Frigola, Jaime (2020): Age determination for borehole PRGL1-4 from the Gulf of Lion, Mediterranean Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.911434, In: Frigola, J (2020): Borehole PRGL1-4 and sediment core MD99-2348 records from the Gulf of Lion, Mediterranean Sea: age model, Globigerina bulloides δ18O, grain-size, XRF-Ca [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.911440
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Frigola, Jaime; Canals, Miquel; Cacho, Isabel; Moreno, Ana; Sierro, Francisco Javier; Berné, Serge; Jouet, Gwenael; Dennielou, Bernard; Herrera, Gemma; Pasqual, C; Galavazi, M; Grimalt, Joan O; Schneider, Ralph R (2012): A 500 kyr record of global sea-level oscillations in the Gulf of Lion, Mediterranean Sea: new insights into MIS 3 sea-level variability. Climate of the Past, 8(3), 1067-1077, https://doi.org/10.5194/cp-8-1067-2012
Further details:
Lisiecki, Lorraine E; Raymo, Maureen E (2005): A Pliocene-Pleistocene stack of 57 globally distributed benthic d18O records. Paleoceanography, 20, PA1003, https://doi.org/10.1029/2004PA001071
Martrat, Belén; Grimalt, Joan O; López-Martinez, Constancia; Cacho, Isabel; Sierro, Francisco Javier; Flores, José-Abel; Zahn, Rainer; Canals, Miquel; Curtis, Jason H; Hodell, David A (2004): Abrupt Temperature Changes in the Western Mediterranean over the Past 250,000 Years. Science, 306(5702), 1762-1765, https://doi.org/10.1126/science.1101706
Roucoux, Katherine H; Tzedakis, Polychronis C; de Abreu, Lucia; Shackleton, Nicholas J (2006): Climate and vegetation changes 180,000 to 345,000 years ago recorded in a deep-sea core off Portugal. Earth and Planetary Science Letters, 249(3-4), 307-325, https://doi.org/10.1016/j.epsl.2006.07.005
Sierro, Francisco Javier; Andersen, Nils; Bassetti, Maria Angela; Berné, Serge; Canals, Miquel; Curtis, Jason H; Dennielou, Bernard; Flores, José Abel; Frigola, Jaime; Gonzalez-Mora, Beatriz; Grimalt, Joan O; Hodell, David A; Jouet, Gwenael; Pérez-Folgado, Marta; Schneider, Ralph R (2009): Phase relationship between sea level and abrupt climate change. Quaternary Science Reviews, 28(25-26), 2867-2881, https://doi.org/10.1016/j.quascirev.2009.07.019
Stein, Ruediger; Hefter, Jens; Gruetzner, Jens; Voelker, Antje H L; Naafs, Bernhard David A (2009): Variability of surface water characteristics and Heinrich-like events in the Pleistocene midlatitude North Atlantic Ocean: Biomarker and XRD records from IODP Site U1313 (MIS 16 - 9). Paleoceanography, 24(2), PA2203, https://doi.org/10.1029/2008PA001639
Svensson, Anders M; Andersen, Katrine K; Bigler, Matthias; Clausen, Henrik Brink; Dahl-Jensen, Dorthe; Davies, Siwan M; Johnsen, Sigfús Jóhann; Muscheler, Raimund; Parrenin, Frédéric; Rasmussen, Sune Olander; Röthlisberger, Regine; Seierstad, Inger K; Steffensen, Jørgen Peder; Vinther, Bo Møllesøe (2008): A 60 000 year Greenland stratigraphic ice core chronology. Climate of the Past, 4(1), 47-57, https://doi.org/10.5194/cp-4-47-2008
