Late Cenozoic Vertebrate Biostratigraphy Across the TransMexican Volcanic Belt, Central Mexico

墨西哥中部跨墨西哥火山带的晚新生代脊椎动物生物地层学

• 批准号: 9902898
• 负责人: Wade Miller
• 金额: $ 23.46万
• 依托单位: Brigham Young University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 1999
• 资助国家: 美国
• 起止时间: 1999-08-01 至 2004-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9902898&HistoricalAwards=false
• 关键词: Late; Cenozoic; Vertebrate; Biostratigraphy; Across

Miller-EAR 9902898The Transmexican Volcanic Belt, which runs basically east-west across central Mexico, contains a series of north-south trending late Cenozoic grabens. These faulted basins contain a rich vertebrate fossil record that has only recently been recognized as to its extent. The apparent completeness of this record, based on preliminary research, shows great promise in being able to establish an unbroken evolutionary series of vertebrates from the early Miocene through the Pleistocene. Climatic and environmental changes of major scope, times of arrivals of South American immigrants, as well as reasons for extinctions of many forms are topics that will be addressed in the present research. Types of sediments, which include abundant volcanic ash and volcanic rocks bordering and underlying the basins, allow for great chronologic precision of the above events.

米勒-伊尔9902898横贯墨西哥中部的横贯东西方向的横贯墨西哥中部的德米西亚火山带，包含一系列南北走向的晚新生代地块。这些断陷盆地包含丰富的脊椎动物化石记录，直到最近才被认识到其程度。根据初步研究，这一记录表面上是完整的，这表明能够建立从早中新世到更新世的不间断的脊椎动物进化系列是很有希望的。主要范围的气候和环境变化、南美移民到达的时间以及多种形式灭绝的原因将是本研究将讨论的主题。沉积类型包括丰富的火山灰和火山岩，这些火山灰和火山岩位于盆地的边缘和下方，使得上述事件具有很高的年代学精度。