Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/1316
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dc.contributor.authorPower, MJen_AU
dc.contributor.authorMarlon, Jen_AU
dc.contributor.authorOrtiz, Nen_AU
dc.contributor.authorBartlein, PJen_AU
dc.contributor.authorHarrison, SPen_AU
dc.contributor.authorMayle, FEen_AU
dc.contributor.authorBallouche, Aen_AU
dc.contributor.authorBradshaw, RHWen_AU
dc.contributor.authorCarcaillet, Cen_AU
dc.contributor.authorCordova, Cen_AU
dc.contributor.authorMooney, SDen_AU
dc.contributor.authorMoreno, PIen_AU
dc.contributor.authorPrentice, ICen_AU
dc.contributor.authorThonicke, Ken_AU
dc.contributor.authorTinner, Wen_AU
dc.contributor.authorWhitlock, Cen_AU
dc.contributor.authorZhang, Yen_AU
dc.contributor.authorZhao, Yen_AU
dc.contributor.authorAli, AAen_AU
dc.contributor.authorAnderson, RSen_AU
dc.contributor.authorBeer, Ren_AU
dc.contributor.authorBehling, Hen_AU
dc.contributor.authorBriles, Cen_AU
dc.contributor.authorBrown, KJen_AU
dc.contributor.authorBrunelle, Aen_AU
dc.contributor.authorBush, Men_AU
dc.contributor.authorCamill, Pen_AU
dc.contributor.authorChu, GQen_AU
dc.contributor.authorClark, Jen_AU
dc.contributor.authorColombaroli, Den_AU
dc.contributor.authorConnor, Sen_AU
dc.contributor.authorDaniau, ALen_AU
dc.contributor.authorDaniels, Men_AU
dc.contributor.authorDodson, JRen_AU
dc.contributor.authorDoughty, Een_AU
dc.contributor.authorEdwards, MEen_AU
dc.contributor.authorFinsinger, Wen_AU
dc.contributor.authorFoster, Den_AU
dc.contributor.authorFrechette, Jen_AU
dc.contributor.authorGaillard, MJen_AU
dc.contributor.authorGavin, DGen_AU
dc.contributor.authorGobet, Een_AU
dc.contributor.authorHaberle, Sen_AU
dc.contributor.authorHallett, DJen_AU
dc.contributor.authorHiguera, Pen_AU
dc.contributor.authorHope, Gen_AU
dc.contributor.authorHorn, Sen_AU
dc.contributor.authorInoue, Jen_AU
dc.contributor.authorKaltenrieder, Pen_AU
dc.contributor.authorKennedy, Len_AU
dc.contributor.authorKong, ZCen_AU
dc.contributor.authorLarsen, Cen_AU
dc.contributor.authorLong, CJen_AU
dc.contributor.authorLynch, Jen_AU
dc.contributor.authorLynch, EAen_AU
dc.contributor.authorMcGlone, Men_AU
dc.contributor.authorMeeks, Sen_AU
dc.contributor.authorMensing, Sen_AU
dc.contributor.authorMeyer, Gen_AU
dc.contributor.authorMinckley, Ten_AU
dc.contributor.authorMohr, Jen_AU
dc.contributor.authorNelson, DMen_AU
dc.contributor.authorNew, Jen_AU
dc.contributor.authorNewnham, Ren_AU
dc.contributor.authorNoti, Ren_AU
dc.contributor.authorOswald, Wen_AU
dc.contributor.authorPierce, Jen_AU
dc.contributor.authorRichard, PJHen_AU
dc.contributor.authorRowe, Cen_AU
dc.contributor.authorGoni, MFSen_AU
dc.contributor.authorShuman, BNen_AU
dc.contributor.authorTakahara, Hen_AU
dc.contributor.authorToney, Jen_AU
dc.contributor.authorTurney, CSMen_AU
dc.contributor.authorUrrego-Sanchez, DHen_AU
dc.contributor.authorUmbanhowar, Cen_AU
dc.contributor.authorVandergoes, Men_AU
dc.contributor.authorVanniere, Ben_AU
dc.contributor.authorVescovi, Een_AU
dc.contributor.authorWalsh, Men_AU
dc.contributor.authorWang, XDen_AU
dc.contributor.authorWilliams, Nen_AU
dc.contributor.authorWilmshurst, Jen_AU
dc.contributor.authorZhang, JHen_AU
dc.date.accessioned2009-06-09T06:20:42Zen_AU
dc.date.accessioned2010-04-30T05:02:09Z-
dc.date.available2009-06-09T06:20:42Zen_AU
dc.date.available2010-04-30T05:02:09Z-
dc.date.issued2007-12-14en_AU