Project(s):
Funding:
Fifth Framework Programme (FP5), grant/award no. EVR1-CT-2002-40024: Profiles across Mediterranean Sedimentary Systems
Coverage:
Latitude: 42.689846 * Longitude: 3.837663
Date/Time Start: 2004-07-09T20:30:00 * Date/Time End: 2004-07-16T00:30:00
Minimum DEPTH, sediment/rock: 19.74 m * Maximum DEPTH, sediment/rock: 299.34 m
Event(s):
PRGL1-4 * Latitude: 42.689846 * Longitude: 3.837663 * Date/Time Start: 2004-07-09T20:30:00 * Date/Time End: 2004-07-16T00:30:00 * Elevation: -298.5 m * Penetration: 300.3 m * Recovery: 304.36 m * Location: Gulf of Lions * Campaign: PROMESS1 * Basis: Bavenit * Method/Device: Drilling/drill rig (DRILL) * Comment: WGS84; Sample hole, Downhole Logging II - 356 cores; 304.36 m cored; 101.25 % recovery
Comment:
This age model is an update and extension of previously published PRGL1-4 age model from Sierro et al., 2009
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Frigola, Jaime | Geocode – Core depth | |
2 | Calendar age | Cal age | ka BP | Frigola, Jaime | ||
3 | Geological event | Geological e | Frigola, Jaime | Reference time event | ||
4 | Reference/source | Reference | Frigola, Jaime | Reference core used for synchronization of δ18O records | ||
5 | Reference of data | Ref data | Frigola, Jaime | Reference of publication | ||
6 | DEPTH, sediment/rock | Depth sed | m | Frigola, Jaime | Geocode – Core depth | |
7 | Calendar age | Cal age | ka BP | Frigola, Jaime | calibrated | From synchronazation of G. bulloides δ18O records from borehole PRGL1-4 with those from other cores with age models already published (see reference of publication) |
8 | Sedimentation rate | SR | cm/ka | Frigola, Jaime | Linear sedimentation rate |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
656 data points
Data
1 Depth sed [m] (Core depth) | 2 Cal age [ka BP] | 3 Geological e (Reference time event) | 4 Reference (Reference core used for synch...) | 5 Ref data (Reference of publication) | 6 Depth sed [m] (Core depth) | 7 Cal age [ka BP] (From synchronazation of G. bu...) | 8 SR [cm/ka] (Linear sedimentation rate) |
---|---|---|---|---|---|---|---|
19.74 | 23.28 | Base GIS 2 | NGRIP | Svensson et al., 2008 | 19.74 | 23.28 | 209 |
25.05 | 25.82 | Maximum | NGRIP | Svensson et al., 2008 | 25.05 | 25.82 | 209 |
27.46 | 27.46 | Top GIS 3 | NGRIP | Svensson et al., 2008 | 25.05 | 25.82 | 147 |
27.99 | 27.84 | Base GIS 3 | NGRIP | Svensson et al., 2008 | 27.46 | 27.46 | 147 |
28.90 | 28.50 | Top GIS 4 | NGRIP | Svensson et al., 2008 | 27.46 | 27.46 | 139 |
29.50 | 28.90 | Base GIS 4 | NGRIP | Svensson et al., 2008 | 27.99 | 27.84 | 139 |
31.56 | 30.72 | peak GIS 4.1 | NGRIP | Svensson et al., 2008 | 27.99 | 27.84 | 138 |
32.88 | 32.04 | Top GIS 5 | NGRIP | Svensson et al., 2008 | 28.90 | 28.50 | 138 |
