Table 24.  In situ temperature measurements in Holes 995A and 995B.						

Core	Depth (mbsf)	Tool	Equil. T a (C)	K b (W/[m*K])	Correction (counts)	Comments

164-995A-						
2H	0	Adara				Electronics failed
4H	20.7	WSTP				Thermistor leaked (#203)
4H	30.2	Adara	4.8 +/- 0.25	1.04		Reference mudline T = 2.9 degrees - 3.0 degrees C +/- 0.5 degrees C
6H	49.2	Adara	5.2 +/- 0.25 	1.07		
10H	78.7	Adara	7.3 +/- 0.50	0.93		Unsteady in-bottom record 
11H	78.7	WSTP	5.4 +/- 0.50	0.93	2800	Mudline T offset by +2.4 degrees C
13H	107.2	Adara	7.2 +/- 0.25			1.03
14H	107.2	WSTP	6.2 +/- 0.50	1.03	2800	Recorder began to fail; thermistor wet (#203)
16H	135.7	Adara	8.2 +/- 0.25	1.19		
20H	165.2	Adara	9.3 +/- 0.25	1		
21X	165.2	DVTP	8.4 +/- 0.75	1	7900	First deployment of new tool; multiple penetrations; thermistors off scale; switch to XCB coring
28X	223.9	WSTP	11.6 +/- 0.25	0.94	290	Recorder replaced; new thermistor (#208)
31X	269.1	WSTP			290	Bad penetration
34X	290.7	DVTP	12.4 +/- 0.75	0.94	7900	Two penetrations; thermistors off scale
35X	300.3	WSTP			450	High drift
39X	319.6	WSTP	13.9 +/- 0.50	0.94	650	Thermistor drifting (apparent)
42X	348.6	WSTP	15.2 +/- 0.50	0.94	1200	Thermistor drifting (apparent)
47X	387.1	WSTP	16.2 +/- 0.50	0.94	1200	

164-995B-						
4W1	109.5	WSTP	7.0 +/- 0.50	1.03	1200	Thermistor drifting (apparent)
4W2	155	WSTP				Tool in borehole water
4W3	200	WSTP	10.0 +/- 0.50	0.94	1500	Thermistor drifting (apparent)

"Notes: Adara = Adara APC temperature shoe; WSTP = water sampling temperature probe, and DVTP = Davis/Villinger Temperature Probe. T = temperature."						
"a The equilibrium temperature was determined by trial-and-error minimization of the misfit between the synthetic equilibration curve and the recorded data in temperature vs. F(alpha,t) space. "						
"The errors are assigned subjectively based on the magnitude of the correction applied to the data, the degree of in-bottom disturbance, and the tool used. "						
"b K indicates the average, uncorrected thermal conductivity value used to convert from depth to resistance. Because no laboratory thermal conductivity data are available for sediments recovered deeper than 210 mbsf at Sites 994 or 995, "
a value of 0.94 W/(m*K) was adopted for all in situ temperatures measured deeper than 200 mbsf.