Citation:

PANGAEA.143183

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Related to:

Murray, James W; Kuivila, K M (1990): Organic matter diagenesis in the northeast Pacific: transition from aerobic red clay to suboxic hemipelagic sediments. Deep-Sea Research Part A. Oceanographic Research Papers, 37(1), 59-80, https://doi.org/10.1016/0198-0149(90)90029-U

Project(s):

Silicon Cycling in the World Ocean (SINOPS)

Funding:

Fourth Framework Programme (FP4), grant/award no. MAS3970141 : Silicon Cycling in the World Ocean

Coverage:

Latitude: 35.011667 * Longitude: -127.953333

Date/Time Start: 1984-09-08T00:00:00 * Date/Time End: 1984-09-08T00:00:00

Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 0.340 m

Event(s):

TT183_4_BC * Latitude: 35.011667 * Longitude: -127.953333 * Date/Time: 1984-09-08T00:00:00 * Elevation: -4772.0 m * Campaign: * Basis: * Method/Device: Box corer (BC)

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Method/Device	Comment
1	DEPTH, sediment/rock	Depth sed	m			Geocode
2	Porosity, fractional	Poros frac		Murray, James W	Calculated from weight/volume
3	Carbon, organic, total	TOC	%	Murray, James W	Element analyser CHN, LECO
4	Carbon, total	TC	%	Murray, James W	Element analyser CHN, LECO
5	Carbon in carbonate	C (carb)	%	Murray, James W
6	Nitrate	[NO3]-	µmol/l	Murray, James W

License:

Creative Commons Attribution 3.0 Unported (CC-BY-3.0)

Size:

80 data points

Data

Download dataset as tab-delimited text — use the following character encoding:

1 Depth sed [m]	2 Poros frac	3 TOC [%]	4 TC [%]	5 C (carb) [%]	6 [NO3]- [µmol/l]
0.000					37.0
0.005	0.76	0.97	1.03	0.05	40.0
0.010					40.0
0.015	0.75	0.57	0.66	0.09	42.0
0.020					46.0
0.025	0.74	0.48	0.61	0.13	46.0
0.030					46.0
0.035	0.73	0.41	0.46	0.05	46.0
0.040					45.0
0.045	0.72	0.40	0.47	0.06	45.0
0.050					45.0
0.055	0.72
0.060					45.0
0.065	0.71
0.075	0.71	0.40	0.45	0.04	46.0
0.085	0.70	0.35	0.50	0.15
0.095	0.70				46.0
0.105	0.70	0.32	0.35	0.03
0.115	0.70
0.120					47.0
0.125	0.70
0.135	0.70	0.28	0.37	0.08
0.145	0.70
0.155	0.70			0.08
0.165	0.70	0.25	0.33	0.10
0.170					50.0
0.175	0.70	0.26	0.37	0.08
0.185	0.69	0.23	0.32	0.09
0.195	0.69	0.25	0.35	0.01
0.205	0.70
0.230					50.0
0.260					50.0
0.340					49.0