33.30 | 32.52 | Base GIS 5 | NGRIP | Svensson et al., 2008 | 28.90 | 28.50 | 150 |
33.86 | 33.38 | Top GIS 6 | NGRIP | Svensson et al., 2008 | 29.50 | 28.90 | 150 |
34.30 | 33.80 | Base GIS 6 | NGRIP | Svensson et al., 2008 | 29.50 | 28.90 | 113 |
35.30 | 34.72 | Top GIS 7 | NGRIP | Svensson et al., 2008 | 31.56 | 30.72 | 113 |
35.65 | 35.46 | Base GIS 7 | NGRIP | Svensson et al., 2008 | 31.56 | 30.72 | 100 |
36.18 | 36.60 | Top GIS 8 | NGRIP | Svensson et al., 2008 | 32.88 | 32.04 | 100 |
36.75 | 38.24 | Base GIS 8 | NGRIP | Svensson et al., 2008 | 32.88 | 32.04 | 88 |
37.77 | 39.96 | Top GIS 9 | NGRIP | Svensson et al., 2008 | 33.30 | 32.52 | 88 |
38.13 | 40.16 | Base GIS 9 | NGRIP | Svensson et al., 2008 | 33.30 | 32.52 | 66 |
39.56 | 41.10 | Top GIS 10 | NGRIP | Svensson et al., 2008 | 33.86 | 33.38 | 66 |
40.08 | 41.50 | Base GIS 10 | NGRIP | Svensson et al., 2008 | 33.86 | 33.38 | 104 |
40.88 | 42.13 | Top GIS 11 | NGRIP | Svensson et al., 2008 | 34.30 | 33.80 | 104 |
42.12 | 43.33 | Base GIS 11 | NGRIP | Svensson et al., 2008 | 34.30 | 33.80 | 109 |
43.00 | 44.33 | Top GIS 12 | NGRIP | Svensson et al., 2008 | 35.30 | 34.72 | 109 |
44.65 | 46.98 | Base GIS 12 | NGRIP | Svensson et al., 2008 | 35.30 | 34.72 | 47 |
46.12 | 48.16 | Top GIS 13 | NGRIP | Svensson et al., 2008 | 35.65 | 35.46 | 47 |
47.46 | 49.28 | Base GIS 13 | NGRIP | Svensson et al., 2008 | 35.65 | 35.46 | 46 |
48.98 | 51.68 | Top GIS 14 | NGRIP | Svensson et al., 2008 | 36.18 | 36.60 | 46 |
49.50 | 54.22 | Base GIS 14 | NGRIP | Svensson et al., 2008 | 36.18 | 36.60 | 35 |
50.39 | 55.42 | Top GIS 15 | NGRIP | Svensson et al., 2008 | 36.75 | 38.24 | 35 |
50.66 | 55.78 | Base GIS 15 | NGRIP | Svensson et al., 2008 | 36.75 | 38.24 | 59 |
51.38 | 56.38 | Top GIS 16 | NGRIP | Svensson et al., 2008 | 37.77 | 39.96 | 59 |
52.37 | 58.32 | Base GIS 16 | NGRIP | Svensson et al., 2008 | 37.77 | 39.96 | 180 |
53.60 | 59.44 | Base GIS 17 | NGRIP | Svensson et al., 2008 | 38.13 | 40.16 | 180 |
58.56 | 63.90 | Top GIS 18 | NGRIP | Svensson et al., 2008 | 38.13 | 40.16 | 152 |
63.59 | 70.70 | Top GIS 19 | NGRIP | Svensson et al., 2008 | 39.56 | 41.10 | 152 |
63.90 | 72.40 | Base GIS 19 | NGRIP | Svensson et al., 2008 | 39.56 | 41.10 | 131 |
63.99 | 74.05 | Top GIS 20 | NGRIP | Svensson et al., 2008 | 40.08 | 41.50 | 131 |
64.25 | 76.40 | Base GIS 20 | NGRIP | Svensson et al., 2008 | 40.08 | 41.50 | 128 |
64.98 | 77.85 | Top GIS 21 | NGRIP | Svensson et al., 2008 | 40.88 | 42.13 | 128 |
65.59 | 84.80 | Base GIS 21 | NGRIP | Svensson et al., 2008 | 40.88 | 42.13 | 103 |
66.14 | 87.75 | Top GIS 22 | NGRIP | Svensson et al., 2008 | 42.12 | 43.33 | 103 |
66.50 | 90.10 | Base GIS 22 | NGRIP | Svensson et al., 2008 | 42.12 | 43.33 | 88 |
67.30 | 104.05 | Base GIS 23 | NGRIP | Svensson et al., 2008 | 43.00 | 44.33 | 88 |
67.90 | 105.45 | Top GIS 24 | NGRIP | Svensson et al., 2008 | 43.00 | 44.33 | 62 |
