Neoproterozoic Milankovitch cycles and the prelude to complex life

新元古代米兰科维奇周期和复杂生命的前奏

• 批准号: 578476-2022
• 负责人: Davies, JoshuaHFL
• 金额: $ 7.29万
• 依托单位: Université du Québec à Montréal
• 依托单位国家: 加拿大
• 项目类别: Alliance Grants
• 财政年份: 2022
• 资助国家: 加拿大
• 起止时间: 2022-01-01 至 2023-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=765300
• 关键词: Neoproterozoic; Milankovitch; cycles; prelude; complex

The late Neoproterozoic Era, between ca. 745 and 539 million years ago, marks a crucial interval in Earth's history. During this time period, Earth experienced multiple glaciations, two of which were global in extent, significantly increased atmospheric oxygen levels, and the rise and diversification of complex life, which set in motion the Cambrian radiation of animals. Despite the importance of these critical events, little is known about the role of cyclic oscillations in Earth's orbit and inclination (Milankovitch cycles) on Neoproterozoic climate and environments. Milankovitch cycles are known to have modulated Phanerozoic climate, including the advance and retreat of Pleistocene ice ages, oxygen levels in the oceans and the distribution and evolution of flora and fauna, including humans. The objective of this International Alliance project is to test whether orbital forcing played a role in triggering major climatic and biospheric change during the Neoproterozoic, with emphases on the time intervals spanning the two global glaciations and the appearance and diversification and eventual disappearance of the Ediacaran biota at the close of the Precambrian (~539 million years ago). This project will foster a multi-disciplinary team of leading researchers in their fields who together will integrate cutting edge cyclostratigraphic, biostratigraphic, chemostratigraphic and sequence stratigraphic techniques with high-precision single zircon U-Pb geochronology, isotope geochemistry and Bayesian age depth modelling. The results will provide novel insights into the Earth system during this great transition in its history. This effort will place Canada and its researchers firmly at the forefront of understanding links between the solar system, Earth's surface environment, climate and complex life.

新元古代晚期，约7.45亿至5.39亿年前，是地球历史上的一个关键时期。在这段时间里，地球经历了多次冰期，其中两次是全球性的，大气含氧量显著增加，复杂生命的兴起和多样化，启动了寒武纪动物的辐射。尽管这些关键事件很重要，但人们对地球轨道和倾角的周期振荡（米兰科维奇周期）在新元古代气候和环境中的作用知之甚少。众所周知，米兰科维奇旋回调节了显生宙的气候，包括更新世冰期的进退、海洋中的氧气水平以及包括人类在内的动植物的分布和进化。这个国际联盟项目的目的是测试轨道强迫在新元古代是否在触发主要的气候和生物圈变化中发挥了作用，重点是跨越两次全球冰期的时间间隔，以及前寒武纪末期（~ 5.39亿年前）埃迪卡拉动物群的出现、多样化和最终消失。该项目将培养一支由各自领域的顶尖研究人员组成的多学科团队，他们将把尖端的旋回地层学、生物地层学、化学地层学和层序地层学技术与高精度的单锆石U-Pb地质年代学、同位素地球化学和贝叶斯年龄深度建模结合起来。这些结果将为地球系统在其历史上的这一巨大转变提供新的见解。这一努力将使加拿大及其研究人员坚定地站在了解太阳系、地球表面环境、气候和复杂生命之间联系的最前沿。