Depth
(mcd)
|
![]()
(‰)
|
Age
(a)
|
Sedimentation rate
(m/ky)
|
Event
|
---|---|---|---|---|
0.06 | –2.72 | 90 | — | |
6.73 | –1.53 | 11,730 | 0.57 | Top YD |
10.01 | –2.04 | 14,375 | 1.24 | IS 1 |
26.19 | –1.17 | 23,370 | 1.80 | IS 2 |
26.89 | –0.62 | 23,810 | 1.59 | H2 |
31.62 | –1.55 | 27,700 | 1.22 | IS 3 |
33.07 | –1.56 | 28,890 | 1.22 | IS 4 |
33.57 | –1.05 | 29,290 | 1.25 | H3 |
36.62 | –1.62 | 31,720 | 1.26 | IS 5 |
38.63 | –1.57 | 33,790 | 0.97 | IS 6 |
41.76 | –1.7 | 36,660 | 1.09 | IS 7 |
44.02 | –1.76 | 38,320 | 1.36 | IS 8 |
44.52 | –1.1 | 38,770 | 1.11 | H4 |
45.52 | –0.14 | 39,660 | 1.12 | IS 9 |
46.97 | –1.72 | 40,960 | 1.12 | IS 10 |
48.73 | –1.77 | 42,530 | 1.12 | IS 11 |
52.9 | –1.66 | 45,140 | 1.60 | IS 12 |
53.56 | –1.04 | 45,660 | 1.27 | H5 |
55.06 | –1.58 | 47,090 | 1.05 | IS 13 |
64.77 | –2.22 | 56,370 | 1.05 | IS 16 |
66.47 | –1.67 | 58,230 | 0.91 | IS 17 |
70.33 | –1.53 | 61,870 | 1.06 | IS 18 |
77.96 | –2.13 | 68,610 | 1.13 | IS 19 |
81.21 | –1.94 | 72,880 | 0.76 | IS 20 |
88.57 | –2.49 | 83,750 | 0.68 | IS 21 |
95.42 | –2.23 | 89,710 | 1.15 | IS 22 |
104.13 | –2.5 | 100,250 | 0.83 | IS 23 |
106.81 | –1.63 | 106,360 | 0.44 | MIS 5.4 |
110.05 | –2.45 | 116,000 | 0.34 | Hiatus top |
110.3 | –1.68 | 128,000 | — | Hiatus bottom |
112.05 | –2.51 | 130,000 | 0.47 | MIS 5.53 |
114.55 | –0.82 | 134,000 | 0.52 | MIS 6.2 top |
133.42 | –1.5 | 141,300 | 0.57 | MIS 6.3 |
143.53 | –0.64 | 155,300 | 0.57 | MIS 6.44 |
157.95 | –2.22 | 167,310 | 0.57 | MIS 6.53 |
168.55 | –1.23 | 177,270 | 1.06 | MIS 6.62 |
172.16 | –0.95 | 181,500 | 0.85 | MIS 6.64 |
179.6 | –2.07 | 194,970 | 0.55 | MIS 7.1 |
188.11 | –2.07 | 215,930 | 0.41 | MIS 7.3 |
190.11 | –1.34 | 220,870 | 0.40 | MIS 7.4 |
195.49 | –2.58 | 234,170 | 0.40 | MIS 7.5 |
195.99 | –1.58 | 235,410 | 0.40 | Hiatus top |
196.24 | –1.96 | 286,000 | — | Hiatus bottom |
196.77 | –2.17 | 287,630 | 0.33 | MIS 8.5 |
198.75 | –1.31 | 293,720 | 0.33 | MIS 8.6 |
205.15 | –2.52 | 313,350 | 0.33 | MIS 9.1 |
205.4 | –1.68 | 318,700 | — | MIS 9.2 |
207.4 | –2.71 | 329,030 | 0.19 | MIS 9.3 |
209.16 | –0.46 | 342,000 | 0.59 | MIS 10.2 |
220.3 | –0.76 | 347,500 | 2.02 | MIS 10.4 |
236.95 | –2.19 | 368,320 | 0.80 | MIS 11.1 |
238.95 | –1.04 | 372,440 | 0.49 | MIS 11.23 |
245.63 | –2.18 | 386,270 | 0.48 | Hiatus top |
246.33 | –1.74 | 412,000 | — | Hiatus bottom |
248.89 | –2.56 | 418,530 | 0.36 | MIS 11.33 |
251.58 | –0.63 | 426,000 | 0.36 | MIS 12.22 |
262.18 | –0.37 | 434,000 | 0.33 | MIS 12.24 |
275.87 | –0.6 | 461,470 | 0.49 | MIS 12.4 |
291.23 | –2.27 | 500,000 | 0.39 | MIS 13.13 |
300.77 | –2.06 | 523,000 | 0.41 | MIS 13.3 |
306.52 | –1.21 | 537,300 | 0.40 | MIS 14.2 |
311.11 | –1.51 | 559,500 | 0.21 | MIS 14.44 |
318.86 | –2.48 | 573,500 | 0.55 | MIS 15.1 |
323.86 | –2.38 | 598,000 | 0.20 | MIS 15.3 |
324.62 | –2.12 | 598,035 | 0.20 | Hiatus top |
324.86 | –0.77 | 626,580 | — | Hiatus bottom |
326.12 | –0.89 | 628,000 | 0.89 | MIS 16.2 |
345.42 | –0.69 | 649,500 | 0.89 | MIS 16.4 |
355.79 | –2.25 | 690,000 | 0.26 | MIS 17.3 |
365.92 | –0.85 | 720,500 | 0.33 | MIS 18.2 |
377.17 | –0.89 | 747,000 | 0.42 | MIS 18.4 |
384.58 | –2.43 | 783,700 | 0.20 | MIS 19.3 |
388.83 | –0.84 | 794,300 | 0.40 | MIS 20.2 |
397.78 | –2.31 | 838,500 | 0.20 | MIS 21.3 |
399.28 | –2.16 | 858,500 | 0.21 | MIS 21.5 |
403.51 | –0.89 | 870,500 | 0.35 | MIS 22.2 |
408.51 | –0.85 | 883,240 | 0.39 | MIS 22.4 |
413.89 | –1.85 | 900,000 | 0.32 | MIS 23 |
415.88 | –0.99 | 908,000 | 0.25 | MIS 24 |
421.88 | –2.18 | 940,000 | 0.19 | MIS 25 |
426.7 | –0.9 | 955,000 | 0.32 | MIS 26 |
450.43 | –0.81 | 1,004,000 | 0.48 | MIS 28 |
472.31 | –1.16 | 1,037,000 | 0.66 | MIS 30 |
500.66 | 1,093,790 | 0.50 | LO small Gephyrocapsa acme | |
503.76 | –2.32 | 1,100,000 | 0.50 | MIS 34. top |
Hiatus | ||||
506.82 | –1.59 | 1,960,000 | — | LO Discoaster brouweri/triradiatus |
517.56 | –2.07 | 1,975,600 | 0.50 | MIS 73 |
Notes: YD = Younger Dryas, IS = GISP2 interstadial equivalent. LO = last occurrence. Ages of last 110 k.y. are based on the Meese/Sowers timescale (Meese et al., 1994). H1–H6 = Heinrich event analog. Ages of MIS 6–34 are based on Shackleton et al. (1990) and Bassinot et al. (1994); nannofossil ages after to Shipboard Scientific Party (2000).