Lee, Cindy (2003): Amino acid compositions in sediment core TT013_2N_A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.124959
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Lee, Cindy (2003): Amino acid compositions in sediment cores. United States JGOFS Process Study Data 1989-1998; CD-ROM volume 1, version 2, Woods Hole Oceanographic Institution, USA: U.S. JGOFS Data Management Office
Lee, Cindy; Wakeham, Stuart G; Hedges, John I (2000): Composition and flux of particulate amino acids and chloropigments in equatorial Pacific seawater and sediments. Deep Sea Research Part I: Oceanographic Research Papers, 47(8), 1535-1568, https://doi.org/10.1016/S0967-0637(99)00116-8
Further details:
Lee, Cindy: Chloropigments and amino acid concentrations in sediment cores and traps. US JGOFS (Joint Global Ocean Flux Study) Data System, Lee_methods.htm
Project(s):
Joint Global Ocean Flux Study (JGOFS)
Coverage:
Latitude: 2.000000 * Longitude: -140.000000
Minimum DEPTH, sediment/rock: -0.0100 m * Maximum DEPTH, sediment/rock: 0.0075 m
Event(s):
TT013_2N_A * Latitude: 2.000000 * Longitude: -140.000000 * Location: Equatorial Pacific * Campaign: TT013 * Basis: Thomas G. Thompson * Method/Device: Gravity corer (GC)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Asp [%] | 5 Glu [%] | 6 Ser [%] | 7 His [%] | 8 Gly [%] | 9 Thr [%] | 10 Arg [%] | 11 Ala [%] | 12 Tyr [%] | 13 Met [%] | 14 Val [%] | 15 Phe [%] | 16 Ile [%] | 17 Leu [%] | 18 Lys [%] | 19 Amino acids/sed [µg/g] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
-0.0100 | 16.9 | 8.0 | 2.3 | 31.5 | 8.3 | 3.3 | 14.4 | 1.9 | 0.2 | 4.6 | 2.1 | 2.5 | 3.4 | 0.6 | 3830 | |||
0.0025 | 0.000 | 0.005 | 18.9 | 9.4 | 3.4 | 0.0 | 22.1 | 10.1 | 5.1 | 14.1 | 0.2 | 0.0 | 6.4 | 1.4 | 3.7 | 4.7 | 0.6 | 930 |
0.0075 | 0.005 | 0.010 | 21.7 | 7.9 | 1.0 | 21.9 | 8.7 | 5.1 | 15.4 | 0.4 | 0.0 | 6.7 | 0.5 | 4.2 | 5.2 | 1.3 | 510 |