• Keine Ergebnisse gefunden

Core no.

N/A
N/A
Protected

Academic year: 2022

Aktie "Core no."

Copied!
2
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

Core no. 16396-1 G.C. N 61° 52.33’ W 11° 14.54’ : 1145 m b.s.l.

Age control: Date: 9/2000

N. pachyderma sin. δ18O record from K.Winn/F.Werner (unpublished data), Sarnthein et al. (1995)

• AMS 14C dating on G. bulloides and N. pachyderma sin. (Weinelt et al., in prep.).

Core fit :

• with neighbour core 16397-2, based on δ18O record and AMS 14C dating

• 510 cm in core 16396-1 = 80 cm in core 16397-2 Surface sediment age :

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

170 11.23 80 13.16 a) - . - G. bulloides - 1

180 13.97 80 16.76 a) 2.8 N. pachyderma sin. - 1

198 15.08 150 18.00 a) - . - N. pachyderma sin. - 1 ignored

198 18.10 13.4 Base H1 - 1

290 15.73 100 18.78 a) 135.3 N. pachyderma sin. - 1

430 16.83 90 20.05 a) 110.2 N. pachyderma sin. - 1

510 21.12 74.8 tuned with core 16397

530 17.40 90 21.29 a) 117.6 N. pachyderma sin. - 1

a) Calendar years converted from 14C years using INTCAL 98.

Remarks :

• None

Original references:

• Weinelt et al., in prep.

• Sarnthein, M., Jansen, E., Weinelt, M., Arnold, M., Duplessy, J.-C., Erlenkeuser, H., Flatøy, A., Johannessen, G., Johannessen, T., Jung, S., Koc, N., Maslin, M., Pflaumann, U. & Schulz, H. (1995): Variations in Atlantic surface ocean paleoceanography, 50° - 85°N: A time-slice record of the last 30,000 years. - Paleoceanography, 10, 1063-1094.

• Werner, F. (1990): Bericht über Reise Nr. 158 des F. S. POSEIDON in das Seegebiet um Island. - Ber.-Rep. Geol.

Paläont. Inst. Univ. Kiel, 38, 17 pp.

LGM time slice:

• GLAMAP: 198-540 cm orig. depth in core (-1)

• EPILOG: 320-540 cm orig. depth in core (-1)

LGM foraminifera counts: Vogelsang (EV), Weinelt (MW)

• GLAMAP: (in core -1) 198, 198, 210, 230, 250, 270, 290, 298, 302, 310, 330, 350, 360, 370, 380, 390, 398, 402, 410, 420, 420, 430, 440, 450, 460, 470, 480, 490, 498, 502, 510, 520, 530, 540 cm orig. depth.

• EPILOG: (in core -1) 330, 350, 360, 370, 380, 390, 398, 402, 410, 420, 420, 430, 440, 450, 460, 470, 480, 490, 498, 502, 510, 520, 530, 540 cm orig. depth.

References for faunal analysis:

• Weinelt et al., Paleoceanography, in prep.

(2)

winter

J J

J JJ

JJ

J J J JJ J

JJJJ J J J J JJJJ J JJJJJJJJJJJJJJJJJJJJJJJ E

E E EE

EE

E E E EE

E

EEEE E E E E EEEE E EE

EEEEEEEEE

EEEEEEEEEE EE

-4 0 4 8

0 100 200 300 400 500 600

Depth (cm)

° C

summer

16465: N. pachyderma sin.

18394: G. bulloides

DD

DD DDD

D D

D D

D DDDDDD

DDDDDD

DDDDDDDDDDDD

DDDDDDDDD DDDDDD

5 4 3 2

16396-1

N. pachyderma sin.

EPILOG GLAMAP 13970

11230

15080

15730 16830

17400

(‰)

Referenzen

ÄHNLICHE DOKUMENTE

The research programme during the cruise included measurements of the physical properties of the water column (temperature and salinity), the sampling of particulate organic

sche Eis fließt, kann es lokaJ auf dem Schelf im Bereich der Polarfront zur Bildung von Meereis und schweren Wassermassen kommen, die über die Sehelfkante abfließen und

POSEIDON in das Seegebiet um

• Zero, based on undisturbed sediment surface of B.C.. wuellerstorfi are unreliable due to a

(1996): Wassermassenaustausch zwischen dem NE-Atlantik und dem Europäischen Nordmeer während der letzten 300.000/80.000 Jahre im Abbild stabiler O- und C-Isotope.- Ber..

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

(1987): Benthic isotope evidence for changes of the Mediterranean outflow during the Late Quaternary.- Paleoceanography, 2, 543-559.. •

(1987): Benthic isotope evidence for changes of the Mediterranean outflow during the Late Quaternary.- Paleoceanography, 2, 543-559.. •