中新世晚期北极极端气候放大的岩浆证据--近未来人为气候变化的类比?

IF 3.8 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Stuart Umbo, Franziska Lechleitner, Thomas Opel, Sevasti Modestou, Tobias Braun, Anton Vaks, Gideon Henderson, Pete Scott, Alexander Osintzev, Alexandr Kononov, Irina Adrian, Yuri Dublyansky, Alena Giesche, Sebastian Breitenbach
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引用次数: 0

摘要

摘要中新世的大气二氧化碳浓度和全球平均气温与下一世纪的预测相似,为不久的将来人为变暖提供了极好的气候模拟。然而,由于缺乏可靠的代用数据,中新世北极变暖的程度仍不清楚。在此,我们利用稳定氧同位素和痕量元素分析,以及岩浆岩的团块同位素和流体包裹体古温度测定法,重建了托尔托尼晚期(8.68 ± 0.09 Ma)西伯利亚北极海岸附近的古环境条件。稳定氧同位素记录表明当时的气温比现在要高。根据团块同位素和流体包裹体的温度估计,年平均气温在+6.6至+11.1 °C之间,而现在的年平均气温为-12.3 °C。微量元素记录显示了一个季节性很强的水文环境。我们估计北极变暖了18 °C,这支持了中新世比现在变暖的广泛共识,并为未来高排放情景下北极变暖提供了罕见的古模拟。重建的平均地表温度增幅远远超过了完全耦合的全球气候模型的预测,即使在极端排放情景下也是如此。鉴于气候模型一直低估了近期北极变暖的程度,我们的代用数据表明北极变暖可能会超过目前的预测。如果到 2100 年北极变暖的程度与我们对中新世晚期的估计一致,那么它将对全球气候产生大规模的影响,包括西伯利亚永久冻土的大面积解冻--永久冻土是一种巨大的化石碳储存。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Speleothem evidence for late Miocene extreme Arctic amplification – an analogue for near future anthropogenic climate change?
Abstract. The Miocene provides an excellent climatic analogue for near future anthropogenic warming, with atmospheric CO2 concentrations and global average temperatures similar to those projected for the coming century. However, the magnitude of Miocene Arctic warming remains unclear due to the scarcity of reliable proxy data. Here we use stable oxygen isotope and trace element analyses, alongside clumped isotope and fluid inclusion palaeothermometry of speleothems to reconstruct palaeo-environmental conditions near the Siberian Arctic coast during the late Tortonian (8.68 ± 0.09 Ma). Stable oxygen isotope records suggest warmer than present temperatures. This is supported by temperature estimates based on clumped isotopes and fluid inclusions giving mean annual air temperatures between +6.6 and +11.1 °C, compared with -12.3 °C today. Trace elements records reveal a highly seasonal hydrological environment. Our estimate of >18 °C of Arctic warming supports the wider consensus of a warmer-than-present Miocene and provides a rare paleo-analogue for future Arctic amplification under high emissions scenarios. The reconstructed increase in mean surface temperature far exceeds those projected in fully coupled global climate models, even under extreme emissions scenarios. Given that climate models have consistently underestimated the extent of recent Arctic amplification, our proxy data suggest Arctic warming may exceed current projections. If Arctic warming by 2100 matches our late Miocene estimates, it would have large-scale impacts on global climate, including extensive thawing of Siberian permafrost – a vast fossil carbon store.
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来源期刊
Climate of The Past
Climate of The Past 地学-气象与大气科学
CiteScore
7.40
自引率
14.00%
发文量
120
审稿时长
4-8 weeks
期刊介绍: Climate of the Past (CP) is a not-for-profit international scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on the climate history of the Earth. CP covers all temporal scales of climate change and variability, from geological time through to multidecadal studies of the last century. Studies focusing mainly on present and future climate are not within scope. The main subject areas are the following: reconstructions of past climate based on instrumental and historical data as well as proxy data from marine and terrestrial (including ice) archives; development and validation of new proxies, improvements of the precision and accuracy of proxy data; theoretical and empirical studies of processes in and feedback mechanisms between all climate system components in relation to past climate change on all space scales and timescales; simulation of past climate and model-based interpretation of palaeoclimate data for a better understanding of present and future climate variability and climate change.
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