Reconstructing Precambrian pCO2 and pO2 Using Paleosols (Elements in Geochemical Tracers in Earth System Science) - Softcover
Book 15 of 23: Elements in Geochemical Tracers in Earth System Science
Synopsis
Paleosols formed in direct contact with the Earth's atmosphere, so they can record the composition of the atmosphere through weathering processes and products. Herein we critically review a variety of different approaches for reconstructing atmospheric O2 and CO2 over the past three billion years. Paleosols indicate relatively low CO2 over that time, requiring additional greenhouse forcing to overcome the 'faint young Sun' paradox in the Archean and Mesoproterozoic, as well as low O2 levels until the Neoproterozoic. Emerging techniques will revise the history of Earth's atmosphere further and may provide a window into atmospheric evolution on other planets.
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Reconstructing Precambrian pCO2 and pO2 Using Paleosols (Elements in Geochemical Tracers in Earth System Science)
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Reconstructing Precambrian pCO2 and pO2 Using Paleosols (Paperback)
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Paperback. Condition: new. Paperback. Paleosols formed in direct contact with the Earth's atmosphere, so they can record the composition of the atmosphere through weathering processes and products. Herein we critically review a variety of different approaches for reconstructing atmospheric O2 and CO2 over the past three billion years. Paleosols indicate relatively low CO2 over that time, requiring additional greenhouse forcing to overcome the 'faint young Sun' paradox in the Archean and Mesoproterozoic, as well as low O2 levels until the Neoproterozoic. Emerging techniques will revise the history of Earth's atmosphere further and may provide a window into atmospheric evolution on other planets. Paleosols formed in direct contact with the Earth's atmosphere, so they can record the composition of the atmosphere through weathering processes and products. Herein we critically review a variety of different approaches for reconstructing atmospheric O2 and CO2 over the past three billion years. Shipping may be from multiple locations in the US or from the UK, depending on stock availability. Seller Inventory # 9781108819008
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Reconstructing Precambrian pCO2 and pO2 Using Paleosols
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Reconstructing Precambrian pCO2 and pO2 Using Paleosols (Elements in Geochemical Tracers in Earth System Science)
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Reconstructing Precambrian pCO2 and pO2 Using Paleosols (Elements in Geochemical Tracers in Earth System Science)
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Reconstructing Precambrian pCO2 and pO2 Using Paleosols (Elements in Geochemical Tracers in Earth System Science)
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Reconstructing Precambrian pCO2 and pO2 Using Paleosols (Elements in Geochemical Tracers in Earth System Science)
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Reconstructing Precambrian pCO2 and pO2 Using Paleosols (Paperback)
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ISBN 10: 1108819001
ISBN 13: 9781108819008
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Paperback. Condition: new. Paperback. Paleosols formed in direct contact with the Earth's atmosphere, so they can record the composition of the atmosphere through weathering processes and products. Herein we critically review a variety of different approaches for reconstructing atmospheric O2 and CO2 over the past three billion years. Paleosols indicate relatively low CO2 over that time, requiring additional greenhouse forcing to overcome the 'faint young Sun' paradox in the Archean and Mesoproterozoic, as well as low O2 levels until the Neoproterozoic. Emerging techniques will revise the history of Earth's atmosphere further and may provide a window into atmospheric evolution on other planets. Paleosols formed in direct contact with the Earth's atmosphere, so they can record the composition of the atmosphere through weathering processes and products. Herein we critically review a variety of different approaches for reconstructing atmospheric O2 and CO2 over the past three billion years. This item is printed on demand. Shipping may be from our UK warehouse or from our Australian or US warehouses, depending on stock availability. Seller Inventory # 9781108819008
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