Swart, Peter K; Eberli, Gregor P (2005): (Table 2) Mean carbon-isotopic composition and standard deviations of deposition sequences of the Bahama Bank [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.763536, In supplement to: Swart, PK; Eberli, GP (2005): The nature of the d13C of periplatform sediments: Implications for stratigraphy and the global carbon cycle. Sedimentary Geology, 175(1-4), 115-129, https://doi.org/10.1016/j.sedgeo.2004.12.029
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Eberli, Gregor P; Anselmetti, Flavio S; Kroon, Dick; Sato, Tokiyuki; Wright, James D (2002): The chronostratigraphic significance of seismic reflections along the Bahamas Transect. Marine Geology, 185(1-2), 1-17, https://doi.org/10.1016/S0025-3227(01)00287-0
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 24.544288 * Median Longitude: -79.258245 * South-bound Latitude: 24.399850 * West-bound Longitude: -79.459200 * North-bound Latitude: 24.641200 * East-bound Longitude: -79.107000
Date/Time Start: 1996-02-28T00:00:00 * Date/Time End: 1996-04-08T00:00:00
Minimum Elevation: -657.8 m * Maximum Elevation: -10.0 m
Event(s):
166-1003 * Latitude: 24.545967 * Longitude: -79.260750 * Date/Time: 1996-02-28T00:00:00 * Elevation: -485.6 m * Penetration: 3140 m * Recovery: 694.6 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 172 cores; 1633.1 m cored; 1052.7 m drilled; 42.5% recovery
166-1004 * Latitude: 24.554700 * Longitude: -79.249200 * Date/Time Start: 1996-03-11T00:00:00 * Date/Time End: 1996-03-12T00:00:00 * Elevation: -418.9 m * Penetration: 200 m * Recovery: 117.5 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 23 cores; 200 m cored; 0 m drilled; 58.7% recovery
166-1005 * Latitude: 24.562767 * Longitude: -79.235700 * Date/Time Start: 1996-03-12T00:00:00 * Date/Time End: 1996-03-20T00:00:00 * Elevation: -351.3 m * Penetration: 1224.1 m * Recovery: 306.1 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 96 cores; 837.5 m cored; 0 m drilled; 36.6% recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Layer description | Layer | Swart, Peter K | of Eberli et al. (2002) | ||
| 3 | AGE | Age | ka BP | Geocode | ||
| 4 | δ13C, carbonate | δ13C carb | ‰ PDB | Swart, Peter K | Mass spectrometer Finnigan MAT 251 | |
| 5 | δ13C, standard deviation | δ13C std dev | ± | Swart, Peter K | Mass spectrometer Finnigan MAT 251 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
192 data points
Data
| 1 Event | 2 Layer | 3 Age [ka BP] | 4 δ13C carb [‰ PDB] | 5 δ13C std dev [±] |
|---|---|---|---|---|
| UNDA | B | 600 | -2.32 | 0.58 |
| UNDA | C | 1700 | -2.42 | 1.72 |
| UNDA | D | 3100 | 1.94 | 0.83 |
| UNDA | E | 3600 | 2.71 | 0.34 |
| UNDA | F | 5400 | 1.90 | 0.32 |
| UNDA | G | 8700 | 2.24 | 0.35 |
| UNDA | H | 9400 | 2.65 | 0.23 |
| CLINO | B | 600 | 0.24 | 2.48 |
| CLINO | C | 1700 | -0.07 | 1.07 |
| CLINO | D | 3100 | 3.43 | 1.41 |
| CLINO | E | 3600 | 3.34 | 0.41 |
| CLINO | F | 5400 | 3.16 | 0.41 |
| CLINO | H | 9400 | 2.56 | 0.18 |
| 166-1005 | A | 100 | 4.51 | 0.60 |
| 166-1005 | B | 600 | 4.12 | 0.66 |
| 166-1005 | C | 1700 | 3.76 | 0.55 |
| 166-1005 | D | 3100 | 2.55 | 0.79 |
| 166-1005 | F | 5400 | 2.11 | 0.54 |
| 166-1005 | G | 8700 | 2.45 | 0.46 |
| 166-1005 | H | 9400 | 2.63 | 0.19 |
| 166-1005 | I | 10700 | 1.91 | 0.57 |
| 166-1004 | A | 100 | 4.76 | 0.19 |
| 166-1004 | B | 600 | 4.12 | 0.64 |
| 166-1004 | C | 1700 | 3.92 | 0.61 |
| 166-1004 | D | 3100 | 2.39 | 0.38 |
| 166-1003 | A | 100 | 4.70 | 0.25 |
| 166-1003 | B | 600 | 4.22 | 0.45 |
| 166-1003 | C | 1700 | 3.80 | 0.71 |
| 166-1003 | D | 3100 | 3.25 | 0.50 |
| 166-1003 | E | 3600 | 2.06 | 0.37 |
| 166-1003 | F | 5400 | 2.03 | 0.57 |
| 166-1003 | G | 8700 | 2.95 | 0.10 |
| 166-1003 | H | 9400 | 2.91 | 0.28 |
| 166-1003 | I | 10700 | 2.80 | 0.18 |
| 166-1003 | K | 12200 | 2.80 | 0.34 |
| 166-1003 | M | 15100 | 2.95 | 0.51 |
| 166-1003 | N | 15900 | 2.97 | 0.39 |
| 166-1003 | O | 18300 | 2.03 | 0.56 |
| 166-1003 | P | 19400 | 1.55 | 0.35 |
| 166-1003 | P2 | 23200 | 1.88 | 0.34 |
| 166-1003 | Q | 23700 | 1.56 | 0.26 |
| 166-1007 | A | 100 | 3.22 | 0.36 |
| 166-1007 | B | 600 | 2.93 | 0.44 |
| 166-1007 | C | 1700 | 3.33 | 1.21 |
| 166-1007 | D | 3100 | 3.99 | 1.41 |
| 166-1007 | F | 5400 | 2.07 | 0.39 |
| 166-1007 | G | 8700 | 2.93 | 1.33 |
| 166-1007 | H | 9400 | 1.89 | 0.00 |
| 166-1007 | I | 10700 | 1.84 | 0.26 |
| 166-1007 | K | 12200 | 2.12 | 0.41 |
| 166-1007 | L | 12700 | 2.65 | 0.26 |
| 166-1007 | M | 15100 | 3.08 | 0.34 |
| 166-1007 | N | 15900 | 2.47 | 0.39 |
| 166-1007 | O | 18300 | 1.90 | 0.41 |
| 166-1007 | P | 19400 | 1.71 | 0.34 |
| 166-1007 | P2 | 23200 | 1.59 | 0.21 |
| 166-1006 | B | 600 | 3.24 | 0.91 |
| 166-1006 | C | 1700 | 2.79 | 1.02 |
| 166-1006 | D | 3100 | 2.45 | 0.58 |
| 166-1006 | E | 3600 | 2.02 | 0.22 |
| 166-1006 | F | 5400 | 1.30 | 0.47 |
| 166-1006 | G | 8700 | 1.46 | 0.32 |
| 166-1006 | H | 9400 | 1.78 | 0.12 |
| 166-1006 | I | 10700 | 1.37 | 0.25 |