Hodell, David A; Channell, James E T (2016): Age model of IODP Site 303-U1308 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.871932, In supplement to: Hodell, DA; Channell, JET (2016): Mode transitions in Northern Hemisphere glaciation: co-evolution of millennial and orbital variability in Quaternary climate. Climate of the Past, 12(9), 1805-1828, https://doi.org/10.5194/cp-12-1805-2016
Always quote citation above when using data! You can download the citation in several formats below.
Other version:
Hodell, David A; Channell, James E T (2016): North Atlantic 3.2MYr Stable Isotope and Physical Properties Data. NOAA National Centers for Environmental Information, https://doi.org/10.25921/HW8A-4C28
Project(s):
Coverage:
Latitude: 49.877760 * Longitude: -24.238110
Date/Time Start: 2004-10-30T00:00:00 * Date/Time End: 2004-10-30T00:00:00
Minimum DEPTH, sediment/rock: 0.0000 m * Maximum DEPTH, sediment/rock: 255.0550 m
Event(s):
303-U1308 * Latitude: 49.877760 * Longitude: -24.238110 * Date/Time: 2004-10-30T00:00:00 * Elevation: -3871.0 m * Penetration: 1253.5 m * Recovery: 1246 m * Location: North Atlantic * Campaign: Exp303 (North Atlantic Climate 1) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 134 cores; 1246.0 m cored; 7.5 m drilled; 95.4 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Hodell, David A | Geocode – rmcd | |
2 | Age model | Age model | ka | Hodell, David A | cal ka | |
3 | Method comment | Method comm | Hodell, David A | |||
4 | Comment | Comment | Hodell, David A | |||
5 | Reference/source | Reference | Hodell, David A |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
706 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 Method comm | 4 Comment | 5 Reference |
---|---|---|---|---|
0.0000 | 0.00 | assume modern core top | ||
0.9530 | 17.79 | radiocarbon | Marine 09 | Obrochta et al., 2012, 2014 |
0.9810 | 19.17 | radiocarbon | Marine 10 | Obrochta et al., 2012, 2014 |
1.0070 | 19.56 | radiocarbon | Marine 11 | Obrochta et al., 2012, 2014 |
1.0760 | 20.18 | radiocarbon | Marine 12 | Obrochta et al., 2012, 2014 |
1.1670 | 22.66 | radiocarbon | Marine 13 | Obrochta et al., 2012, 2014 |
1.2200 | 23.90 | radiocarbon | Marine 14 | Obrochta et al., 2012, 2014 |
1.2380 | 24.58 | radiocarbon | Marine 15 | Obrochta et al., 2012, 2014 |
1.2560 | 25.28 | radiocarbon | Marine 16 | Obrochta et al., 2012, 2014 |
1.3050 | 25.59 | radiocarbon | Marine 17 | Obrochta et al., 2012, 2014 |
1.3350 | 27.05 | radiocarbon | Marine 18 | Obrochta et al., 2012, 2014 |
1.5550 | 30.10 | radiocarbon | Marine 19 | Obrochta et al., 2012, 2014 |
1.6350 | 30.89 | radiocarbon | Marine 20 | Obrochta et al., 2012, 2014 |
1.7000 | 31.98 | radiocarbon | Marine 21 | Obrochta et al., 2012, 2014 |
1.8860 | 33.20 | radiocarbon | Marine 22 | Obrochta et al., 2012, 2014 |
1.9880 | 33.92 | radiocarbon | Marine 23 | Obrochta et al., 2012, 2014 |
2.2510 | 35.45 | %Nps | GICC05 | Obrochta et al., 2012, 2014 |
2.5120 | 38.15 | %Nps | GICC05 | Obrochta et al., 2012, 2014 |
