Integration of ice-core, marine and terrestrial records for the Australian Last Glacial Maximum and Termination: a contribution from the OZ INTIMATE group

Simple item page
dc.contributor.authorTurney, CSMen_AU
dc.contributor.authorHaberle, SGen_AU
dc.contributor.authorFink, Den_AU
dc.contributor.authorKershaw, APen_AU
dc.contributor.authorBarbetti, Men_AU
dc.contributor.authorBarrows, TTen_AU
dc.contributor.authorBlack, Men_AU
dc.contributor.authorCohen, TJen_AU
dc.contributor.authorCorrège, Ten_AU
dc.contributor.authorHesse, PPen_AU
dc.contributor.authorHua, Qen_AU
dc.contributor.authorJohnston, Ren_AU
dc.contributor.authorMorgan, VIen_AU
dc.contributor.authorMoss, PTen_AU
dc.contributor.authorNanson, GCen_AU
dc.contributor.authorvan Ommen, TDen_AU
dc.contributor.authorRule, Sen_AU
dc.contributor.authorWilliams, NJen_AU
dc.contributor.authorZhao, JXen_AU
dc.contributor.authorD'Costa, Den_AU
dc.contributor.authorFeng, YXen_AU
dc.contributor.authorGagan, MKen_AU
dc.contributor.authorMooney, SDen_AU
dc.contributor.authorXia, Qen_AU
dc.date.accessioned2021-12-16T02:24:02Zen_AU
dc.date.available2021-12-16T02:24:02Zen_AU
dc.date.issued2006-10en_AU
dc.date.statistics2021-11-09en_AU
dc.descriptionSpecial Issue: Integrating High‐Resolution Past Climate Records for Future Prediction in the Australasian Regionen_AU
dc.description.abstractThe 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 conflicting evidence for the degree of hemispheric ‘teleconnection’ and an unresolved debate as to the principle forcing mechanism(s). The available hypotheses are difficult to test robustly, however, because the few detailed palaeoclimatic records in the Southern Hemisphere are widely dispersed and lack duplication. Here we present climatic and environmental reconstructions from across Australia, a key region of the Southern Hemisphere because of the range of environments it covers and the potentially important role regional atmospheric and oceanic controls play in global climate change. We identify a general scheme of events for the end of the last glacial period and early Holocene but a detailed reconstruction proved problematic. Significant progress in climate quantification and geochronological control is now urgently required to robustly investigate change through this period. © 2006 John Wiley & Sons, Ltd.en_AU
dc.identifier.citationTurney, C. S. M., Haberle, S., Fink, D., Kershaw, A. P., Barbetti, M., Barrows, T. T., Black, M., Cohen, T. J., Corrège, T., Hesse, P. P., Hua, Q., Johnston, R., Morgan, V., Moss, P., Nanson, G., van Ommen, T., Rule, S., Williams, N. J., Zhao, J.-X. D'Costa, D., Feng, Y.-X., Gagan, M., Mooney, S., & Xia, Q. (2006). Integration of ice-core, marine and terrestrial records for the Australian Last Glacial Maximum and Termination: a contribution from the OZ INTIMATE group. Journal of Quaternary Science, 21(7), 751-761. doi:10.1002/jqs.1073en_AU
dc.identifier.issn1099-1417en_AU
dc.identifier.issue7en_AU
dc.identifier.journaltitleJournal of Quaternary Scienceen_AU
dc.identifier.pagination751-761en_AU
dc.identifier.urihttps://doi.org/10.1002/jqs.1073en_AU
dc.identifier.urihttps://apo.ansto.gov.au/dspace/handle/10238/12481en_AU
dc.identifier.volume21en_AU
dc.language.isoenen_AU
dc.publisherWileyen_AU
dc.subjectCarbon 14en_AU
dc.subjectAccuracyen_AU
dc.subjectGlaciersen_AU
dc.subjectGeomorphologyen_AU
dc.subjectIceen_AU
dc.subjectSouthern Hemisphereen_AU
dc.subjectClimatic changeen_AU
dc.subjectQuaternary perioden_AU
dc.titleIntegration of ice-core, marine and terrestrial records for the Australian Last Glacial Maximum and Termination: a contribution from the OZ INTIMATE groupen_AU
dc.typeJournal Articleen_AU
Files
License bundle
Now showing 1 - 1 of 1
Thumbnail Image
Name:
license.txt
Size:
1.63 KB
Format:
Item-specific license agreed upon to submission
Description:
Download
Collections
Journal Articles