µÚÈý²¿·Ö£º¸ÅÀ¨´óÒâÓëÍê³É¾ä×Ó £¨Ã¿Ìâ1·Ö£¬¹²8·Ö£¬¡¡½¨Ò飱£°·ÖÖÓÒÔÄÚÍê³É£©
ÔĶÁÏÂÃæÕâÆª¶ÌÎÄ£¬¶ÌÎĺóÓÐ2Ïî²âÊÔÈÎÎñ£º£¨1£©1---4 ÌâÒªÇó´ÓËù¸øµÄ6¸öÑ¡ÏîÖÐΪµÚ2--5 ¶Îÿ¶ÎÑ¡Ôñ1¸öÕýÈ·µÄС±êÌ⣻£¨2£©µÚ5--8ÌâÒªÇó´ÓËù¸øµÄ6¸öÑ¡ÏîÖÐÑ¡Ôñ4¸öÕýÈ·µÄÑ¡Ï·Ö±ðÍê³Éÿ¸ö¾ä×Ó¡£Ç뽫´ð°¸Í¿ÔÚ´ðÌ⿨ÏàÓ¦µÄλÖÃÉÏ¡£
ÄѶȣ£¯A¼¶
Blasts from the past
1 Volcanoes were more destructive in ancient history£®Not because they were bigger,¡¡but¡¡because the carbon dioxide they released wiped out 1ife with greater ease£®
2 Paul Wignall from the University of Leeds was investigating the link between volcanic
eruptions and mass extinctions£®Not a11 volcanic eruptions killed off large numbers of animals£¬but all the mass extinctions over the past 300 million years coincided with huge formations of volcanic rock£®To his surprise£¬the older the massive volcanic eruptions were£¬the more damage they seemed to do£®
3 Wignall calculated the¡° killing efficiency ¡±for these volcanoes by comparing the
proportion £®ion of life they killed off with the volume of lava that they produced£®He found that size for size£¬older eruptions were at least 1 0 times as effective at wiping out life as their more recent rivals£®
4 The Permian extinction£¬for example£¬which happened 250 million years ago£¬is marked
by floods of volcanic rock in Siberia that cover an area roughly the size of western Europe£®Those volcanoes are thought to have pumped out about 10 gigatonnes of carbon as carbon dioxide£®The global warming that followed wiped out 80 per cent of all marine genera at the time¡£And it took 5 million years for the planet to recover£®
5 Yet 60 million years ago in the late Palaeocene there was another huge amount of
volcanic activity and global warming but}Io mass extinction£®Some animals did disappear but things returned to normal within ten thousands of years£¬¡°The most recent ones hardly have an effect at all¡£¡± Wignall says£®He ignored the extinction which wiped out the dinosaurs at the end of the Cretaceous£¬¡£65 million years ago£¬because many scientists believe it was primarily caused by the impact of an asteroid£® ¡¯
6 Wignall thinks that older volcanoes had more killing power because more recent life
forms were better adapted to dealing with increased levels of C02 £®Ocean chemistry may also have played a role£®As the supercontinents broke up and exposed more coastline there may have been more weathering of silica rocks£®This would have encouraged the growth of phytoplankton in the oceans¡£increasing me amount of C02 absorbed from the atmosphere£®
7 Vincent Courtillot director of the Paris Geophysical Institute in France£¬says that
Wignall¡¯s idea is provocative£®But he says it is incredibly hard to do these sorts of calculations£®He points out that the killing power of volcanic eruptions depends on how long they lasted£®And it is impossible to tell whether the huge blasts lasted for thousands or millions of years¡£
8 Courtillot also adds t11at it is difficult to estimate how much 1ava prehistoric volcanoes produced , and that 1ava volume may not necessarily correspond to carbon dioxide or sulphur dioxide emissions£®