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Borowski, Walter S; Paull, Charles K (2000): (Table 1) Stable nitrogen isotopes of ammonium in interstitial waters from ODP Site 164-997 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.804017, Supplement to: Borowski, WS; Paull, CK (2000): Data Report: Nitrogen isotopic composition of pore-water ammonium, Blake Ridge, Site 997. In: Paull, CK; Matsumoto, R; Wallace, PJ; Dillon, WP (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 164, 1-2, https://doi.org/10.2973/odp.proc.sr.164.213.2000

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Abstract:
Ammonium (NH4+) concentration profiles in piston-core sediments of the Carolina Rise and Blake Ridge generally have linear concentration profiles within the sulfate reduction zone (Borowski, 1998). Deep Sea Drilling Project (DSDP) Site 533, located on the Blake Ridge, also displayed a linear ammonium concentration profile through the sulfate reduction zone and the profile linearity continues into the upper methanogenic zone to a depth of ~200 meters below seafloor (mbsf), where the first methane gas hydrates probably occur (Jenden and Gieskes, 1983, doi:10.2973/dsdp.proc.76.114.1983; Kvenvolden and Barnard, 1983, doi:10.2973/dsdp.proc.76.106.1983). Sediments from the Ocean Drilling Program (ODP) Leg 164 deep holes (Sites 994, 995, and 997) also exhibit linear ammonium profiles above the top of the gas hydrate zone (~200 mbsf) (Paull, Matsumoto, Wallace, et al., 1996, doi:10.2973/odp.proc.ir.164.1996).
We hypothesized that a possible cause of linear ammonium profiles was diffusion of ammonium from a concentrated ammonium source at depth. We further reasoned that if this ammonium were produced by microbial fermentation reactions at depth, that a comparison of the nitrogen isotopic composition of sedimentary organic nitrogen and the nitrogen with pore-water ammonium would test this hypothesis. Convergence with depth of d15N values of the nitrogen source (sedimentary organic matter) and the nitrogen product (dissolved NH4+) would strongly suggest that ammonium was produced within a particular depth zone by microbial fermentation reactions. Here, we report d15N values of pore-water ammonium from selected interstitial water (IW) samples from Site 997, sampled during ODP Leg 164.
Project(s):
Coverage:
Median Latitude: 31.843200 * Median Longitude: -75.468550 * South-bound Latitude: 31.843100 * West-bound Longitude: -75.468600 * North-bound Latitude: 31.843300 * East-bound Longitude: -75.468500
Date/Time Start: 1995-12-06T12:35:00 * Date/Time End: 1995-12-17T07:25:00
Minimum DEPTH, sediment/rock: 16.80 m * Maximum DEPTH, sediment/rock: 687.65 m
Event(s):
164-997A * Latitude: 31.843100 * Longitude: -75.468600 * Date/Time Start: 1995-12-06T12:35:00 * Date/Time End: 1995-12-10T00:10:00 * Elevation: -2770.1 m * Penetration: 434.3 m * Recovery: 342.66 m * Location: Nicaraguan Rise, North Atlantic Ocean * Campaign: Leg164 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 55 cores; 434.3 m cored; 0 m drilled; 78.9 % recovery
164-997B * Latitude: 31.843300 * Longitude: -75.468500 * Date/Time Start: 1995-12-10T00:30:00 * Date/Time End: 1995-12-17T07:25:00 * Elevation: -2770.1 m * Penetration: 750 m * Recovery: 242.75 m * Location: Nicaraguan Rise, North Atlantic Ocean * Campaign: Leg164 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 47 cores; 364.6 m cored; 0 m drilled; 66.6 % recovery
Comment:
Sediment depth is given in mbsf. For ammonium concentrations (and other water chemical data) of ODP Site 164-997 see Paull, Matsumoto, Wallace, et al. (1996, doi:10.2973/odp.proc.ir.164.1996) or datasets: doi:10.1594/PANGAEA.256060 and doi:10.1594/PANGAEA.256061.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Sample code/labelSample labelBorowski, Walter SDSDP/ODP/IODP sample designation
3DEPTH, sediment/rockDepth sedmGeocode
4δ15N, ammoniumδ15N [NH4]+‰ airBorowski, Walter SMass spectrometer VG SIRA
Size:
18 data points

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