dc.identifier.citationPower, M. J., Marlon, J., Ortiz, N., Bartlein, P. J., Harrison, S. P., Mayle, F. E., Ballouche, A. Bradshaw, R. H. W., Carcaillet, C., Cordova, C., Mooney, S., Moreno, P. I., Prentice, I. C., Thonicke, K. , Tinner, W., Whitlock, C., Zhang, Y., Zhao, Y., Ali, A. A., Anderson, R. S., Beer, R., Behling, H., Briles, C., Brown, K. J., Brunelle, A., Bush, M., Camill, P., Chu, GQ., Clark, J; Colombaroli, D; Connor, S; Daniau, A. L., Daniels, M., Dodson, J. R., Doughty, E., Edwards, M. E., Finsinger, W., Foster, D., Frechette, J., Gaillard, M. J., Gavin, D. G., Gobet, E., Haberle, S., Hallett, D. J., Higuera, P., Hope, G., Horn, S., Inoue, J.,Kaltenrieder, P., Kennedy, L., Kong, Z. C., Larsen, C., Long, C. J., Lynch, J., Lynch, E. A., McGlone, M., Meeks, S., Mensing, S., Meyer, G., Minckley, T., Mohr, J., Nelson, D. M., New, J., Newnham, R., Noti, R., Oswald, W., Pierce, J., Richard, P. J. H., Rowe, C., Goni, M. F. S., Shuman, B. N., Takahara, H., Toney, J., Turney, C., Urrego-Sanchez, D. H., Umbanhowar, C., Vandergoes, M., Vanniere, B., Vescovi, E., Walsh, M., Wang, X. D., Williams, N., Wilmshurst, J., & Zhang, J. H. (2008). Changes in fire regimes since the last glacial maximum: an assessment based on a global synthesis and analysis of charcoal data. Climate Dynamics, 30(7-8), 887-907. doi:10.1007/s00382-007-0334-xen_AU
dc.identifier.govdoc1132-
dc.identifier.issn0930-7575en_AU
dc.identifier.urihttp://dx.doi.org/10.1007/s00382-007-0334-xen_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/1316en_AU
dc.description.abstractFire activity has varied globally and continuously since the last glacial maximum (LGM) in response to long-term changes in global climate and shorter-term regional changes in climate, vegetation, and human land use. We have synthesized sedimentary charcoal records of biomass burning since the LGM and present global maps showing changes in fire activity for time slices during the past 21,000 years (as differences in charcoal accumulation values compared to pre-industrial). There is strong broad-scale coherence in fire activity after the LGM, but spatial heterogeneity in the signals increases thereafter. In North America, Europe and southern South America, charcoal records indicate less-than-present fire activity during the deglacial period, from 21,000 to similar to 11,000 cal yr BP. In contrast, the tropical latitudes of South America and Africa show greater-than-present fire activity from similar to 19,000 to similar to 17,000 cal yr BP and most sites from Indochina and Australia show greater-than-present fire activity from 16,000 to similar to 13,000 cal yr BP. Many sites indicate greater-than-present or near-present activity during the Holocene with the exception of eastern North America and eastern Asia from 8,000 to similar to 3,000 cal yr BP, Indonesia and Australia from 11,000 to 4,000 cal yr BP, and southern South America from 6,000 to 3,000 cal yr BP where fire activity was less than present. Regional coherence in the patterns of change in fire activity was evident throughout the post-glacial period. These complex patterns can largely be explained in terms of large-scale climate controls modulated by local changes in vegetation and fuel load. © 2008, Springer.en_AU
dc.language.isoenen_AU
dc.publisherSpringeren_AU
dc.subjectCharcoalen_AU
dc.subjectGlobal analysisen_AU
dc.subjectFiresen_AU
dc.subjectClimatic changeen_AU
dc.subjectLand useen_AU
dc.subjectPlantsen_AU
dc.titleChanges in fire regimes since the last glacial maximum: an assessment based on a global synthesis and analysis of charcoal dataen_AU
dc.typeJournal Articleen_AU
dc.date.statistics2008-06en_AU
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