首页> 外文学位 >FOSSIL HISTORY OF THE JUGLANDACEAE.
【24h】

FOSSIL HISTORY OF THE JUGLANDACEAE.

机译:G科化石的历史。

获取原文
获取原文并翻译 | 示例

摘要

The Juglandaceae (walnut family) has an excellent fossil record in the Northern Hemisphere which includes foliage, wood, inflorescences, pollen and fruits. A review of this record, focusing on, but not limited to, fruits, reveals patterns of evolution, distribution and extinction in the history of the family.; Palynological evidence suggests origin and rapid diversification of the Juglandaceae during the late Cretaceous and Paleocene. Well-documented juglandaceous megafossils first occur in the Paleocene of North America. By the late Paleocene and early Eocene, modern tribes and some modern genera (e.g. Cyclocarya and Platycarya) are recognizable on the basis of fruits. The family reached its greatest diversity by the middle Eocene. In contrast to the eight genera recognized today, fossil fruit data indicate the presence of at least ten distinct genera. Early Tertiary assemblages included both modern genera (e.g. Platycarya, cyclocarya, Pterocarya, and Juglans) and extinct genera (e.g. Paraengelhardtia, Paleooreomunnea, and Polyptera gen. nov.). As today, most of the early Tertiary genera had winged nutlets adapted for wind dispersal. The evolution of large wingless nuts coincides well with diversification of rodents. Although basic morphological patterns characteristic of modern genera were evolved early in the Tertiary, post-Eocene evolution is also evident, particularly involving shape and size of fruits.; There were two major periods of extinction in the history of the family. During the first episode, late Eocene, at least four genera became extinct and the ranges of others were substantially reduced. The surviving genera were those which had achieved a broad European-American distribution by the mid-Eocene. The second episode occurred during the Pleistocene, and also resulted in widescale reductions in geographic ranges, but not in generic extinction. These periods of extinction, both apparently climate-related, account for the relatively limited modern diversity and distribution of the walnut family.
机译:胡桃科(核桃科)在北半球有出色的化石记录,包括叶子,木材,花序,花粉和果实。回顾这份记录,重点是但不限于水果,揭示了家庭历史上的进化,分布和灭绝的模式。孢粉学证据表明,在白垩纪和新世晚期,胡桃科的起源和迅速多样化。有据可查的侏罗纪大型化石首先出现在北美的古新世。到古新世晚期和始新世早期,现代部落和一些现代属(例如Cyclocarya和Platycarya)已基于水果得以识别。到始新世中期,这个家庭达到了最大的多样性。与当今公认的八属相反,化石果实数据表明至少存在十个不同的属。早期的第三纪组合既包括现代属(例如Platycarya,cyclocarya,Pterocarya和Juglans),也包括绝种(例如Paraengelhardtia,Paleooreomunnea和Polyptera gen.nov。)。到今天为止,第三纪早期的大多数动物都有带翅的小坚果,适合风传播。无翼大坚果的进化与啮齿动物的多样化相吻合。尽管现代属植物的基本形态特征是在第三纪早期演化的,但始新世后的演化也很明显,特别是果实的形状和大小。家庭历史上有两个主要的灭绝时期。在第一个事件中,始新世晚期,至少有四个属灭绝,而其他的范围则大大减少。尚存的属是到新世中期已在欧美广泛分布的属。第二次发作发生在更新世,也导致了地理范围的广泛缩小,但没有造成一般性灭绝。这些灭绝时期显然都与气候有关,这是核桃家族现代多样性和分布相对有限的原因。

著录项

  • 作者

    MANCHESTER, STEVEN RUSSELL.;

  • 作者单位

    Indiana University.;

  • 授予单位 Indiana University.;
  • 学科 Paleobotany.
  • 学位 Ph.D.
  • 年度 1981
  • 页码 245 p.
  • 总页数 245
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 古植物学;
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号