简介:三叶虫证据表明,除北疆区的阿尔泰地体和兴安区的额尔古纳-兴安地体与西伯利亚和劳伦陆块在动物群方面紧密关联外,中国奥陶纪的所有板块和大部分地体均系当时东泛冈瓦纳的重要组成部分,在生物地理上彼此密切相关。对这些属于东泛冈瓦纳的中国区块的台地或内陆棚三叶虫动物群的综合分析研究证明,它们在特马豆克期(Tremadocian)以及凯迪晚期-赫南特期(lateKatian-Hirnantian)或阿石极期(Ashgill)应归属同一生物地理区,而在弗洛期-凯迪早期(Floian—earlyKatian)或阿仑尼克期-卡拉多克期(Arenig—Caradoc)则可划分为两个生物地理亚区:一个由华南、塔里木板块和安南或印支地体组成,另一个包括华北板块以及滇缅马、藏南、中天山-北山地体(可能还有海南地体)。饶有趣味的是在凯迪晚期或阿石极期开始发生的生物地理亚区解体之前,有关陆块的深水相三叶虫动物群已经历了从达瑞威尔中期(midDarriwilian)至凯迪早期的长期频繁交流以及组成逐渐趋于齐一的过程。因此深水动物群之间的属种交流和一体化进程的发生、发展和完成显然均先于浅水一侧的三叶虫。
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简介:摘 要:准确认定地表覆盖图斑类型,是地理国情监测的重要内容,对地理国情监测成果的应用至关重要。本文结合多年生产经验,梳理总结地表覆盖图斑类型的认定思路和方法,以提高地理国情监测中地表覆盖图斑类型认定的准确性。