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广东南雄盆地晚白垩世—早第三纪非海相腹足类组合序列 被引量:19
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作者 余汶 顾和林 张显球 《古生物学报》 CAS CSCD 北大核心 1990年第2期160-182,263-266,共27页
一、前言南雄盆地位于粤北浈水流域,横跨粤赣两省,呈北东向展布,面积约1000km^2(插图1)。盆地受新华夏构造体系控制,是一个地堑式断陷盆地,晚白垩世至早第三纪沉积了厚达2000—3000m以河湖相为主的地层,其中含有极丰富的非海相腹足类化... 一、前言南雄盆地位于粤北浈水流域,横跨粤赣两省,呈北东向展布,面积约1000km^2(插图1)。盆地受新华夏构造体系控制,是一个地堑式断陷盆地,晚白垩世至早第三纪沉积了厚达2000—3000m以河湖相为主的地层,其中含有极丰富的非海相腹足类化石。通过近几年来资料的收集、积累并加以系统的分析研究。 展开更多
关键词 晚白垩世 早第三纪 南雄 新华夏构造体系 地堑 层位 登记号 浓山组 口视 上湖
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First Asian Paleocene pantolambdid pantodont(Mammalia)and its implications to intercontinental faunal exchange
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作者 QUAN Shuo-Shuo WANG Yuan-Qing 《古脊椎动物学报(中英文)》 CSCD 北大核心 2024年第4期291-312,共22页
Pantodonta was one of the first groups of eutherians to evolve at the beginning of Cenozoic era,including the largest herbivores at that time.Pantodonta shows considerable diversity during the Paleocene and Eocene,wit... Pantodonta was one of the first groups of eutherians to evolve at the beginning of Cenozoic era,including the largest herbivores at that time.Pantodonta shows considerable diversity during the Paleocene and Eocene,with most of the species having been discovered in Asia and North America.Here,we report on a new pantodont,represented by lower jaws with well-preserved dentition,discovered from the Middle Paleocene Nongshan Formation of the Nanxiong Basin,Guangdong Province,China.Its unique dental and mandibular characteristics distinguish it well from any known Asian pantodont,but are quite consistent with North American taxa,especially Pantolambda and Titanoides.The new specimen is identified as Nanxiongilambda yei gen.et sp.nov.,characterized by the combination of the following morphological features:thick and robust mandible with a conspicuous anteroexternal flange,high positioned condyloid process,posteriorly protruding angular process,robust but not elongated lower canines,double-rooted p1,small but distinct talonids on posterior lower premolars,talonids nearly as wide as trigonids on lower molars,and m3 with a well-developed hypoconulid and a distinct entoconid.The new discovery marks the first record of a pantolambdid pantodont outside of North America,suggesting a broader geographical distribution and intercontinental dispersal of this clade during the Paleocene.Considering the more primitive Pantolambda only found from Torrejonian to early Tiffanian NALMA(equivalent to middle-late Shanghuan to early Nongshanian ALMA),which is slightly earlier than Nanxiongilambda(early Nongshanian ALMA),pantolambdids have likely undergone a particular wave of migration from North America to Asia during the Early-Middle Paleocene.Previous researches have suggested that pantodonts had dispersed only from Asia to North America during the Early Paleocene,but our new specimen indicates the biotic dispersal may have occurred in the opposite direction.The new specimen also contributes to the renewal of the evolutionary history of pantodonts and provides further insights into the migration and dispersal of Paleocene mammals. 展开更多
关键词 Nanxiong Basin Paleocene Nongshan Formation Pantodonta Pantolambdidae Nanxiongilambda
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广东第三纪岩石地层划分 被引量:2
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作者 黎汉明 《广东地质》 1995年第1期69-76,共8页
广东第三纪地层分布于雷州半岛及茂名,南雄,淡水和三水等盆地及其外围,主要由紫红色、灰黑色等碎屑岩组成,含哺乳类,腹足类,叶肢介,介形虫,有孔虫,植物和轮藻等化石。据地层位置和宏观岩性特征,以研究程度较高的盆地为基础,... 广东第三纪地层分布于雷州半岛及茂名,南雄,淡水和三水等盆地及其外围,主要由紫红色、灰黑色等碎屑岩组成,含哺乳类,腹足类,叶肢介,介形虫,有孔虫,植物和轮藻等化石。据地层位置和宏观岩性特征,以研究程度较高的盆地为基础,划分为19个岩石地层单位。 展开更多
关键词 第三纪 岩石 地层划分 广东 浓山组
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