Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Kawahata, Hodaka; Ishizuka, Toshio (2000): Amino acid concentrations in interstitial waters from ODP Sites 113-689 and 113-690 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.726857, Supplement to: Kawahata, H; Ishizuka, T (2000): Amino acids in interstitial waters from ODP Sites 689 and 690 on the Maud Rise, Antarctic Ocean. Geochemical Journal, 34(4), 247-261, https://doi.org/10.2343/geochemj.34.247

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Biogenic calcareous and siliceous sediments were drilled at ODP Sites 689 and 690 on the Maud Rise, Antarctic Ocean. We analyzed dissolved combined amino acids (DCAA) and dissolved free amino acids (DFAA) in interstitial waters in order to characterize the amino acids in dissolved organic matter. The DFAA was predominant over the DCAA in interstitial waters at Sites 689 and 690, which contradicted the previous results from interstitial water and seawater studies. The DCAA in the interstitial waters probably originated from calcareous biogenic debris with less amounts of siliceous debris. Although glutamic acid constituted 41% of the total concentration of DCAA, it accounted for only 1% of the total concentration of DFAA due to the adsorption and/or reaction with biogenic carbonate. Ornithine, a nonprotein amino acid, is a decomposed product of arginine and made up 17 mol% of the total DFAA and. The total hydrolyzable amino acids (=DCAA + DFAA) accounted for 5 to 28% of the dissolved organic carbon (DOC) concentration, which implied that high molecular weight organic matter was a major contributor for the DOM (dissolved organic matter) in interstitial waters. Fairly positive correlation between the dissolved manganese and the total DCAA values suggested that the redox condition plays a significant role in controlling the total DCAA content. A small decrease in the sulfate concentration in the interstitial waters from both sites suggested fairly low microbial activity by sulfate-reducing bacteria.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -64.946000 * Median Longitude: 1.836533 * South-bound Latitude: -65.161000 * West-bound Longitude: 1.204800 * North-bound Latitude: -64.517000 * East-bound Longitude: 3.099900
Date/Time Start: 1987-01-16T08:00:00 * Date/Time End: 1987-01-23T20:30:00
Event(s):
113-689B * Latitude: -64.517000 * Longitude: 3.099900 * Date/Time Start: 1987-01-16T08:00:00 * Date/Time End: 1987-01-18T06:45:00 * Elevation: -2091.0 m * Penetration: 297.3 m * Recovery: 229.45 m * Location: South Atlantic Ocean * Campaign: Leg113 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 33 cores; 297.3 m cored; 0 m drilled; 77.2 % recovery
113-690B * Latitude: -65.161000 * Longitude: 1.204900 * Date/Time Start: 1987-01-20T03:15:00 * Date/Time End: 1987-01-21T07:00:00 * Elevation: -2925.0 m * Penetration: 213.4 m * Recovery: 214.75 m * Location: South Atlantic Ocean * Campaign: Leg113 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 25 cores; 213.4 m cored; 0 m drilled; 100.6 % recovery
113-690C * Latitude: -65.160000 * Longitude: 1.204800 * Date/Time Start: 1987-01-21T07:00:00 * Date/Time End: 1987-01-23T20:30:00 * Elevation: -2925.0 m * Penetration: 321.2 m * Recovery: 177.19 m * Location: South Atlantic Ocean * Campaign: Leg113 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 200.6 m cored; 0 m drilled; 88.3 % recovery
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
6 datasets

Download Data

Download ZIP file containing all datasets as tab-delimited text — use the following character encoding:

Datasets listed in this publication series

  1. Kawahata, H; Ishizuka, T (2000): (Table 1) Dissolved combined amino acid concentrations in interstitial waters from ODP Hole 113-689B sediments. https://doi.org/10.1594/PANGAEA.726531
  2. Kawahata, H; Ishizuka, T (2000): (Table 1) Dissolved combined amino acid concentrations in interstitial waters from ODP Hole 113-690B sediments. https://doi.org/10.1594/PANGAEA.726532
  3. Kawahata, H; Ishizuka, T (2000): (Table 1) Dissolved combined amino acid concentrations in interstitial waters from ODP Hole 113-690C sediments. https://doi.org/10.1594/PANGAEA.726533
  4. Kawahata, H; Ishizuka, T (2000): (Table 2) Dissolved free amino acid concentrations in interstitial waters from ODP Hole 113-689B sediments. https://doi.org/10.1594/PANGAEA.726534
  5. Kawahata, H; Ishizuka, T (2000): (Table 2) Dissolved free amino acid concentrations in interstitial waters from ODP Hole 113-690B sediments. https://doi.org/10.1594/PANGAEA.726535
  6. Kawahata, H; Ishizuka, T (2000): (Table 2) Dissolved free amino acid concentrations in interstitial waters from ODP Hole 113-690C sediments. https://doi.org/10.1594/PANGAEA.726536