Atmospheric radiocarbon during the Younger Dryas: Production, ventilation, or both?

Earth and Planetary Science Letters

Volumn 185, Issue 3-4, 2001, Pages 383-395

  Marchal, Olivier ^a   Stocker, Thomas F ^a   Muscheler, Raimund ^b  

^a UNIVERSITY OF BERN   (Switzerland)

^b SWISS FEDERAL INSTITUTE OF AQUATIC SCIENCE AND TECHNOLOGY   (Switzerland)

Author keywords

C 14 C 13; Paleoatmosphere; Younger Dryas

Indexed keywords

CARBON ISOTOPE; PALEOATMOSPHERE; THERMOHALINE CIRCULATION; VENTILATION; YOUNGER DRYAS;

EID: 0035101036     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(00)00383-6     Document Type: Article

References (50)

1. Irregular interstadials recorded in a new Greenland ice core
2. 18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability
3. Coupled ocean-atmosphere model response to freshwater input: Comparison to Younger Dryas event
4. The stability of the North Atlantic thermohaline circulation in a coupled ocean-atmosphere general circulation model
5. 2 emission rates on the stability of the thermohaline circulation
6. Does the ocean-atmosphere system have more than one stable mode of operation?
7. Younger Dryas experiments
8. Rapid changes in ocean circulation and atmospheric radiocarbon
9. Temporal-geographical melt-water influences on the North Atlantic conveyor: Implications for the Younger Dryas
10. 2 during the Younger Dryas climate event
11. Simulation of particle fluxes and cosmogenic nuclide production in the Earth's atmosphere
12. Tracers in the Sea, Eldigio Press
13. The global beryllium-10 cycle
14. 14C records
15. 14C during the Younger Dryas cold episode
16. Synchronized terrestrial-atmospheric deglacial records around the North Atlantic
17. Deglacial changes in ocean circulation from an extended radiocarbon calibration
18. 14C over the Allerød-Younger Dryas transition
19. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event
20. 230Th ages of corals
21. Geochemical and geophysical implications of the radiocarbon calibration
22. Variations of Younger Dryas atmospheric radiocarbon explicable without ocean circulation changes
23. Paleointensity of the geomagnetic field during the last 80 000 years
24. Theoretically expected variations in the terrestrial cosmic-ray production rates of isotopes
25. Physical and biogeochemical responses to freshwater-induced thermohaline variability in a zonally averaged ocean model
26. Beryllium-10 concentrations in the Greenland Ice Sheet Project 2 ice core from 3-40 ka
27. Greenland palaeotemperatures derived from GRIP bore hole temperature and ice core isotope profiles
28. Changes in continental and sea-salt atmospheric loadings in central Greenland during the most recent deglaciation: Model-based estimates
29. Chlorine-36 evidence for the Mono Lake event in the Summit GRIP ice core
30. Dominant influence of atmospheric circulation on snow accumulation in Greenland over the last 18 000 years
31. Numerical Recipes (in Fortran)
32. Abrupt climate change at the end of the last glacial period inferred from trapped air in polar ice
33. 18O in the oceans
34. Paleocean circulation during the last deglaciation: A bipolar seesaw
35. Relative variations in geomagnetic intensity from sedimentary records: The past 200 000 years
36. 10Be in globally stacked deep-sea sediments
37. Late Pleistocene geomagnetic excursion in Iceland lavas: Confirmation of the Laschamp excursion
38. Comparison of cosmogenic radionuclide production and geomagnetic field intensity over the last 200 000 years
39. The origin of Arctic precipitation under present and glacial conditions
40. Glacial-interglacial changes in moisture sources for Greenland: Influences on the ice core record of climate
41. 36Cl flux in the GRIP ice core, Greenland
42. Lateral mixing and advection of reactive isotope tracers in ocean basins: Observations and mechanisms
43. 10Be-derived geomagnetic paleointensity data
44. 14C gradient during the Younger Dryas climatic event
45. 14C
46. Variability in radiocarbon ages of individual organic compounds from marine sediments
47. 14C calibration 9200-11 855 cal. BP
48. 14C data