2.9170 | 41.45 | %Nps | GICC05 | Obrochta et al., 2012, 2014 |
3.0600 | 43.30 | %Nps | GICC05 | Obrochta et al., 2012, 2014 |
3.3240 | 46.65 | %Nps | GICC05 | Obrochta et al., 2012, 2014 |
4.0990 | 54.40 | %Nps | GICC05 | Obrochta et al., 2012, 2014 |
4.3080 | 57.80 | %Nps | GICC05 | Obrochta et al., 2012, 2014 |
4.3600 | 59.05 | %Nps | GICC05 | Obrochta et al., 2012, 2014 |
4.5260 | 63.95 | %Nps | GICC05modelext | Obrochta et al., 2012, 2014 |
4.7340 | 69.60 | %Nps | GICC05modelext | Obrochta et al., 2012, 2014 |
4.8850 | 72.25 | %Nps | GICC05modelext | Obrochta et al., 2012, 2014 |
5.1630 | 76.50 | %Nps | GICC05modelext | Obrochta et al., 2012, 2014 |
5.9475 | 87.54 | L* | GICC05modelext | Obrochta et al., in prep |
6.0975 | 90.20 | L* | GICC05modelext | Obrochta et al., in prep |
7.0050 | 105.32 | L* | GICC05modelext | Obrochta et al., in prep |
7.3475 | 110.42 | L* | GICC05modelext | Obrochta et al., in prep |
8.7550 | 127.00 | O18 | LR04 | Hodell et al., 2008 |
9.1750 | 136.00 | O18 | LR04 | Hodell et al., 2008 |
11.5350 | 191.00 | O18 | LR04 | Hodell et al., 2008 |
12.4150 | 201.00 | O18 | LR04 | Hodell et al., 2008 |
13.6500 | 220.00 | O18 | LR04 | Hodell et al., 2008 |
15.3300 | 243.00 | O18 | LR04 | Hodell et al., 2008 |
18.0700 | 281.00 | O18 | LR04 | Hodell et al., 2008 |
18.7500 | 292.00 | O18 | LR04 | Hodell et al., 2008 |
21.4500 | 329.40 | O18 | LR04 | Hodell and Channel, 2016 |
21.8600 | 341.80 | O18 | LR04 | Hodell and Channel, 2016 |
24.7400 | 392.00 | O18 | LR04 | Hodell et al., 2008 |
27.4200 | 431.00 | O18 | LR04 | Hodell et al., 2008 |
29.0800 | 475.00 | O18 | LR04 | Hodell et al., 2008 |
32.7000 | 513.00 | O18 | LR04 | Hodell et al., 2008 |
34.9400 | 534.00 | O18 | LR04 | Hodell et al., 2008 |
37.5800 | 580.00 | O18 | LR04 | Hodell et al., 2008 |
38.6000 | 596.00 | O18 | LR04 | Hodell et al., 2008 |
39.9000 | 622.00 | O18 | LR04 | Hodell et al., 2008 |
43.7400 | 690.00 | O18 | LR04 | Hodell et al., 2008 |
47.2600 | 726.00 | O18 | LR04 | Hodell et al., 2008 |
48.7400 | 746.00 | O18 | LR04 | Hodell et al., 2008 |
51.1600 | 788.00 | O18 | LR04 | Hodell et al., 2008 |
52.6000 | 814.00 | O18 | LR04 | Hodell et al., 2008 |
56.4300 | 866.00 | O18 | LR04 | Hodell et al., 2008 |
58.5300 | 902.00 | O18 | LR04 | Hodell et al., 2008 |
60.2100 | 922.00 | O18 | LR04 | Hodell et al., 2008 |
64.3900 | 964.00 | O18 | LR04 | Hodell et al., 2008 |
65.7300 | 978.00 | O18 | LR04 | Hodell et al., 2008 |
65.9900 | 984.00 | O18 | LR04 | Hodell et al., 2008 |
67.7500 | 998.00 | O18 | LR04 | Hodell et al., 2008 |
68.0700 | 1004.00 | O18 | LR04 | Hodell et al., 2008 |
70.4300 | 1032.00 | O18 | LR04 | Hodell et al., 2008 |
72.0900 | 1058.00 | O18 | LR04 | Hodell et al., 2008 |
72.7900 | 1070.00 | O18 | LR04 | Hodell et al., 2008 |
77.2700 | 1098.00 | O18 | LR04 | Hodell et al., 2008 |
78.2700 | 1108.00 | O18 | LR04 | Hodell et al., 2008 |
80.0100 | 1126.00 | O18 | LR04 | Hodell et al., 2008 |
80.7700 | 1132.00 | O18 | LR04 | Hodell et al., 2008 |
86.0600 | 1200.00 | O18 | LR04 | Hodell et al., 2008 |
