Recognition of abrupt climate changes in clastic sedimentary environments: An introduction

Global and Planetary Change

Volumn 28, Issue 1-2, 2001, Pages

  Fard, A M ^a  

^a STOCKHOLM UNIVERSITY   (Sweden)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0035098410     PISSN: 09218181     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0921-8181(00)00059-X     Document Type: Editorial

References (14)

1. Sudden climate transition during the Quaternary
2. Methods, potential, and limitations for tracing abrupt climate change in clastic environments
3. An event stratigraphy for the last termination in the North Atlantic region based on the Greenland ice-core record: A proposal by the INTIMATE group
4. Synchronized terrestrial atmospheric deglacial records around the North Atlantic
5. A pervasive millenial-scale cycle in North Atlantic Holocene and Glacial climates
6. Late Holocene ∼ 1500 yr periodicities and their implications
7. Rapid climatic variability of the North Atlantic Ocean and global climate: A focus of the IMAGES program
8. Continental biogenic species in Greenland Ice Core Project core: Tracing back the biomass history of the North American continent
9. A calendar age estimate of the Younger Dryas - Holocene boundary at Kråkenes, western Norway
10. A 110,000 year history of change in continental biogenic emissions and related atmospheric circulation inferred from the Greenland Ice Sheet Project Ice Core
11. Rapid deglaciation and ice sheet retreat in the Stockholm area
12. Past and future recognitions in the climate system
13. The "flickering switch" of late Pleistocene climate change
14. The Holocene - Younger Dryas transition recorded at Summit, Greenland