Integration of ice-core, marine and terrestrial records for the Australian Last Glacial Maximum and Termination: a contribution from the OZ INTIMATE group
The degree to which Southern Hemisphere climatic changes during the end of the last glacial period and early Holocene (30-8 ka) were influenced or initiated by events occurring in the high latitudes of the Northern Hemisphere is a complex issue. There is
Published in: | Journal of Quaternary Science |
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Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Wiley-VCH Verlag GMBH
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/22128 https://doi.org/10.1002/jqs.1073 https://openresearch-repository.anu.edu.au/bitstream/1885/22128/5/Turney%25282006%2529.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/22128/7/01_Turney_Integration_of_ice-core%2c_2006.pdf.jpg |
Summary: | The degree to which Southern Hemisphere climatic changes during the end of the last glacial period and early Holocene (30-8 ka) were influenced or initiated by events occurring in the high latitudes of the Northern Hemisphere is a complex issue. There is |
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