中山大学生物学系
纸质出版日期:1986,
网络出版日期:1986-5-25,
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大陆漂移与有花植物区系的发展[J]. 中山大学学报(自然科学版)(中英文), 1986,25(3):4-14.
The Continental Drift and the Development of the Flowering Plants[J]. Acta Scientiarum Naturalium Universitatis SunYatseni, 1986,25(3):4-14.
本文依据大陆漂移的理论
探讨了华夏、澳洲、南美、非洲、北美、热带亚洲及印度等古陆和陆块
在中生代各个时期的古气候和地质变迁的生态环境.同时
分别讨论了各个古陆和陆块的有花植物区系的特点
着重分析了它们的植物区系的总量
组成分子
具有哪些邃古性的成分
有多少木兰目、番荔支目、毛茛目、金缕梅目及葇荑花序类的代表.然后分别讨论了各个古陆或陆块与华夏植物区系的关系.以澳洲为例
它和南极古陆在晚侏罗纪即已脱离了贡瓦纳古陆的主体
竟拥有40%的有花植物属是和华夏植物区系共有的.依次的亲缘关系为印度、热带亚洲、北美、南美及非洲古陆
它们都与华夏植物区系具有很多共有的属.从而推论有花植物是在中生代初期的三迭纪或侏罗纪
就已经在统一的联合古陆(Pangaea)存在着.文章列举了化石及现代植物作为佐证.随着大陆飘移
统一发生的有花植物在各古陆继续发展下去.文章最后提到华夏古陆具有最多而且最古老的有花植物
它们只能是当地起源的.而其他各个古陆或陆块在整个中生代分别处于冰川、海侵及干旱的条件
很难成为原始有花植物的发源地
只有华夏古陆在古生代末期及整个中古代都处于较稳定的状态
在这里有可能是原始的种子植物及有花植物起源的摇篮
According to the continental drift theory
the ancient ecology of the climateand geological vicissitude of the Cathaysian
Australian
South American
Afri-can
North American
Tropical Asian and Indian ancient lands or landmassesthroughout the Mesozoic Period are discussed.Subsequently
the characteristicsof the flowering floras of the ancient lands are analysed
the principal questionsunder discussion is concerning with the total amount
the composition and theantiquitic taxa
such as Magnoliales
Annonales
Ranunculales
Hamamelidales andthe orders of Amentiflorae
etc.And then
the discussed question falls on therelationship between the floras of the ancient lands and the Cathaysian flora.An interest and valuable existing State of affair has shown
that although theAustralian and the Antarctic landmasses was broke away from the mainland ofGongwana at the late Jurassic
but more than 40% of genera (998) are coexistingin Cathaysia and Australia; and in the proper order
a large amount of generaare found between the Cathaysia and India、Tropical Asia、north America、south America and Africa also.Thus it can be seen that the flowering plantswould be originate at the dawn of Triassic or Mesozoic
in other word
it wasoriginated before the breakdown of the unionized Pangaea
Such assessment isproved by the (?)ossils and the survived flowering plants.Following the driftinglandmasses
the flowering plants of all the continents are developed continuously along with the new environment.Lastly
a suggestion is given
that the Cathaysian flora is originated locally
since there are numerous primary taxa survived here which are not found fromother continents
and all the remaining landmasses either covered by the gra-cial or by the sea transgression
or by the droughty climate throughout theMesozoic Period
it is imposible to nurse the flowering plants
only the stabilized Cathaysia will become the cradle of the primary spermatophytes as well asof the flowering plants.
&nbsp植物区系澳洲有花植物北美第三纪热带亚洲植物群生物区系华夏植物区热带成分地球动力学大陆漂移
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