Enhanced Terrestrial Weathering in the North American Interior across the Paleocene/Eocene Boundary

古新世/始新世边界北美内陆陆地风化增强

• 批准号: 0518437
• 负责人: D Kelly
• 金额: --
• 依托单位: University of Wisconsin-Madison
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2005
• 资助国家: 美国
• 起止时间: 2005-07-01 至 2009-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0518437&HistoricalAwards=false
• 关键词: Enhanced; Terrestrial; Weathering; North; American

It is important to understand the past responses of earth's terrestrial geochemical reservoirs to atmospheric perturbations in order to predict future impacts on the existing environment. The "initial Eocene thermal maximum" (IETM, ca. 55 Ma) was a short-lived (~100 - 200 kyr) global warming event driven by a sudden increase in greenhouse gases similar in temporal scale to present-day anthropogenic influxes. This influx was postulated to have been due to a massive release of methane from marine gas hydrates. The subsequent increased levels of atmospheric greenhouse gases [carbon dioxide (CO2) and methane (CH4)] had a worldwide impact on the earth's surficial processes and functional partitioning of biogeochemical cycles. Marine records of the IETM clearly document the isotopic and mineralogic shifts triggered by this perturbation, while the response on subaerially exposed landmasses is not as well understood. Of particular interest is the transient character of this climatic overshoot, which reflects the presence of negative feedbacks (accelerated weathering reactions) that stabilized climate by reducing atmospheric levels of greenhouse gases. We propose to study the influence of this climatic warming on sedimentation patterns and weathering rates within the remarkably fine-textured sedimentary members of the Williston Basin (WB) in western North Dakota. These units contain well preserved, multi-proxy information (i.e., palynomorph/ macrofloral fossils, authigenic minerals and paleopedogenic features, well-preserved organic materials) that lends itself well to temporal and spatial cross-correlation. This study poses the hypothesis that the fine resolution stratigraphic package in the WB records a sympathetic terrestrial signal/response to the release of isotopically-light marine methane hydrate and subsequent global warming. To investigate this hypothesis, we will use 1) whole sediment composition, 2) semi-quantitative clay mineralogy, and 3) stable isotope geochemistry to ascertain alterations and rates in sedimentary process and sub-aerial weathering intensity in response to the warmer global climate hypothesized to have prevailed during the IETM. Our preliminary investigations provide evidence indicating that a record of the IETM is preserved within the WB and that there is a definitive shift in sediment geochemistry across this boundary. This integrated record can be tied to well-documented IETM records in neighboring contemporaneous interior basins (e.g., Bighorn Basin of Wyoming) and will augment our understanding of mid-latitude sub-continental response to rapid climate change.Broader Impacts: It is important to compare the reality of a well-preserved multi-proxystratigraphic record to thermodynamic models of biogeochemical fluxes and estimated physical reconstructions from an interdisciplinary aspect. The linkage of our records to those preserved in the Big Horn Basin will build a stronger understanding of sub-continental land mass responses to rapid global warming. The principle investigators will utilize the information to strengthen fledgling research programs in paleoenvironmental reconstruction and paleopedology. This study will be a mechanism for graduate/ undergraduate students to develop research projects. Once investigative work has yielded a comprehensive data set, a colloquium field trip class will be conducted, with participants conducting weekly discussions in preparation for a two-week field excursion through the Western Interior Basin (WIB) province (Williston, Powder River, Bighorn, Wasatch, and Green River Basins). This will provide students an opportunity to view and synthesize sub-continental scale information. Manuscripts from this project will be published in recognized interdisciplinary earth science journals and a linked website devoted to the WIB with specific focus on the work encompassed by this study will be constructed for access by the academic community. Finally, results of this proposed research will be incorporated into a public outreach program at the University of Wisconsin Geology Museum.

了解地球陆地地球化学储层对大气扰动的过去响应对于预测未来对现有环境的影响是很重要的。“始新世初始热最大值”（IETM，ca。55 Ma）是一个短暂的（约100 - 200 kyr）全球变暖事件，由温室气体突然增加驱动，其时间尺度类似于当今的人为流入。据推测，这种流入是由于海洋天然气水合物大量释放甲烷造成的。随后大气中温室气体[二氧化碳（CO2）和甲烷（CH 4）]水平的增加对地球的表面过程和地球化学循环的功能分区产生了世界范围的影响。IETM的海洋记录清楚地记录了这种扰动引发的同位素和矿物学变化，而对地表下暴露的陆块的反应还不清楚。特别令人感兴趣的是这种气候超调的短暂性，这反映了负反馈（加速风化反应）的存在，通过减少大气中的温室气体水平来稳定气候。我们建议研究这种气候变暖的影响，在北达科他州西部的威利斯顿盆地（WB）的纹理非常细的沉积成员的沉积模式和风化速率。这些单元包含保存良好的多代理信息（即，孢粉/大植物群化石、自生矿物和古土壤特征、保存完好的有机物质），这很适合于时间和空间的相互关联。这项研究提出了一个假设，即WB中的精细分辨率地层包记录了对同位素轻海洋甲烷水合物释放和随后的全球变暖的同情陆地信号/响应。为了研究这一假设，我们将使用1）全沉积物组成，2）半定量粘土矿物学，和3）稳定同位素地球化学，以确定沉积过程和陆上风化强度的变化和速率，以应对IETM期间假设的全球气候变暖。我们的初步调查提供的证据表明，记录的IETM保存在WB和有一个明确的转变，在沉积物地球化学跨越这一边界。这一综合记录可以与邻近的同生内陆盆地中有据可查的IETM记录联系起来（例如，Bighorn盆地的怀俄明州），并将增加我们的中纬度次大陆的快速气候变化的反应的理解。更广泛的影响：重要的是比较现实的保存完好的多proxystratification记录的热力学模型的地球化学通量和估计的物理重建从跨学科的方面。将我们的记录与大角盆地保存的记录联系起来，将有助于更好地了解次大陆大陆对快速全球变暖的反应。主要研究人员将利用这些信息来加强古环境重建和古土壤学方面的新兴研究项目。这项研究将成为研究生/本科生制定研究项目的机制。一旦调查工作产生了一个全面的数据集，将进行一个座谈会实地考察班，与参与者进行每周讨论，准备通过西部内陆盆地（WIB）省（威利斯顿，粉河，大角，瓦萨奇，和绿色河流域）为期两周的实地考察。这将使学生有机会查看和综合次大陆规模的信息。该项目的论文将发表在公认的跨学科地球科学期刊上，并将建立一个专门针对WIB的链接网站，专门关注本研究所涵盖的工作，供学术界访问。最后，这项研究的结果将被纳入威斯康星州地质博物馆的公共宣传计划。