87.2500 | 1218.00 | O18 | LR04 | Hodell et al., 2008 |
87.5900 | 1222.00 | O18 | LR04 | Hodell et al., 2008 |
89.9500 | 1250.00 | O18 | LR04 | Hodell et al., 2008 |
91.8900 | 1290.00 | O18 | LR04 | Hodell et al., 2008 |
94.4300 | 1316.00 | O18 | LR04 | Hodell et al., 2008 |
96.6500 | 1340.00 | O18 | LR04 | Hodell et al., 2008 |
98.2700 | 1354.00 | O18 | LR04 | Hodell et al., 2008 |
100.7550 | 1372.00 | O18 | LR04 | Hodell et al., 2008 |
102.2700 | 1398.00 | O18 | LR04 | Hodell et al., 2008 |
103.0300 | 1406.00 | O18 | LR04 | Hodell et al., 2008 |
103.7400 | 1412.00 | O18 | LR04 | Hodell et al., 2008 |
104.0000 | 1418.00 | O18 | LR04 | Hodell et al., 2008 |
104.6800 | 1426.00 | O18 | LR04 | Hodell et al., 2008 |
105.6800 | 1442.00 | O18 | LR04 | Hodell et al., 2008 |
106.3500 | 1448.00 | O18 | LR04 | Hodell et al., 2008 |
106.5100 | 1456.00 | O18 | LR04 | Hodell et al., 2008 |
108.7500 | 1488.00 | O18 | LR04 | Hodell et al., 2008 |
109.0900 | 1496.00 | O18 | LR04 | Hodell et al., 2008 |
110.0200 | 1510.00 | O18 | LR04 | Hodell et al., 2008 |
112.5500 | 1530.50 | O18 | LR04 | Channell et al., 2016 |
113.8000 | 1546.90 | O18 | LR04 | Channell et al., 2016 |
115.4650 | 1571.10 | O18 | LR04 | Channell et al., 2016 |
116.9900 | 1584.40 | O18 | LR04 | Channell et al., 2016 |
118.9900 | 1610.90 | O18 | LR04 | Channell et al., 2016 |
119.7100 | 1618.80 | O18 | LR04 | Channell et al., 2016 |
120.2250 | 1625.00 | O18 | LR04 | Channell et al., 2016 |
120.7250 | 1628.90 | O18 | LR04 | Channell et al., 2016 |
121.9750 | 1641.40 | O18 | LR04 | Channell et al., 2016 |
123.8850 | 1666.40 | O18 | LR04 | Channell et al., 2016 |
128.4650 | 1698.40 | O18 | LR04 | Channell et al., 2016 |
129.1250 | 1710.80 | O18 | LR04 | Channell et al., 2016 |
130.7150 | 1743.30 | O18 | LR04 | Channell et al., 2016 |
131.4450 | 1752.50 | O18 | LR04 | Channell et al., 2016 |
135.3250 | 1787.50 | O18 | LR04 | Channell et al., 2016 |
136.2450 | 1800.80 | O18 | LR04 | Channell et al., 2016 |
137.9850 | 1815.80 | O18 | LR04 | Channell et al., 2016 |
138.9850 | 1826.70 | O18 | LR04 | Channell et al., 2016 |
140.3250 | 1859.20 | O18 | LR04 | Channell et al., 2016 |
140.6350 | 1870.80 | O18 | LR04 | Channell et al., 2016 |
145.1350 | 1898.30 | O18 | LR04 | Channell et al., 2016 |
145.9950 | 1906.70 | O18 | LR04 | Channell et al., 2016 |
146.7250 | 1913.30 | O18 | LR04 | Channell et al., 2016 |
148.6250 | 1941.70 | O18 | LR04 | Channell et al., 2016 |
150.1050 | 1964.50 | O18 | LR04 | Channell et al., 2016 |
151.8150 | 1998.00 | O18 | LR04 | Channell et al., 2016 |
152.9150 | 2009.00 | O18 | LR04 | Channell et al., 2016 |
156.8850 | 2044.00 | O18 | LR04 | Channell et al., 2016 |
157.4950 | 2047.60 | O18 | LR04 | Channell et al., 2016 |
159.3950 | 2062.90 | O18 | LR04 | Channell et al., 2016 |
160.6550 | 2086.30 | O18 | LR04 | Channell et al., 2016 |
161.9950 | 2116.10 | O18 | LR04 | Channell et al., 2016 |
162.4150 | 2123.40 | O18 | LR04 | Channell et al., 2016 |
164.0650 | 2145.30 | O18 | LR04 | Channell et al., 2016 |
165.1750 | 2167.20 | O18 | LR04 | Channell et al., 2016 |
