成都理工大学马义权团队近日取得一项新成果。他们报道了中始新世气候最佳期火山和轨道所致的碳释放。这一研究成果发表在2024年7月30日出版的国际学术期刊《地质学》上。
据介绍,始新世中期气候最佳期(MECO)的驱动因素仍然是一个谜。研究人员报道了中国东部渤海湾盆地的高分辨率陆地MECO记录。记录显示,MECO期间显示出汞的阶段性富集和独特的火山成因Δ199Hg特征,而在MECO暖峰期间,显示出突发性化学风化增强和δ13Corg负偏移(CIE)为特征。
一个高分辨率的年龄模型将MECO的年龄限制在ca. 40.59-40.18 Ma,开始于第一个约320k.y.峰值温暖期,CIE开始于40.27 Ma,对应于405k.y.和100k.y.的偏心率最大值,并持续了约90k.y.,提示始新世早期的热液活动。
研究结果表明,幕式火山活动导致大气中二氧化碳分压的逐渐上升和MECO发作的持续时间较长。40.27Ma的轨道作用力,加上二氧化碳作用力,导致了峰值温度和正的碳循环反馈。区域风化的增加与全球大陆风化减弱的证据不一致,表明MECO变暖的风化响应具有强烈的空间异质性。
附:英文原文
Title: Volcanic and orbitally forced carbon release during the Middle Eocene Climatic Optimum
Author: Yiquan Ma, Majie Fan, Chen Zhang, Stephen E. Grasby, Runsheng Yin, Yangbo Lu, Bolin Zhang, Xin Jin, Chao Ma, Yongchao Lu, Appy Sluijs
Issue&Volume: 2024-07-30
Abstract: The drivers of the Middle Eocene Climatic Optimum (MECO) remain enigmatic. Here we report a high-resolution terrestrial MECO record from the Bohai Bay Basin, eastern China. The record shows episodic Hg enrichments and a volcanogenic Δ199Hg signature during the MECO, and an abrupt chemical weathering enhancement and negative δ13Corg excursion (CIE) during the MECO peak warmth. A high-resolution age model constrains the MECO to ca. 40.59-40.18 Ma with the onset in the first ~320 k.y. Peak warmth and the CIE initiated at 40.27 Ma, corresponding to 405 k.y. and 100 k.y. eccentricity maxima, and lasted for ~90 k.y., reminiscent of the early Eocene hyperthermals. Our findings suggest that episodic volcanism contributed to gradual atmospheric pCO2 rise, leading to the long duration of the MECO onset. Orbital forcing at 40.27 Ma, on top of CO2 forcing, caused the peak warmth and a positive carbon cycle feedback. The regional increase in weathering is inconsistent with evidence for weakened global continental weathering, suggesting strong spatial heterogeneity in the weathering response to MECO warming.
DOI: 10.1130/G52435.1
Geology:《地质学》,创刊于1973年。隶属于美国地质学会,最新IF:6.324
官方网址:https://pubs.geoscienceworld.org/geology
投稿链接:https://geology.msubmit.net/cgi-bin/main.plex