/* DATA DESCRIPTION:
Citation:	Alt, Jeffrey C; Burdett, James W (1992): (Table 1) Sulphur content and stable isotope ratios of ODP Leg 129 holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.779034, 
	Supplement to: Alt, JC; Burdett, JW (1992): Sulfur in pacific deep-sea sediments (Leg 129) and implications for cycling of sediment in subduction zones. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 283-294, https://doi.org/10.2973/odp.proc.sr.129.125.1992
Abstract:	The mineralogy of S-bearing phases, S-contents, and S-isotopic compositions of sediments and interstitial waters were determined for three cores drilled during Leg 129 in the western Pacific. Pelagic clays, chalks, and radiolarites generally contain 350-1200 ppm S, with essentially all S present as sulfate. Volcanogenic turbidite units contain about 400 ppm S, with about 10%-20% of total sulfur as pyrite-S and the remainder as sulfate. A single claystone from the base of Hole 802A has high pyrite-S content (1200 ppm) and contains a component of metalliferous sediment. The single analyzed chert has the highest sulfur content (4020 ppm) with essentially all sulfur present as pyrite-S. Sulfate in pore waters ranges from seawater concentrations to nearly zero, and has d34S values ranging from seawater values (+20 per mil) to slightly enriched in 34S (+28 per mil). Pyrite sulfur has 34S values of -4.8 per mil to -37.1 per mil. These general trends are attributed to bacterial reduction of seawater sulfate, but the data do not fit simple models for downward diffusion of sulfate or closed-system reduction of buried sulfate. These complications are due to variations in the d34S of seawater sulfate in the past, uptake of sulfate by thaumasite (Ca3Si(OH)6CO3SO4-12H2O) without isotopic fractionation in the Unit II tuff in Hole 802A, the presence of cherts that act as barriers to diffusion, and possible variations in the magnitude of isotopic fractionation during bacterial sulfate reduction.
	The average sediment from Leg 129 contains around 850 ppm S (85% as sulfate, 15% as sulfide), with a bulk d34S of +12 per mil. The bulk sulfur isotopic composition of deep-sea sediment is highly dependent on the proportion of pyrite-sulfur present, which varies depending on the sedimentary environment and history. The sedimentary sulfur component during subduction thus likely varies from near seawater values (+20 per mil) to possibly strongly negative values (-20 per mil).
Project(s):	Ocean Drilling Program (ODP) (URI: https://www-odp.tamu.edu:443/)
Coverage:	MEDIAN LATITUDE: 17.989280 * MEDIAN LONGITUDE: 154.922440 * SOUTH-BOUND LATITUDE: 12.096300 * WEST-BOUND LONGITUDE: 152.322900 * NORTH-BOUND LATITUDE: 21.923000 * EAST-BOUND LONGITUDE: 156.359800
	DATE/TIME START: 1989-11-26T02:45:00 * DATE/TIME END: 1990-01-16T07:15:00
	MINIMUM DEPTH, sediment/rock: 20.85 m * MAXIMUM DEPTH, sediment/rock: 501.87 m
Event(s):	129-800A * LATITUDE: 21.923000 * LONGITUDE: 152.322900 * DATE/TIME START: 1989-11-26T02:45:00 * DATE/TIME END: 1989-12-05T20:27:00 * ELEVATION: -5697.0 m * PENETRATION: 544.4 m * RECOVERY: 150.73 m * LOCATION: North Pacific Ocean * CAMPAIGN: Leg129 * BASIS: Joides Resolution (URI: https://www-odp.tamu.edu:443/resolutn.html) * METHOD/DEVICE: Drilling/drill rig (DRILL) * COMMENT: 61 core; 544.4 m cored; 0 m drilled; 27.7 % recovery
	129-801A * LATITUDE: 18.642800 * LONGITUDE: 156.359500 * DATE/TIME START: 1989-12-06T17:15:00 * DATE/TIME END: 1989-12-09T17:00:00 * ELEVATION: -5685.0 m * PENETRATION: 194 m * RECOVERY: 31.49 m * LOCATION: North Pacific Ocean * CAMPAIGN: Leg129 * BASIS: Joides Resolution (URI: https://www-odp.tamu.edu:443/resolutn.html) * METHOD/DEVICE: Drilling/drill rig (DRILL) * COMMENT: 20 cores; 186 m cored; 0 m drilled; 16.9 % recovery
