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Core no. 15669-1 G.C. N 34° 53.5' W 7° 48.9': 2022 m b.s.l.

Age control: Date: 28/06/1991

C. wuellerstorfi δ18O record from Zahn-Knoll, 1986.

14C ages on carbonate coarse fraction (Zahn et al., 1987).

• AMS 14C analogue stratigraphy.

Core fit :

• None

Surface sediment age :

• 1.9 ka, assuming 6 cm loss of surface sediment, per analogy with neighbouring cores.

Age/depth correlation : Orig.

depth

14C age Error

± Calendar

years Sed.rate Original interval/

material/ Core

no. Remarks

[cm] [ky BP] [ka] [cm/ky] 18O stratigraphy

0 1.9 - . - - 1

15 4.46 50 5.05 a) - . - 10- 20 cm

carbonate >125µm - 1 ignored b)

25 9.1 9.8 c) 3.21 AMS 14C analogue - 1

45 12.37 150 14.37 c) 4.38 40- 50 cm

carbonate >125µm - 1

60 13.6 17.1 c) - . - AMS 14C analogue - 1 ignored

65 14.8 18.3 c) 5.09 AMS 14C analogue - 1

78 16.63 330 20.13 c) - . - 73- 83 cm

carbonate >125µm - 1 good, but ignored

125 22.82 630 26.32 c) - . - 120-130 cm

carbonate >125µm - 1 ignored

135 26 29.5 c) 6.25 AMS 14C analogue - 1

a) see Winn et al. (1991).

b) near surface bioturbation.

c) corrected after Bard et al. (1990).

Remarks:

• None

Original references:

• Sarnthein, M., Winn, K., Jung, S.J.A., Duplessy, J.-A., Labeyrie, L., Erlenkeuser, H. & Ganssen, G. (1994): Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions.- Paleoceanography, 9, 209-267.

• Winn, K., Sarnthein, M. & Erlenkeuser, H. (1991): δ18O stratigraphy and chronology of Kiel sediment cores from the East Atlantic.- Ber.-Rep. Geol. Paläont. Inst. Univ. Kiel, 45, 99 pp.

• Zahn, R., Sarnthein, M. & Erlenkeuser, H. (1987): Benthic isotope evidence for changes of the Mediterranean outflow during the Late Quaternary.- Paleoceanography, 2, 543-559.

• Zahn-Knoll, R. (1986): Spätquartäre Entwicklung von Küstenauftrieb und Tiefenwasserzirkulation im Nordost- Atlantik. Rekonstruktion anhand stabiler Isotope kalkschaliger Foraminiferen.- Diss. Univ. Kiel, 111 pp.

LGM time slice:

• GLAMAP: 65-85 cm orig. depth in core (-1)

• EPILOG: 69-91 cm orig. depth in core (-1) LGM foraminifera counts: Pflaumann (UP)

• GLAMAP: (in core -1) 65, 70, 75, 80, 85 cm orig. depth.

• EPILOG: (in core -1) 70, 75, 80, 85, 90 cm orig. depth.

References for faunal analysis:

• Pflaumann et al., Paleoceanography, in prep.

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winter

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E E

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8 12 16 20

0 50 100 150 200 250

Depth (cm)

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summer

D DDDD DDDD

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C. wuellerstorfi EPILOG

GLAMAP

15669-1

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