Geomagnetic paleointensity and environmental record from Labrador Sea core MD95-2024: Global marine sediment and ice core chronostratigraphy for the last 110 kyr

Earth and Planetary Science Letters

Volumn 183, Issue 1-2, 2000, Pages 161-177

  Stoner, J S ^a   Channell, J E T ^b   Hillaire Marcel, C ^c   Kissel, C ^d  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b UNIVERSITY OF FLORIDA   (United States)

^c UNIVERSITÉ DU QUÉBEC À MONTRÉAL   (Canada)

^d LABORATOIRE DES SCIENCES DU CLIMAT ET DE L ENVIRONNEMENT   (France)

Author keywords

Chronostratigraphy; Climate change; Holocene; Ice cores; Labrador Sea; Magnetic intensity; Paleomagnetism

Indexed keywords

CHRONOSTRATIGRAPHY; ICE CORE; MAGNETIC INTENSITY; MARINE SEDIMENT; PALEOMAGNETISM;

LABRADOR SEA;

EID: 0034527927     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(00)00272-7     Document Type: Article

References (50)

1. North Atlantic paleointensity stack since 75 ka (NAPIS-75) and the duration of the Laschamp event
2. Rapid climatic variations during marine isotope stage 3: Magnetic analysis of sediments from Nordic Seas and North Atlantic
3. Late Pleistocene relative geomagnetic paleointensity from the deep Labrador Sea: Regional and global correlations
4. A 200 kyr geomagnetic stratigraphy for the Labrador Sea: Indirect correlation of the sediment record to SPECMAP
5. Relative paleointensity and δ18O at ODP Site 983, since 350 ka
6. Paleointensity of the geomagnetic field during the last 80 000 years
7. Relative geomagnetic intensity of the field during the last 140 ka
8. Geomagnetic paleointensity from late Brunhes-age piston cores from the subantarctic South Atlantic
9. Relative variations in geomagnetic intensity from sedimentary records: The past 200 000 years
10. The magnetic signature of rapidly deposited detrital layers from the deep Labrador Sea: Relationship to North Atlantic Heinrich layers
11. Isotope stratigraphy, sedimentation rates, deep circulation and carbonate events in the Labrador Sea during the last ~ 200 ka
12. Instabilities in the Labrador Sea water mass structure during the last climatic cycle
13. Improvements in long core measurement techniques: Applications in palaeomagnetism and palaeoceanography
14. The least squares lines and plane analysis of paleomagnetic data
15. On the possibility of obtaining relative paleointensities from lake sediments
16. A new rock magnetic approach to selecting sediments for geomagnetic intensity studies: Application to paleointensity for the last 4000 years
17. Sedimentary records of relative paleointensity of the geomagnetic field: Theory and practice
18. Hysteresis properties of titanomagnetites: Grain-size and compositional dependence
19. Evidence for general instability of past climate from a 250-kyr ice-core record
20. 5-year time resolution
21. Correlations between climate records from North Atlantic sediments and Greenland ice
22. High-resolution climate records from the North Atlantic during the last interglacial
23. Volcanic aerosol records and tephrochronology of the Summit, Greenland, ice cores
24. 36Cl flux in the GRIP ice core, Greenland
25. Beryllium 10 concentrations in the Greenland Ice Sheet Project 2 ice core from 3-40 ka
26. A geomagnetic chronology for antarctic ice accumulation
27. Chlorine-36 evidence for the Mono Lake event in the Summit GRIP ice core
28. 14C calibration beyond 25 ka BP
29. Rapid changes in surface and deep water conditions at the Faeroe margin during the last 58 000 years
30. 10Be deposition in Antarctic ice during the last glacial period
31. Preliminary depth-age scale for the GISP2 ice core
32. Climate correlations between Greenland and Antarctica during the past 100 000 years
33. Asynchrony of Antarctic and Greenland climate change during the last glacial period
34. Greenland palaeotemperatures derived from GRIP bore hole temperature and ice core isotope profiles
35. High precision correlations of Greenland and Antarctic ice core records over the last 100 kyr
36. Climate and atmospheric history of the past 420 000 years from the Vostok ice core, Antarctica
37. 2 climate relationship as deduced from the Vostok ice core: A re-examination based on new measurements and on a re-evaluation of the air dating
38. Age dating and the orbital theory of the Ice Ages: Development of a high-resolution 0 to 300 000-year chronostratigraphy
39. 2 and ice volume changes during the penultimate deglaciation
40. A 135 000-year Vostok-SPECMAP common temporal framework
41. High-resolution stable isotope stratigraphy from bulk sediment
42. Origin of global millennial scale climate events: Constraints from the Southern Ocean deep sea sedimentary record
43. Tyrrhenian sea tephrochronology of the oxygen isotope records for the past 60 000 years
44. Climate connections between the hemispheres revealed by deep sea sediment core/ice core correlations
45. Trade wind forcing of upwelling seasonality and Heinrich events as a response to sub-Milankovitch climate variability
46. Link between the North and South Atlantic during the Heinrich events of the last glacial period
47. The stability of the North Atlantic thermohaline circulation in a coupled ocean-atmosphere general circulation model
48. The North Atlantic's 1-2 kyr climate rhythm: Relation to Heinrich events, Dansgaard/Oeschger cycles and the little Ice Age
49. Vostok ice core a continuous isotope temperature record over the last climatic cycle (160 000 years)
50. Macintosh program performs time-series analysis