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Sackett, William M (1986): Concentration and stable carbon isotopic composition of organic carbon of DSDP Hole 28-266 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.757317, Supplement to: Sackett, WM (1986): d13C signatures of organic carbon in southern high latitude deep sea sediments; paleotemperature implications. Organic Geochemistry, 9(2), 63-68, https://doi.org/10.1016/0146-6380(86)90087-2

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Abstract:
The 7% carbon-13 depletion in cold water phytoplankton provides a striking signal that is traceable in deep-sea cores taken in high latitude regions of the Southern hemisphere. This signal may be weakened by noise due to (1) terrestrially derived debris in areas close to the continents; (2) changing current patterns resulting in varying settling trajectories; (3) erosion and redeposition and (4) maturation-diagenetic effects. Data for two cores taken southwest of Australia are evaluated with respect to these interferences.
Project(s):
Coverage:
Latitude: -56.402200 * Longitude: 110.111700
Date/Time Start: 1973-01-02T00:00:00 * Date/Time End: 1973-01-02T00:00:00
Minimum DEPTH, sediment/rock: 1.0 m * Maximum DEPTH, sediment/rock: 375.0 m
Event(s):
28-266 * Latitude: -56.402200 * Longitude: 110.111700 * Date/Time: 1973-01-02T00:00:00 * Elevation: -4167.0 m * Penetration: 384 m * Recovery: 145 m * Location: Antarctic Ocean/RIDGE * Campaign: Leg28 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 219.5 m cored; 0 m drilled; 66.1 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample code/labelSample labelSackett, William MDSDP/ODP/IODP sample designation
DEPTH, sediment/rockDepth sedmGeocode
EpochEpochSackett, William M
Carbon, organic, totalTOC%Sackett, William M
δ13C, organic carbonδ13C Corg‰ PDBSackett, William M
Calcium carbonateCaCO3%Sackett, William M
Size:
162 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Sample label

Depth sed [m]

Epoch

TOC [%]

δ13C Corg [‰ PDB]

CaCO3 [%]
28-266-1-1,102-1041.0Late Pleistocene0.18-18.4
28-266-1-2,100-1022.5Late Pleistocene0.15-19.4
28-266-1-2,100-1022.5Late Pleistocene0.13-19.6
28-266-1-3,100-1024.0Late Pleistocene0.16-16.5
28-266-1-3,100-1024.0Late Pleistocene0.16-16.6
28-266-2-3,98-10029.0Early Pleistocene0.15-19.8
28-266-2-3,98-10029.0Early Pleistocene0.19-19.7
28-266-4-1,130-13264.3Early Pleistocene0.21-19.50.9
28-266-4-3,97-9967.0Early Pleistocene0.15-20.5
28-266-5-1,98-10083.0Pliocene0.19-22.7
28-266-5-1,98-10083.0Pliocene0.19-22.6
28-266-5-3,100-10286.0Pliocene0.10-25.1
28-266-5-3,100-10286.0Pliocene0.12-24.7
28-266-5-5,98-10089.0Pliocene0.15-22.8
28-266-5-5,98-10089.0Pliocene0.15-23.2
28-266-6-1,100-102102.0Pliocene0.13-22.4
28-266-6-3,100-102105.0Pliocene0.11-21.9
28-266-6-3,100-102105.0Pliocene0.10-22.0
28-266-6-5,100-102108.0Pliocene0.14-21.8
28-266-6-5,100-102108.0Pliocene0.16-21.9
28-266-7-1,131-133121.3Pliocene0.14-21.9
28-266-7-3,100-102124.0Pliocene0.15-23.1
28-266-7-3,100-102124.0Pliocene0.13-22.7
28-266-7-5,100-102127.0Pliocene0.18-22.9
28-266-8-1,100-102130.5Pliocene0.16-22.9
28-266-8-1,100-102130.5Pliocene0.15-23.2
28-266-8-3,100-102133.5Pliocene0.17-22.7
28-266-8-3,100-102133.5Pliocene0.16-22.6
28-266-8-5,100-102136.5Pliocene0.18-22.1
28-266-8-5,100-102136.5Pliocene0.17-22.2
28-266-9-1,104-106140.0Pliocene0.16-23.4
28-266-9-1,104-106140.0Pliocene0.16-23.3
28-266-9-3,103-105143.0Pliocene0.12-23.9
28-266-9-3,103-105143.0Pliocene0.12-24.2
28-266-11-5,104-106165.0Middle Miocene0.07-28.6
28-266-11-5,104-106165.0Middle Miocene0.08-28.7
28-266-12-1,103-105178.0Lower Miocene0.11-25.7
28-266-12-1,103-105178.0Lower Miocene0.11-25.4
28-266-14-1,105-107216.0Lower Miocene0.10-26.21.2
28-266-24-1,100-102375.0Basement Basalt0.02-23.7