Direct dating of the oxygen-isotope record of the last deglaciation by 14C accelerator mass spectrometry

Nature ◽  
1986 ◽  
Vol 320 (6060) ◽  
pp. 350-352 ◽  
Author(s):  
Jean-Claude Duplessy ◽  
Maurice Arnold ◽  
Pierre Maurice ◽  
Edouard Bard ◽  
Josette Duprat ◽  
...  
Radiocarbon ◽  
2003 ◽  
Vol 45 (3) ◽  
pp. 467-477 ◽  
Author(s):  
Ulrich von Rad ◽  
Michael Sarnthein ◽  
Pieter M Grootes ◽  
Heidi Doose-Rolinski ◽  
Jochen Erbacher

In a core off Pakistan, we obtained 38 14C analyses by accelerator mass spectrometry (AMS) from a 4.4-m-thick, expanded, annually-laminated Last Glacial Maximum (LGM) section, bracketed by bioturbated intervals ascribed to the Heinrich-1 (H1) and Heinrich-2 (H2) equivalent events (52 14C analyses between 24–15 kyr BP). A floating varve age scale, anchored to the oxygen isotope record of the layer-counted GISP2 ice core at the H2/LGM boundary, results in an annually dated record for the LGM from 23,450–17,900 cal BP. The floating varve scale of the LGM provides us with a tentative calibration of local marine AMS 14C age dates to calendar years.


1989 ◽  
Vol 31 (3) ◽  
pp. 381-391 ◽  
Author(s):  
Edouard Bard ◽  
Richard Fairbanks ◽  
Maurice Arnold ◽  
Pierre Maurice ◽  
Josette Duprat ◽  
...  

AbstractCoupled measurements of δ18O and accelerator mass spectrometry (AMS) 14C in a particular species of planktonic foraminifera may be used to calculate sea-level estimates for the last deglaciation. Of critical importance for this type of study is a knowledge of the seasonality of foraminiferal growth, which can be provided by δ18O measurements of modern shells (core tops, plankton tows). Isotopic (δ18O, AMS-14C dating) and faunal records (transfer function sea surface temperature) were obtained from two cores in the North Atlantic at about 37°N. The locations were chosen to obtain high sedimentation rate records removed from the major ice-melt discharge areas of the last deglaciation. Based upon Globigerina bulloides data, four δ18O-based sea-level estimates were calculated: −67 ± 7 m at 12,200 yr B.P. and −24 ± 8 m at about 8200 yr B.P. for core SU 81-18; −83 ± 10 m at 12,200 yr B.P. and −13 ± 11 m at about 8500 yr B.P. for core SU 81-14. Using a second working hypothesis concerning the seasonability of G. bulloides growth, it is suggested that the sea-level rose by about 40 m during the millennium which followed 14,500 yr B.P.


Nature ◽  
1987 ◽  
Vol 328 (6133) ◽  
pp. 791-794 ◽  
Author(s):  
Edouard Bard ◽  
Maurice Arnold ◽  
Pierre Maurice ◽  
Josette Duprat ◽  
Jean Moyes ◽  
...  

2016 ◽  
Vol 175 ◽  
pp. 239-251 ◽  
Author(s):  
Stefan Markovic ◽  
Adina Paytan ◽  
Hong Li ◽  
Ulrich G. Wortmann

1998 ◽  
Vol 33 (3-4) ◽  
pp. 223-240 ◽  
Author(s):  
Stefan Mulitza ◽  
Tobias Wolff ◽  
Jürgen Pätzold ◽  
Walter Hale ◽  
Gerold Wefer

2022 ◽  
Vol 278 ◽  
pp. 107376
Author(s):  
Matthew S. Finkenbinder ◽  
Byron A. Steinman ◽  
Broxton W. Bird ◽  
Ellen C. Heilman ◽  
Alexandria R. Aspey ◽  
...  

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