68.70 | 108.30 | Base GIS 24 | NGRIP | Svensson et al., 2008 | 44.65 | 46.98 | 62 |
69.99 | 110.65 | Top GIS 25 | NGRIP | Svensson et al., 2008 | 44.65 | 46.98 | 125 |
71.20 | 118.70 | Top GIS 26 | NGRIP | Svensson et al., 2008 | 46.12 | 48.16 | 125 |
72.27 | 126.00 | MIS 5.53 | IODP977 | Martrat et al., 2004 | 46.12 | 48.16 | 120 |
72.45 | 133.00 | T II | IODP977 | Martrat et al., 2004 | 47.46 | 49.28 | 120 |
103.27 | 149.60 | Base AI 3´ | IODP977 | Martrat et al., 2004 | 47.46 | 49.28 | 63 |
110.88 | 162.00 | Top 6.5 =Top AI 6´ | IODP977 | Martrat et al., 2004 | 48.98 | 51.68 | 63 |
112.08 | 165.42 | 2nd warming in 6.5 = AI 6´ | IODP977 | Martrat et al., 2004 | 48.98 | 51.68 | 20 |
112.87 | 170.77 | 1st warming in 6.5 = AI 7´ | IODP977 | Martrat et al., 2004 | 49.50 | 54.22 | 20 |
114.47 | 175.05 | Base 6.5 = AI 8´ | IODP977 | Martrat et al., 2004 | 49.50 | 54.22 | 74 |
117.88 | 180.00 | Max isot - AS 9´ | IODP977 | Martrat et al., 2004 | 50.39 | 55.42 | 74 |
119.12 | 181.41 | Min isot - AI 9´ | IODP977 | Martrat et al., 2004 | 50.39 | 55.42 | 76 |
121.76 | 184.00 | Base AI 9´ | IODP977 | Martrat et al., 2004 | 50.66 | 55.78 | 76 |
123.11 | 186.72 | Top AS 10` | IODP977 | Martrat et al., 2004 | 50.66 | 55.78 | 119 |
123.44 | 191.00 | Top MIS 7 | L&R04 | Lisieki and Raymo, 2005 | 51.38 | 56.38 | 119 |
124.09 | 201.00 | MIS 7.1 | L&R04 | Lisieki and Raymo, 2005 | 51.38 | 56.38 | 51 |
125.37 | 205.00 | MIS 7.2 | L&R04 | Lisieki and Raymo, 2005 | 52.37 | 58.32 | 51 |
125.75 | 217.00 | MIS 7.3 | L&R04 | Lisieki and Raymo, 2005 | 52.37 | 58.32 | 110 |
125.97 | 222.52 | Base MIS 7.3 | L&R04 | Lisieki and Raymo, 2005 | 53.60 | 59.44 | 110 |
127.36 | 232.00 | Top MIS 7.5 | L&R04 | Lisieki and Raymo, 2005 | 53.60 | 59.44 | 111 |
127.57 | 240.00 | MIS 7.5 | L&R04 | Lisieki and Raymo, 2005 | 58.56 | 63.90 | 111 |
128.19 | 246.00 | T III | L&R04 | Lisieki and Raymo, 2005 | 58.56 | 63.90 | 74 |
142.05 | 266.00 | Bottom MIS 8.43 | L&R04 | Lisieki and Raymo, 2005 | 63.59 | 70.70 | 74 |
157.10 | 277.00 | Base MIS 8.4 | L&R04 | Lisieki and Raymo, 2005 | 63.59 | 70.70 | 18 |
157.78 | 286.00 | MIS 8.5 | L&R04 | Lisieki and Raymo, 2005 | 63.90 | 72.40 | 18 |
159.00 | 295.00 | MIS 8.6 | L&R04 | Lisieki and Raymo, 2005 | 63.90 | 72.40 | 5 |
159.43 | 304.00 | Polen Zone MD-7 | MD01-2443 | Roucoux et al., 2006 | 63.99 | 74.05 | 5 |
159.91 | 307.00 | Polen Zone MD-6 | MD01-2443 | Roucoux et al., 2006 | 63.99 | 74.05 | 11 |
160.24 | 314.00 | Polen Zone MD-5 | MD01-2443 | Roucoux et al., 2006 | 64.25 | 76.40 | 11 |
160.71 | 320.00 | Polen Zone MD-4 | MD01-2443 | Roucoux et al., 2006 | 64.25 | 76.40 | 50 |
161.20 | 328.00 | MIS 9.3 | L&R04 | Lisieki and Raymo, 2005 | 64.98 | 77.85 | 50 |
162.91 | 337.00 | T IV | L&R04 | Lisieki and Raymo, 2005 | 64.98 | 77.85 | 9 |
185.42 | 360.00 | Base MIS 10.4 | IODP U1313 | Stein et al., 2009 | 65.59 | 84.80 | 9 |
