Lee, Cindy (2003): Amino acid compositions in sediment core TT013_2S_A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.124960
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_2S_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 | 21.8 | 8.4 | 7.2 | 24.0 | 7.9 | 4.3 | 11.5 | 0.9 | 0.2 | 4.4 | 2.0 | 2.7 | 3.7 | 0.9 | 1250 | |||
0.0025 | 0.000 | 0.005 | 22.4 | 9.1 | 4.3 | 0.3 | 20.8 | 8.0 | 4.8 | 13.6 | 0.6 | 0.0 | 5.9 | 2.4 | 3.3 | 4.6 | 0.0 | 490 |
0.0075 | 0.005 | 0.010 | 21.6 | 7.2 | 1.3 | 20.3 | 8.4 | 5.7 | 15.4 | 0.5 | 0.0 | 6.9 | 2.7 | 3.8 | 5.2 | 1.0 | 380 |