• 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. 16017-2 G.C. N 21° 14.7' W 17° 48.2': 812 m b.s.l.

Age control: Date: 11/03/1992

C. wuellerstorfi, U. mediterranea δ18O records from Zahn-Knoll (1986), Winn et al. (1991) and Sarnthein et al.

(1994).

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

• AMS 14C analogue stratigraphy.

Core fit :

• None

Surface sediment age :

• Zero, assuming no sediment loss at surface of G.C. -1.

Age/depth correlation : Orig.

depth

14C age Error

±

Calendar years

Sed.rate Original interval/ material/ Remarks

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

0 0

13 3.6 85 3.91 a) - . - 10-16 cm, carb. >125µm ignored b)

37.5 7.2 430 8.05 a) - . - 35-40 cm, carb. >125µm ignored b)

80 11.47 110 13.47 c) - . - 76- 84 cm, carb. >125µm ignored b)

120 13.7 140 17.2 c) - . - 117-123 cm, carb. >125µm ignored b)

125.5 9.1 9.8 c) 12.81 AMS 14C analogue d)

160.5 11.6 c) 19.44 Top Younger Dryas GISP2, d)

160 16.06 230 19.56 c) - . - 156-164 cm, carb. >125µm ignored b)

216.5 15.36 490 18.86 c) - . - 211- 222 cm, carb. >500µm ignored b)

216.5 15.7 150 19.2 c) - . - 211- 222 cm,

carb. 200-500µm

ignored b)

216.5 17.80 220 21.3 c) - . - 211- 222 cm

carb. 125-200µm

ignored b)

220.5 13.6 17.1 c) 10.91 AMS 14C analogue

225 20.06 300 23.56 c) - . - 222- 228 cm, carb. >125µm ignored b)

235.5 14.8 18.3 c) 12.5 AMS 14C analogue d)

280 25.49 770 28.99 c) - . - 276- 284 cm, carb. >125µm ignored b)

310 29.52 850 ?33.02 c) - . - 307- 313 cm, carb. >125µm ignored b)

340.5 26 29.5 c) 9.37 AMS 14C analogue

a) see Winn et al. (1991).

b) 14C ages probably too old because of downslope sediment reworking.

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

d) Based on Cibicides wuellerstorfi δ18O (comparison with core 12345-5).

Remarks :

• Dry bulk density data (U. Pflaumann, unpublished).

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: 235.5-265.5 cm orig. depth in core (-2)

• EPILOG: 242-275 cm orig. depth in core (-2) LGM foraminifera counts: Pflaumann (UP)

• GLAMAP: (in core -2) 240, 245, 250, 255, 260, 265 cm orig. depth.

• EPILOG: (in core -2) 245, 250, 255, 260, 265, 270, 275 cm orig. depth.

References for faunal analysis:

• Pflaumann et al., Paleoceanography, in prep.

(2)

winter

JJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJ EEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEEE

16 20 24

0 100 200 300 400

Depth (cm)

summer

DDDDDD

D DD

D DDDDD

DD D

D DDD

D DD

D D

DDDDD DD

D D

DDDDDDDDD D DD

DDDDD DDDD

F F

F F F

FF F

F F FF

F F

F FFFF

FF F

F F

F

FF F

F

F F

FF F

FF F

FF FFF

F F

F F F

F

F F

F F

F

6 5 4 3 2

0 -1 -2 -3

δ

1 8

O

C. wuellerstorfi EPILOG

GLAMAP

16017-2

( ‰) δ

1 8

O

( ‰)

G. ruber

° C

Referenzen

ÄHNLICHE DOKUMENTE

The lower part of this core (3–9 m) is dominated by representatives of the hygrophilous chrysomelid families, Plateumaris spp., and Donacia spp., impying a mixture of

The same vegetation pattern was observed at Serra do Tabuleiro and Rincão das Cabritas (Jeske- Pieruschka and Behling 2011; Jeske-Pieruschka et al. 2012) once graminoids dominated

Although fluvial activity through Late Pleistocene time is seen in seismic data of the exposed Laptev shelf (Kleiber and Niessen, 1999), IC deposition in the area of

This change and an episodic pattern of enhanced ice- rafted debris deposition during times of deglaciation provide evidence for a dynamic and likely wet-based late Miocene

Pedicythere neofluitans (Figure 6) characterizes Upper Arctic Ocean deep water but is not a major component of lower AODW or CBDW. The occurrence of these species in

(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.. •

This paper presents the obtaincd rccorcls of 29 current rneters and 5 thcrmistor cables in thc form of time series, amplitudc spcctra, and progressive ycctor