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Coupling of surface temperatures and atmospheric CO_2 concentrations during the Palaeozoic era

机译:古生代地表温度与大气CO_2浓度的耦合

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Atmospheric carbon dioxide concentrations seem to have been several times modern levels during much of the Palaeozoic era (543-248 million years ago), but decreased during the Carboniferous period to concentrations similar to that of today. Given that carbon dioxide is a greenhouse gas, it has been proposed that surface temperatures were significantly higher during the earlier portions of the Palaeozoic era. A reconstruction of tropical sea surface temperatures based on the δ~(18)O of carbonate fossils indicates, however, that the magnitude of temperature variability throughout this period was small, suggesting that global climate may be independent of variations in atmospheric carbon dioxide concentration. Here we present estimates of sea surface temperatures that were obtained from fossil brachiopod and mollusc shells using the 'carbonate clumped isotope' method—an approach that, unlike the δ~(18)O method, does not require independent estimates of the isotopic composition of the Palaeozoic ocean. Our results indicate that tropical sea surface temperatures were significantly higher than today during the Early Silurian period (443-423 Myr ago), when carbon dioxide concentrations are thought to have been relatively high, and were broadly similar to today during the Late Carboniferous period (314-300 Myr ago), when carbon dioxide concentrations are thought to have been similar to the present-day value. Our results are consistent with the proposal that increased atmospheric carbon dioxide concentrations drive or amplify increased global temperatures.%地球大气中高浓度的二氧化碳在遥远的地质年代是否始终与全球变暖 联系在一起?关于这个问题,地质学家有不同看法。对全球变暖持怀 疑态度的人们总是能抓住这一点。但一项新的研究工作为传统观点提 供了进一步支持:大气二氧化碳浓度和地球表面温度在地球的整个历 史上一直是紧密联系在一起的。应用“carbonate clumped isotope" “古温度计”(palaeothermometer)对古生代海洋温度所做的分析表 明,当大气二氧化碳浓度相对于目前水平较高时,地球温度明显较 高;而当大气二氧化碳浓度低到跟今天差不多时,地球温度也跟今天 的相似。
机译:在古生代的大部分时期(543-2.48亿年前),大气中的二氧化碳浓度似乎已经是现代水平的几倍,但在石炭纪时期降低到今天的浓度。考虑到二氧化碳是一种温室气体,已经提出在古生代早期,地表温度要高得多。然而,基于碳酸盐化石的δ〜(18)O重建热带海面温度表明,在此期间温度变化的幅度很小,这表明全球气候可能与大气二氧化碳浓度的变化无关。在这里,我们介绍了使用“碳酸盐成簇同位素”方法从腕足动物和软体动物壳中获得的海面温度的估算值,该方法与δ〜(18)O方法不同,不需要对同位素的同位素组成进行独立估算古生代海洋。我们的结果表明,在志留纪早期(443-423 Myr以前),热带海面温度明显高于今天,当时人们认为二氧化碳浓度相对较高,并且与今天石炭纪晚期(今天)大致相似( 314-300 Myr之前),当时认为二氧化碳浓度与当前值相似。我们的结果与增加大气中二氧化碳浓度驱动或放大全球温度升高的提议相符。%地球大气中高浓度的二氧化碳在遥远的地质年代是否始终与全球变暖联系在一起?关于这个问题,地质学家有对全球变暖持怀问题态度的人们总是能抓住这一点。但一项新的研究工作为传统观点提供了更多支持:大气浓度和地球表面温度在地球的整个历史上应用“碳酸盐丛集的同位素”“古温度计”(古温度计)对古生代海洋温度处理的分析表明,当大气二氧化碳浓度相对于目前水平较高时,地球温度明显较高;而当大气二氧化碳浓度低到跟今天差不多时,地球温度也跟今天的相似。

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