Flammable biomes dominated by eucalypts originated at the Cretaceous-Palaeogene boundary

被引:197
作者
Crisp, Michael D. [1 ]
Burrows, Geoffrey E. [2 ]
Cook, Lyn G. [3 ]
Thornhill, Andrew H. [1 ]
Bowman, David M. J. S. [4 ]
机构
[1] Australian Natl Univ, Res Sch Biol, Div Evolut Ecol & Genet, Canberra, ACT 0200, Australia
[2] Charles Sturt Univ, Inst Land Water & Soc, Wagga Wagga, NSW 2678, Australia
[3] Univ Queensland, Sch Biol Sci, Brisbane, Qld 4072, Australia
[4] Sch Plant Sci, Hobart, Tas 7001, Australia
基金
澳大利亚研究理事会;
关键词
STRAND STRUCTURE; WOODY-PLANTS; MYRTACEAE; FIRE; PHYLOGENIES; DIVERSITY; EVOLUTION; ECOSYSTEMS; PALEOCENE; AUSTRALIA;
D O I
10.1038/ncomms1191
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Fire is a major modifier of communities, but the evolutionary origins of its prevalent role in shaping current biomes are uncertain. Australia is among the most fire-prone continents, with most of the landmass occupied by the fire-dependent sclerophyll and savanna biomes. In contrast to biomes with similar climates in other continents, Australia has a tree flora dominated by a single genus, Eucalyptus, and related Myrtaceae. A unique mechanism in Myrtaceae for enduring and recovering from fire damage likely resulted in this dominance. Here, we find a conserved phylogenetic relationship between post-fire resprouting (epicormic) anatomy and biome evolution, dating from 60 to 62 M Ma, in the earliest Palaeogene. Thus, fire-dependent communities likely existed 50 million years earlier than previously thought. We predict that epicormic resprouting could make eucalypt forests and woodlands an excellent long-term carbon bank for reducing atmospheric CO2 compared with biomes with similar fire regimes in other continents.
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页数:8
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