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中生代主要植物化石的古气候指示意义
  • ISSN号:1671-1505
  • 期刊名称:《古地理学报》
  • 时间:0
  • 分类:Q914.6[天文地球—古生物学与地层学;生物学—古生物学]
  • 作者机构:[1]中国石油勘探开发研究院,北京100083
  • 相关基金:国家科技部973项目(2006CB701400)和国家自然科学基金项目(40372021)资助
作者: 邓胜徽[1]
中文摘要:

中生代植物群以真蕨纲、苏铁纲、银杏纲、松柏纲为主,另有苔藓类、石松纲、楔叶纲及其他种子植物等。从化石的形态和结构、埋藏特点、分布及与现生类型的对比等方面,概要地分析了中生代植物群常见分子的古气候指示意义。其中,反映温暖潮湿气候或生境的主要有苔藓类,石松纲的Lycopodites和Selaginel-lites属等,楔叶纲,真蕨纲的单缝孢类、早白垩世的蚌壳蕨科、海金砂科的Ruffordia属、紫萁科及可能相关的小羽片大型的Cladophlebis,银杏纲银杏目的主要类型,松柏纲杉科的Athrotaxoites、Cunninghamia、Cephalotaxop-sis、Sequoia等,紫杉科的Taxus、Torreya等,苏铁杉科的Ferganiella、Podozamites、Swedenborgia等以及形态属Elatocladus;反映温凉气候的主要有松柏纲的松科和银杏纲的茨康目;适应热带、亚热带气候的包括真蕨类的海金沙科、合囊蕨科、马通蕨科、双扇蕨科、桫椤科、里白科以及中国蕨科的Onychiopsis等,苏铁目和本内苏铁目的主要类型;指示偏干旱型气候的主要有石松纲的Pleuromeia和Isoetites,真蕨纲的Weichiselia,本内苏铁目的Otozamites、Zamites、Ptilophyllum等,松柏纲掌鳞杉科的Pseudoflenelopsis、Flenelopsis、Hirmeriella和可能属于掌鳞杉科的Brachyphyllum和Pagiophyllum,柏科的Cupressinocladus以及买麻藤目的Ephedrites等。

英文摘要:

The typical Mesozoic floras are mainly composed of Filicopsida, Cycadopsida, Ginkgopsida and Coniferopsida, as well as some Bryophyta, Lycopdopsida, Sphenopsida and other seed plants. The palaeoclimatic implications of main fossil plants of the Mesozoic except the angiosperms are dealt with in this paper based on their morphologic and anatomic features, taphonomic data, geographic distribution and comparisons with their living affinitive groups. The Mesozoic plants with palaeoclimatic significances are roughly divided into four groups. The first one, which represents temperate-humid climate, consists of bryophytes; Lycopodites and Selaginellites of lycopods; sphenophytes; ferns including the Early Cretaceous Dicksoniaceae, Ruffordia of Schizaeaceae, Osmundaceae and Cladophlebis with large pinnules, monolete spore ferns, the main elements of the Ginkgoales; conifers including Athrotaxoites, Cunninghamia, Elatocladus, Swedenborgia, Cephalotaxopsis, Sequoia, Taxus, Torreya, Ferganiella, Podozamites, and etc..The second group mainly includes the Pinaceae of conifers and some of Ginkgopsida, especially the Czekanowskiales, which usually indicate a moderate-cool climate. The third group indicates warm tropical and subtropical climate, which mainly consists of ferns, such as Schizaeaceae, Marratiaceae, Matoniaceae, Dipteridaceae, Cyatheaceae, Gleicheniaceae and the possible sinopteridaceous fern Onychiopsis and most of the Cycadales and Bennettitales. The fourth group adapted to warm-arid climate is represented chiefly by the lycopod Pleuromeia and Isoetites; fern Weichselia; Bennettitales, such as Otozamites, Zamites, Ptilophyllum, Tyrmia, and etc.; the Cheirolepidaceae including Pseudoflenelopsis, Flenelopsis, Hirmeriella and the possible cheirolepidaceous conifers Brachyphyllum and Pagiophyllum; cupressaceous conifer Cupressinocladus; as well as the possible desert plant Ephedrites.

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期刊信息
  • 《古地理学报》
  • 中国科技核心期刊
  • 主管单位:中华人民共和国教育部
  • 主办单位:中国石油大学 中国矿物岩石地球化学学会
  • 主编:冯增昭
  • 地址:北京市学院路20号中国石油大学
  • 邮编:100083
  • 邮箱:Jpalaeo1999@163.com
  • 电话:010-62396246 62341089
  • 国际标准刊号:ISSN:1671-1505
  • 国内统一刊号:ISSN:11-4678/P
  • 邮发代号:2-739
  • 获奖情况:
  • 国内外数据库收录:
  • 俄罗斯文摘杂志,美国化学文摘(网络版),美国剑桥科学文摘,美国石油文摘,中国中国科技核心期刊,中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版)
  • 被引量:9344