Environmental mutagenesis during the end-Permian ecological crisis

被引:194
作者
Visscher, H
Looy, CV
Collinson, ME
Brinkhuis, H
Cittert, JHAVKV
Kürschner, WM
Sephton, MA
机构
[1] Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands
[2] Smithsonian Inst, Natl Museum Amer Hist, Dept Paleobiol, Washington, DC 20560 USA
[3] Royal Hollowa Univ London, Dept Geol, Egham TW20 0EX, Surrey, England
[4] Natl Museum Nat Hist, NL-2300 RA Leiden, Netherlands
[5] Open Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, England
关键词
D O I
10.1073/pnas.0404472101
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
During the end-Permian ecological crisis, terrestrial ecosystems experienced preferential dieback of woody vegetation. Across the world, surviving herbaceous lycopsids played a pioneering role in repopulating deforested terrain. We document that the microspores of these lycopsids were regularly released in unseparated tetrads indicative of failure to complete the normal process of spore development. Although involvement of mutation has long been hinted at or proposed in theory, this finding provides concrete evidence for chronic environmental mutagenesis at the time of global ecological crisis. Prolonged exposure to enhanced UV radiation could account satisfactorily for a worldwide increase in land plant mutation. At the end of the Permian, a period of raised UV stress may have been the consequence of severe disruption of the stratospheric ozone balance by excessive emission of hydrothermal organohalogens in the vast area of Siberian Traps volcanism.
引用
收藏
页码:12952 / 12956
页数:5
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