |
TA |
997A |
32X |
4 |
255-256.5 |
256.0 |
TA |
997A |
42X |
3 |
330-331.1 |
330.6 |
Massive hydrate, S, TA, Cl- |
997A |
49P |
1 |
0-50 |
395.4 |
S |
997A |
51P |
1 |
0-20 |
404.9 |
S |
997B |
6P |
1 |
0-26 |
433.6 |
S (core photo) |
997A |
55P |
1 |
0-40 |
433.8 |
S |
997B |
11X |
1-5 |
463-472 |
TA (below BSR) attributed to gas expansion |
|
997B |
12X |
1-4 |
472-482 |
TA (below BSR) attributed to gas expansion |
|
997B |
13X |
1-4 |
482-491 |
TA (below BSR) attributed to gas expansion |
|
997B |
15P |
1 |
0-10 |
501.0 |
S (core photo) |
997B |
16X |
1-7 |
501-510 |
TA (below BSR) attributed to gas expansion |
Notes: Interval depths given at the interval start unless otherwise noted. * = for Core 4H, measurements were taken from Section 5, 90 cm, through Section 7, 70 cm. S = soupy sediments noted in notebooks or, where indicated, in core photos; TA = core temperature anomaly (much colder than surrounding sediment or frozen, as noted); PCS gas = pressure coring system methane saturation within gas hydrate-stability field; Cl- = chlorinity anomaly; BSR = bottom-simulating reflection.