	129-801B * LATITUDE: 18.642000 * LONGITUDE: 156.359700 * DATE/TIME START: 1989-12-09T17:00:00 * DATE/TIME END: 1989-12-17T01:15:00 * ELEVATION: -5685.0 m * PENETRATION: 511.2 m * RECOVERY: 59.17 m * LOCATION: North Pacific Ocean * CAMPAIGN: Leg129 * BASIS: Joides Resolution (URI: https://www-odp.tamu.edu:443/resolutn.html) * METHOD/DEVICE: Drilling/drill rig (DRILL) * COMMENT: 44 cores; 317.2 m cored; 0 m drilled; 18.7 % recovery
	129-801C * LATITUDE: 18.642300 * LONGITUDE: 156.359800 * DATE/TIME START: 1990-01-06T11:48:00 * DATE/TIME END: 1990-01-16T07:15:00 * ELEVATION: -5685.0 m * PENETRATION: 594.3 m * RECOVERY: 60.6 m * LOCATION: North Pacific Ocean * CAMPAIGN: Leg129 * BASIS: Joides Resolution (URI: https://www-odp.tamu.edu:443/resolutn.html) * METHOD/DEVICE: Drilling/drill rig (DRILL) * COMMENT: 12 cores; 100.6 m cored; 0 m drilled; 60.2 % recovery
	129-802A * LATITUDE: 12.096300 * LONGITUDE: 153.210300 * DATE/TIME START: 1989-12-25T10:15:00 * DATE/TIME END: 1990-01-04T17:20:00 * ELEVATION: -5980.0 m * PENETRATION: 559.8 m * RECOVERY: 165.01 m * LOCATION: North Pacific Ocean * CAMPAIGN: Leg129 * BASIS: Joides Resolution (URI: https://www-odp.tamu.edu:443/resolutn.html) * METHOD/DEVICE: Drilling/drill rig (DRILL) * COMMENT: 62 cores; 559.8 m cored; 0 m drilled; 29.5 % recovery
Parameter(s):	Event label (Event)
	Sample code/label (Sample label) * PI: Alt, Jeffrey C * METHOD/DEVICE: DSDP/ODP/IODP sample designation (URI: hdl:10013/epic.27914.d001)
	Sample type (Samp type) * PI: Alt, Jeffrey C
	DEPTH, sediment/rock [m] (Depth sed) * GEOCODE * COMMENT: mbsf
	Sulfate [mg/kg] ([SO4]2-) * PI: Alt, Jeffrey C * COMMENT: water soluble
	Sulfate [mg/kg] ([SO4]2-) * PI: Alt, Jeffrey C * COMMENT: acid soluble
	Sulfide [mg/kg] (S2-) * PI: Alt, Jeffrey C * COMMENT: acid solible
	Sulfur of pyrite [mg/kg] (S Py) * PI: Alt, Jeffrey C
	Sulfur, total [mg/kg] (TS) * PI: Alt, Jeffrey C
	Sulfate [mg/kg] ([SO4]2-) * PI: Alt, Jeffrey C * COMMENT: interstitial water
	δ34S, sulfate [‰ CDT] (δ34S [SO4]2-) * PI: Alt, Jeffrey C * COMMENT: water soluble
	δ34S, sulfate [‰ CDT] (δ34S [SO4]2-) * PI: Alt, Jeffrey C * COMMENT: acid soluble
	δ34S, pyrite [‰ CDT] (δ34S Py) * PI: Alt, Jeffrey C
	δ34S [‰ CDT] (δ34S) * PI: Alt, Jeffrey C * COMMENT: interstitial water
	δ34S [‰ CDT] (δ34S) * PI: Alt, Jeffrey C * COMMENT: mineral
License:	Creative Commons Attribution 3.0 Unported (CC-BY-3.0) (URI: https://creativecommons.org/licenses/by/3.0/)
Size:	320 data points
*/
Event	Sample label	Samp type	Depth sed [m] (mbsf)	[SO4]2- [mg/kg] (water soluble)	[SO4]2- [mg/kg] (acid soluble)	S2- [mg/kg] (acid solible)	S Py [mg/kg]	TS [mg/kg]	[SO4]2- [mg/kg] (interstitial water)	δ34S [SO4]2- [‰ CDT] (water soluble)	δ34S [SO4]2- [‰ CDT] (acid soluble)	δ34S Py [‰ CDT]	δ34S [‰ CDT] (interstitial water)	δ34S [‰ CDT] (mineral)
129-800A	129-800A-4R-2,25-30	Interstitial water	22.00						25.8				20.4	
129-800A	129-800A-4R-2,44-49	Pelagic clay	22.14	1450	870		<1	2320		20.4	19.7			
129-800A	129-800A-10R-1,8-10	Radiolarian chert	78.28	220	180		4020	4420		-15.9	-27.9	-37.1		
129-800A	129-800A-26R-2,74-76	Volcanic sandstone	230.84	80	150	<1	40	270			15.2	-14.4		
129-800A	129-800A-26R-2,140-180	Interstitial water	232.00						17.6				25.9	
129-800A	129-800A-27R-1,140-150	Interstitial water	239.00						14.5				26.4	
129-800A	129-800A-33R-6,60-70	Interstitial water	296.00						14.0				25.2	
129-800A	129-800A-37R-2,0-10	Interstitial water	327.00						16.4				24.6	
129-800A	129-800A-37R-2,111-116	Volcanic sandstone	327.71	130	110		10	250			21.5			
129-800A	129-800A-41R-2,0-10	Interstitial water	364.00						11.1				26.3	
