Channell, James E T (2020): Age model of IODP Site 303-U1304 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.919735, In: Channell, JET (2020): Age model, RPI and VGP from IODP Sites 303-U1304, 303-U1305 and 303-U1306 at the Matuyama-Brunhes boundary [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.919883
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Channell, James E T (2017): Complexity in Matuyama–Brunhes polarity transitions from North Atlantic IODP/ODP deep-sea sites. Earth and Planetary Science Letters, 467, 43-56, https://doi.org/10.1016/j.epsl.2017.03.019
Further details:
Xuan, Chuang; Channell, James E T; Hodell, David A (2016): Quaternary magnetic and oxygen isotope stratigraphy in diatom-rich sediments of the southern Gardar Drift (IODP Site U1304, North Atlantic). Quaternary Science Reviews, 142, 74-89, https://doi.org/10.1016/j.quascirev.2016.04.010
Project(s):
Coverage:
Latitude: 53.000000 * Longitude: -33.529000
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 224.36 m
Event(s):
303-U1304 * Latitude: 53.000000 * Longitude: -33.529000 * Elevation: -3064.0 m * Penetration: 794.9 m * Recovery: 761 m * Location: North Atlantic * Campaign: Exp303 (North Atlantic Climate 1) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 81 cores; 741.9 m cores; 102.6 % recovered; 53 m drilled
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Channell, James E T | Geocode – mcd | |
2 | Age model | Age model | ka | Channell, James E T | Age model, composite | see Xuan et al. (2016) |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
40 data points
Data
1 Depth sed [m] | 2 Age model [ka] |
---|---|
0.00 | 0.00 |
0.80 | 3.37 |
1.83 | 8.32 |
4.05 | 32.48 |
5.88 | 42.38 |
8.60 | 62.18 |
12.70 | 92.67 |
17.63 | 118.71 |
26.39 | 189.03 |
27.72 | 196.63 |
33.34 | 238.02 |
39.60 | 261.39 |
42.17 | 285.45 |
50.81 | 328.71 |
53.23 | 336.14 |
62.44 | 388.12 |
78.09 | 477.23 |
133.95 | 731.29 |
136.72 | 743.27 |
138.57 | 770.30 |
140.60 | 791.23 |
144.19 | 829.70 |
146.90 | 845.15 |
149.20 | 857.70 |
151.87 | 878.48 |
158.34 | 954.93 |
164.58 | 986.30 |
167.37 | 1010.50 |
176.10 | 1070.00 |
178.46 | 1109.00 |
190.11 | 1207.30 |
195.14 | 1255.00 |
196.00 | 1266.60 |
206.26 | 1337.40 |
208.61 | 1354.80 |
213.11 | 1421.30 |
220.91 | 1473.60 |
223.59 | 1497.80 |
223.80 | 1502.30 |
224.36 | 1504.90 |