Table 21. In situ temperature measurements in Hole 994C.

Core	Depth (mbsf)	Tool	Equil. Ta (degrees C)	Kb (W/[m*K])	Comments

2H	0	Adara	3.1 +/- 0.5		Mudline temperature stop
4H	32.9  	Adara	4.6 +/- 0.5	1.01
6H	51.9	Adara	5.7 +/- 0.25	0.89
10H	81.4	Adara	6.9 +/- 0.5	0.88
13H	109.9	Adara	8.2 +/- 0.25	1.08
16H	139.4	Adara	8.5 +/- 0.5	0.95
25X	203.3	WSTP	11.2 +/- 0.3	0.98	Switch to XCB coring
30X	241.7	WSTP	12.2 +/- 0.3	0.98
35X	299.4	WSTP	5.6	0.98	Anomalous
39X	318.6	WSTP	15.4 +/- 0.3	0.98
42X	347.6	WSTP	6.4	0.98	Anomalous
47X	386.1	WSTP	6.6	0.98	Anomalous; bent probe
52X	424.5	WSTP	8.3	0.98	Anomalous; thermistor malfunction during equilibration interval
55X	443.7	WSTP			Broke probe tip

Notes: Adara = Adara APC temperature shoe, and WSTP = water-sampling temperature probe.
a The equilibrium temperature reported here was obtained by minimizing the standard deviation between the synthetic equilibration curve and the recorded data during multiple processing runs.
 The value of equilibrium temperature for the anomalous runs actually represents the baseline value recorded during this equilibration interval. Errors are estimated based on factors discussed in the text.
b K indicates the average, corrected thermal conductivity value used to convert from depth to resistance. No laboratory thermal conductivity data were obtained in cores recovered from deeper than 210 mbsf, 
and 0.98 W/(m*K) was adopted for all in situ temperature measurements deeper than Core 164-994C-25X.