129-800A	129-800A-49R-2,135-138	Volcanic sandstone	433.75	120	240		10	370		25.7	20.0			
129-800A	129-800A-49R-2,140-150	Interstitial water	434.00						12.3				25.3	
129-800A	129-800A-54R-2,0-12	Interstitial water	473.00						13.2				23.5	
129-800A	129-800A-55R-2,95-99	Radiolarian claystone	481.55	190	30		<1	220		23.5				
129-801A	129-801A-3R-1,45-49	Pelagic clay	20.85	1560	870		10	2440		20.4	19.8			
129-801A	129-801A-3R-2,145-150	Interstitial water	29.30						29.3				20.5	
129-801A	129-801A-5R-3,145-150	Interstitial water	36.00						37.2				21.0	
129-801A	129-801A-5R-5,97-102	Pelagic clay	46.57	810	350			1160		20.6	19.9			
129-801A	129-801A-18R-1,102-107	Volcanic sandstone	166.02	130	230		200	560		20.7	8.7	-14.9		
129-801A	129-801A-19R-1,65-73	Interstitial water	167.00						19.3				25.1	
129-801B	129-801B-5R-2,0-10	Interstitial water	225.00						16.1		25.7			
129-801B	129-801B-5R-2,35-39	Volcanic sandstone	233.55	150	130		40	320		23.9	23.6	-20.7		
129-801B	129-801B-8R-2,117-120	Volcanic claystone	263.37	300		<1	10			22.7	13.6	-13.9		
129-801B	129-801B-8R-3,115-125	Interstitial water	257.00						16.8				26.2	
129-801B	129-801B-27R-1,56-61	Clayey radiolarite	415.26	200	290		10	500		21.0	16.8			
129-801B	129-801B-33R-1,143-150	Interstitial water	436.00						17.5				22.6	
129-801B	129-801B-35R-2,0-10	Interstitial water	446.00						21.0				22.8	
129-801C	129-801C-9R-1	Pyrite												-41.7
129-801C	129-801C-9R-2	Pyrite												-18.1
129-802A	129-802A-4R-1,140-150	Interstitial water	26.00						26.8				20.6	
129-802A	129-802A-4R-2,98-101	Volcanic siltstone	26.78	530	50		<1	580		20.3				
129-802A	129-802A-5R-1,64-66	Volcanic tuff	34.34	340	300	<1	50	690		12.7	16.3	-4.8		
129-802A	129-802A-6R-2,0-10	Interstitial water	44.00						36.5				20.8	
129-802A	129-802A-10R-2,140-150	Interstitial water	83.00						0.4					
129-802A	129-802A-11R-1,143-147	Volcanic tuff	91.03	50	70	<1	20	140			14.1	-10.2		
129-802A	129-802A-13R-1,53-58	Interstitial water	109.00						3.7				20.5	
129-802A	129-802A-13R-2,71-73	Pelagic clay	109.59	30	20		10	60		13.3				
129-802A	129-802A-16R-1,30-33	Thaumasite	131.40											20.4
129-802A	129-802A-19R-2,107-117	Interstitial water	162.00						9.9				21.4	
129-802A	129-802A-20R-1,0-2	Thaumasite												19.5
129-802A	129-802A-21R-1,103-110	Interstitial water	179.00						11.9				21.1	
129-802A	129-802A-21R-1,93-95	Clayey siltstone	178.53	230			10	240		22.0				
129-802A	129-802A-26R-1,0-10	Interstitial water	225.00						12.2				22.1	
129-802A	129-802A-26R-2,63-66	Clayey chalk	227.53	300	150		<1	450		21.6	20.9			
129-802A	129-802A-29R-2,144-149	Claystone	257.44	550	330			880		22.4	22.1			
129-802A	129-802A-29R-3,29-34	Interstitial water	258.00						12.0				22.2	
129-802A	129-802A-32R-2,140-150	Interstitial water	286.00						12.5					
129-802A	129-802A-32R-2,26-30	Chalk	285.26	150	110			260		23.3	20.1			
129-802A	129-802A-40R-2,140-150	Interstitial water	361.00						15.0				25.4	
129-802A	129-802A-40R-3,81-86	Volcanic claystonesiltstone	361.91	140	100	<1	230	470		22.2	13.9	-31.3		
129-802A	129-802A-43R-1,140-150	Interstitial water	384.00						15.1					
129-802A	129-802A-47R-2,140-150	Interstitial water	422.00						13.2				25.5	
129-802A	129-802A-49R-3,5-9	Silty claystone	441.15	240	220		80	540		23.2	15.3	-31.2		
129-802A	129-802A-50R-2,140-150	Interstitial water	450.00						13.6					
129-802A	129-802A-56R-2,140-150	Interstitial water	500.00						15.7				26.2	
129-802A	129-802A-56R-4,27-31	Claystone	501.87	140	100		1270	1510		27.6	5.6	-30.9	28.6	
129-802A	129-802A-59R-1	Pyrite												-40.3
129-802A	129-802A-59R-3	Pyrite												-36.8
129-802A	129-802A-62R-1	Pyrite												-24.5
