Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
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Equatorial heat accumulation as a long-term trigger of permanent Antarctic ice sheets during the CenozoicExtreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum.Future climate forcing potentially without precedent in the last 420 million years.Very large release of mostly volcanic carbon during the Palaeocene-Eocene Thermal Maximum.Highly selective and active CO2 reduction electrocatalysts based on cobalt phthalocyanine/carbon nanotube hybrid structures.Initiation and long-term instability of the East Antarctic Ice Sheet.Regulation of Coordination Number over Single Co Sites: Triggering the Efficient Electroreduction of CO2.Did Photosymbiont Bleaching Lead to the Demise of Planktic Foraminifer Morozovella at the Early Eocene Climatic Optimum?Stratigraphic and Earth System approaches to defining the AnthropoceneNo substantial long-term bias in the Cenozoic benthic foraminifera oxygen-isotope recordMiddle Eocene greenhouse warming facilitated by diminished weathering feedbackBeyond equilibrium climate sensitivityDeep time evidence for climate sensitivity increase with warmingCapturing the global signature of surface ocean acidification during the Palaeocene-Eocene Thermal MaximumLate Lutetian Thermal Maximum-Crossing a Thermal Threshold in Earth's Climate System?A record of Neogene seawater <i>δ</i><sup>11</sup>B reconstructed from paired <i>δ</i><sup>11</sup>B analyses on benthic and planktic foraminiferaLessons on Climate Sensitivity From Past Climate ChangesA lower limit to atmospheric CO2 concentrations over the past 800,000 yearsCalibration of the B/Ca proxy in the planktic foraminifer Orbulina universa to Paleocene seawater conditionsModerate levels of Eocene pCO2 indicated by Southern Hemisphere fossil plant stomata
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P2860
Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
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2016 nî lūn-bûn
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2016年の論文
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2016年学术文章
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Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
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Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
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Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
@en
Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
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Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate
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Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
@en
Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
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Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
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Eleanor H John
Paul N Pearson
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10.1038/NATURE17423
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P577
2016-04-25T00:00:00Z