167.0150 | 2192.70 | O18 | LR04 | Channell et al., 2016 |
168.0750 | 2205.30 | O18 | LR04 | Channell et al., 2016 |
169.6850 | 2236.60 | O18 | LR04 | Channell et al., 2016 |
170.7250 | 2250.30 | O18 | LR04 | Channell et al., 2016 |
174.0950 | 2273.70 | O18 | LR04 | Channell et al., 2016 |
174.9050 | 2290.00 | O18 | LR04 | Channell et al., 2016 |
176.2950 | 2309.50 | O18 | LR04 | Channell et al., 2016 |
178.3750 | 2332.90 | O18 | LR04 | Channell et al., 2016 |
179.8350 | 2349.90 | O18 | LR04 | Channell et al., 2016 |
181.5050 | 2373.30 | O18 | LR04 | Channell et al., 2016 |
184.2150 | 2388.40 | O18 | LR04 | Channell et al., 2016 |
185.9050 | 2406.00 | O18 | LR04 | Channell et al., 2016 |
188.8550 | 2428.80 | O18 | LR04 | Channell et al., 2016 |
189.0550 | 2434.60 | O18 | LR04 | Channell et al., 2016 |
189.2550 | 2463.30 | O18 | LR04 | Channell et al., 2016 |
189.8050 | 2487.40 | O18 | LR04 | Channell et al., 2016 |
190.6250 | 2500.40 | O18 | LR04 | Channell et al., 2016 |
190.8550 | 2520.60 | O18 | LR04 | Channell et al., 2016 |
191.4550 | 2540.10 | O18 | LR04 | Channell et al., 2016 |
193.0550 | 2553.80 | O18 | LR04 | Channell et al., 2016 |
194.6950 | 2571.40 | O18 | LR04 | Channell et al., 2016 |
196.7450 | 2594.80 | O18 | LR04 | Channell et al., 2016 |
197.2950 | 2601.90 | O18 | LR04 | Channell et al., 2016 |
197.6050 | 2650.60 | O18 | LR04 | Channell et al., 2016 |
199.4750 | 2681.20 | O18 | LR04 | Channell et al., 2016 |
200.3950 | 2689.40 | O18 | LR04 | Channell et al., 2016 |
201.7950 | 2704.40 | O18 | LR04 | Channell et al., 2016 |
203.4750 | 2730.60 | O18 | LR04 | Channell et al., 2016 |
210.6050 | 2799.40 | O18 | LR04 | Channell et al., 2016 |
210.8150 | 2805.00 | O18 | LR04 | Channell et al., 2016 |
211.3350 | 2819.50 | O18 | LR04 | Channell et al., 2016 |
212.9950 | 2840.60 | O18 | LR04 | Channell et al., 2016 |
213.5750 | 2847.70 | O18 | LR04 | Channell et al., 2016 |
213.6650 | 2857.00 | O18 | LR04 | Channell et al., 2016 |
216.3350 | 2864.80 | O18 | LR04 | Channell et al., 2016 |
220.1650 | 2876.60 | O18 | LR04 | Channell et al., 2016 |
221.5350 | 2893.00 | O18 | LR04 | Channell et al., 2016 |
224.1950 | 2913.30 | O18 | LR04 | Channell et al., 2016 |
225.6650 | 2936.70 | O18 | LR04 | Channell et al., 2016 |
227.4950 | 2957.00 | O18 | LR04 | Channell et al., 2016 |
228.9450 | 2967.20 | O18 | LR04 | Channell et al., 2016 |
231.3350 | 2982.00 | O18 | LR04 | Channell et al., 2016 |
232.4950 | 2999.20 | O18 | LR04 | Channell et al., 2016 |
233.9150 | 3015.60 | O18 | LR04 | Channell et al., 2016 |
234.9950 | 3025.80 | O18 | LR04 | Channell et al., 2016 |
236.9150 | 3040.60 | O18 | LR04 | Channell et al., 2016 |
237.4150 | 3048.40 | O18 | LR04 | Channell et al., 2016 |
238.6450 | 3059.90 | O18 | LR04 | Channell et al., 2016 |
240.2450 | 3084.90 | O18 | LR04 | Channell et al., 2016 |
241.4650 | 3092.70 | O18 | LR04 | Channell et al., 2016 |
247.0750 | 3134.90 | O18 | LR04 | Channell et al., 2016 |
255.0550 | 3220.00 | pmag | top of Mammoth | Channell et al., 2016 |