Hostname: page-component-78c5997874-lj6df Total loading time: 0 Render date: 2024-11-07T23:29:15.107Z Has data issue: false hasContentIssue false
  • English
  • Français

Manop Site C

Published online by Cambridge University Press:  18 July 2016

Rights & Permissions [Opens in a new window]

Extract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

This project was initiated by Alan Mix working in cooperation with Jack Dymond. It involves measurements of one size fractions and hand-picked foraminifera shells from material caught in sediment traps deployed in the equatorial Pacific Ocean (see Tables 14, 15).

Type
Accelerator Mass Spectrometry Radiocarbon Measurements on Marine Carbonate Samples from Deep Sea Cores and Sediment Traps
Information
Radiocarbon , Volume 30 , Issue 3 , 1988 , pp. 293 - 295
Copyright
Copyright © The American Journal of Science

References

References Cited in Tables

1.Andrée, M, Beer, J, Oeschger, H, Bonani, G, Hofmann, J H, Morenzoni, E, Nessi, M, Suter, M and Wolfli, W, 1984, Target preparation for milligram sized 14C samples and data evaluation for AMS measurements: Nuclear Instruments & Methods, v B5, p 274–279.Google Scholar
2.Suter, M, Balzer, R, Bonani, G, Hofmann, H J, Morenzoni, E, Nessi, M, Wolfli, W, Andrée, M, Beer, J and Oeschger, H, 1984, Precision measurements of 14C in AMS—some results and prospects. Nuclear Instruments & Methods, v B5, p 117–122.Google Scholar
3.Broecker, W S, Mix, A, Andrée, M and Oeschger, H, 1984, Radiocarbon measurements on coexisting benthic and planktonic foraminifera shells: Potential for reconstructing ocean ventilation times over the past 20,000 years: Nuclear Instruments & Methods, v B5, p 331–339.Google Scholar
4.Andrée, M, Beer, J, Oeschger, H, Broecker, W S, Mix, A, Ragano, N, O'Hara, P, Bonani, G, Hofmann, H J, Morenzoni, E, Nessi, M, Suter, M and Wolfli, W, 1984, 14C measurements on foraminifera of deep sea core V28–238 and their preliminary interpretation-Nuclear Instruments & Methods, v B5, p 340–345.Google Scholar
5.Peng, T-H and Broecker, W S, 1984, The impacts of bioturbation on the age difference between benthic and planktonic foraminifera in deep sea sediments: Nuclear Instruments & Methods, v B5, p 346–352.Google Scholar
6.Andrée, M, Beer, J, Oeschger, H, Mix, A, Broecker, W S, Ragano, N, O'Hara, P, Bonani, G, Hofmann, H J, Morenzoni, E, Nessi, M, Suter, M and Wolfli, W, 1985, Accelerator radiocarbon ages on foraminifera separated from deep-sea sediments. Reprinted from, The carbon cycle and atmospheric CO2: Natural variations Achean to present: Geophys Mono 32, Am Geophys Union.Google Scholar
7.Andrée, M, Oeschger, H, Broecker, W S, Beavan, N, Mix, A, Bonani, G, Hofmann, H J, Morenzoni, E, Nessi, M, Suter, M and Wolfli, W, 1986, AMS radiocarbon dates on foraminifera from deep sea sediments, in Stuiver, M, and Kra, R S, eds, Internal 14C conf, 12th, Proc: Radiocarbon, v 28, no. 2A, p 424–428.Google Scholar
8.Clark, D L, Andrée, M, Broecker, W S, Mix, A, Bonani, G, Hofmann, H J, Morenzoni, E, Nessi, M, Suter, M and Wolfli, W, 1986, Arctic Ocean chronology confirmed by accelerator 14C dating: Geophys Research Letters 13, no. 4 p 319–321.Google Scholar
9.Andrée, M, Oeschger, H, Broecker, W S, Beavan, N, Klas, M, Mix, A, Bonani, G, Hofmann, H J, Suter, M, Wolfli, W and Peng, T-H, 1986, Limits on the ventilation rate for the deep ocean over the last 12,000 years: Climate Dynamics, v 1, p 53–62.Google Scholar
10.Broecker, W S, 1986, Paleocean circulation rates as determined from accelerator radiocarbon measurements on hand-picked foraminifera: Internatl conf, 6th, Geochronology, cosmochronology and isotope geology, Cambridge, England, abs.Google Scholar
11.Andrée, M, 1987, The impact of bioturbation on AMS 14C dates on hand-picked foraminifera: A statistical model: Radiocarbon, v 29, no 2 p 169–175.Google Scholar
12.Broecker, W S, Andrée, M, Wolfli, W, Oeschger, H, Bonani, G, Kennett, J and Peteet, D, in press, The chronology of the last deglaciation: Implications to the cause of the Younger Dryas event: Paleoceanography.Google Scholar
13.Broecker, W S, Andrée, M, Bonani, G, Wolfli, W, Oeschger, H and Klas, M, in press, Can the Greenland climate jumps be identified in records from ocean and land?: Quaternary Research.Google Scholar
14.Broecker, W S, Andrée, M, Klas, M, Bonani, G, Wolfli, W and Oeschger, H, in press New evidence from the South China Sea for an abrupt termination of the last glacial period about 13,100 years ago: Nature.Google Scholar
15.Broecker, W S, Andrée, M, Bonani, G, Mix, A, Klas, M, Wolfli, W and Oeschger, H, ms in preparation, Differences between the radiocarbon ages of coexisting planktonic foraminifera.Google Scholar
16.Broecker, W S, Andrée, M, Bonani, G, Wolfli, W, Oeschger, H, Klas, M, Mix, A and Curry, W, ms in preparation, The radiocarbon age of deep water in the glacial ocean.Google Scholar
17.Broecker, W S, Oppo, D, Curry, W, Andrée, M, Wolfli, W and Bonani, G, ms in preparation, Radiocarbon based chronology for the 18O/16O record for the last deglaciation.Google Scholar
18.Broecker, W S, 1987, The biggest chill: Natural History, v 96, no 10 p 74–75.Google Scholar