196.76 | 383.00 | MIS 11.23 | IODP U1313 | Stein et al., 2009 | 65.59 | 84.80 | 19 |
197.92 | 390.00 | MIS 11.24 | IODP U1313 | Stein et al., 2009 | 66.14 | 87.75 | 19 |
199.12 | 406.00 | MIS 11.3 | L&R04 | Lisieki and Raymo, 2005 | 66.14 | 87.75 | 15 |
212.00 | 424.00 | T V | Sierro, F.J. | 66.50 | 90.10 | 15 | |
290.30 | 491.00 | MIS 13.1 | Sierro, F.J. | 66.50 | 90.10 | 6 | |
295.02 | 513.00 | MIS 13.2 | Sierro, F.J. | 67.30 | 104.05 | 6 | |
299.34 | 525.00 | MIS 13.3 | Sierro, F.J. | 67.30 | 104.05 | 43 | |
67.90 | 105.45 | 43 | |||||
67.90 | 105.45 | 28 | |||||
68.70 | 108.30 | 28 | |||||
68.70 | 108.30 | 55 | |||||
69.99 | 110.65 | 55 | |||||
69.99 | 110.65 | 15 | |||||
71.20 | 118.70 | 15 | |||||
71.20 | 118.70 | 15 | |||||
72.27 | 126.00 | 15 | |||||
72.27 | 126.00 | 3 | |||||
72.45 | 133.00 | 3 | |||||
72.45 | 133.00 | 186 | |||||
103.27 | 149.60 | 186 | |||||
103.27 | 149.60 | 61 | |||||
110.88 | 162.00 | 61 | |||||
110.88 | 162.00 | 35 | |||||
112.08 | 165.42 | 35 | |||||
112.08 | 165.42 | 15 | |||||
112.87 | 170.77 | 15 | |||||
112.87 | 170.77 | 37 | |||||
114.47 | 175.05 | 37 | |||||
114.47 | 175.05 | 69 | |||||
117.88 | 180.00 | 69 | |||||
117.88 | 180.00 | 88 | |||||
119.12 | 181.41 | 88 | |||||
119.12 | 181.41 | 102 | |||||
121.76 | 184.00 | 102 | |||||
121.76 | 184.00 | 50 | |||||
123.11 | 186.72 | 50 | |||||
123.11 | 186.72 | 8 | |||||
123.44 | 191.00 | 8 | |||||
123.44 | 191.00 | 6 | |||||
124.09 | 201.00 | 6 | |||||
124.09 | 201.00 | 32 | |||||
125.37 | 205.00 | 32 | |||||
125.37 | 205.00 | 3 | |||||
125.75 | 217.00 | 3 | |||||
125.75 | 217.00 | 4 | |||||
125.97 | 222.52 | 4 | |||||
125.97 | 222.52 | 15 | |||||
127.36 | 232.00 | 15 | |||||
127.36 | 232.00 | 3 | |||||
127.57 | 240.00 | 3 | |||||
127.57 | 240.00 | 10 | |||||
128.19 | 246.00 | 10 | |||||
128.19 | 246.00 | 69 | |||||
142.05 | 266.00 | 69 | |||||
142.05 | 266.00 | 137 | |||||
157.10 | 277.00 | 137 | |||||
157.10 | 277.00 | 8 | |||||
157.78 | 286.00 | 8 | |||||
157.78 | 286.00 | 14 | |||||
159.00 | 295.00 | 14 | |||||
159.00 | 295.00 | 5 | |||||
159.43 | 304.00 | 5 | |||||
159.43 | 304.00 | 16 | |||||
159.91 | 307.00 | 16 | |||||
159.91 | 307.00 | 5 | |||||
160.24 | 314.00 | 5 | |||||
160.24 | 314.00 | 8 | |||||
160.71 | 320.00 | 8 | |||||
160.71 | 320.00 | 6 | |||||
161.20 | 328.00 | 6 | |||||
161.20 | 328.00 | 19 | |||||
162.91 | 337.00 | 19 | |||||
162.91 | 337.00 | 98 | |||||
185.42 | 360.00 | 98 | |||||
185.42 | 360.00 | 49 | |||||
196.76 | 383.00 | 49 | |||||
196.76 | 383.00 | 17 | |||||
197.92 | 390.00 | 17 | |||||
197.92 | 390.00 | 7 | |||||
199.12 | 406.00 | 7 | |||||
199.12 | 406.00 | 72 | |||||
212.00 | 424.00 | 72 | |||||
212.00 | 424.00 | 117 | |||||
290.30 | 491.00 | 117 | |||||
290.30 | 491.00 | 21 | |||||
295.02 | 513.00 | 21 | |||||
295.02 | 513.00 | 36 | |||||
299.34 | 525.00 | 36 |