RUI: Characterizing Arctic lakes during greenhouse climates through an analysis of siliceous organisms: A glimpse of what the future may hold.

RUI：通过对硅质生物的分析来描述温室气候下的北极湖泊的特征：展望未来。

• 批准号: 1144098
• 负责人: Peter Siver
• 金额: $ 37.98万
• 依托单位: Connecticut College
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-02-01 至 2017-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1144098&HistoricalAwards=false
• 关键词: RUI; Characterizing; Arctic; lakes; during

Over 40 million years ago, long before anthropogenic greenhouse gas emissions was an issue, the Earth was engulfed in an extremely warm period known as the Cenozoic hot house. The warming correlated with an ice-free Earth, lush forests on land masses near the North Pole, and alligators, giant tortoises and tapirs roaming the high Arctic. Indeed, the warmth experienced during the Cenozoic hot house was strikingly similar to future warming estimates derived from climate models. Thus, the Cenozoic hot house represents an ideal analog for understanding future changes resulting from warmer climates. The goal of this project is to document the remains of microscopic plant and animal organisms from three extensive Arctic lake cores that collectively span the Cenozoic hot house, and use the findings to evaluate the development and resilience of freshwater ecosystems in a warm greenhouse world. Preservation and sheer numbers of microfossils in the three cores are unprecedented and the project will also yield a unique opportunity to address long-standing evolutionary questions for ecologically important freshwater organisms. Global warming, caused by higher concentrations of greenhouse gases, is advancing at an unprecedented rate and is arguably the most pressing environmental issue facing society today. Computer models predict significantly elevated warming in Arctic regions, and all indications are that the warming will cause profound reorganizations of biological communities. However, since there are no Arctic ecosystems currently experiencing such warm conditions, we lack data that could be used to verify the computer models. The project offers a unique chance to understand how Arctic freshwater ecosystems did, and most likely will, respond to warming.

4000多万年前，早在人为温室气体排放成为问题之前，地球就被一个被称为新生代热屋的极端温暖时期所吞没。 气候变暖与无冰的地球、北极附近陆地上茂密的森林以及在北极高纬度地区漫游的短吻鳄、巨龟和貘有关。 事实上，在新生代热屋期间经历的温暖与气候模型得出的未来变暖估计惊人地相似。 因此，新生代温室是理解未来气候变暖所导致的变化的理想模拟。 该项目的目标是记录来自三个广泛的北极湖泊核心的微观植物和动物有机体的遗骸，这些湖泊核心共同跨越新生代温室，并利用这些发现来评估淡水生态系统在温暖的温室世界中的发展和恢复力。 三个核心中保存的微化石数量是前所未有的，该项目还将为解决具有生态重要性的淡水生物长期存在的进化问题提供独特的机会。 由温室气体浓度升高引起的全球变暖正以前所未有的速度发展，可以说是当今社会面临的最紧迫的环境问题。 计算机模型预测，北极地区的变暖将显著加剧，所有迹象都表明，变暖将导致生物群落的深刻重组。 然而，由于目前没有北极生态系统经历如此温暖的条件，我们缺乏可用于验证计算机模型的数据。 该项目提供了一个独特的机会来了解北极淡水生态系统如何应对气候变暖。