The Chemical Evolution of the Atmosphere and Oceans / / Heinrich D. Holland.

• Superior document: Title is part of eBook package: De Gruyter Princeton University Press eBook-Package Archive 1927-1999
• VerfasserIn: Holland, Heinrich D.,
• Place / Publishing House: Princeton, NJ : : Princeton University Press, , [2021]; ©1984
• Year of Publication: 2021
• Language: English
• Series: Princeton Series in Geochemistry ; 2
• Physical Description: 1 online resource (598 p.)
• Other title: Frontmatter --; Contents --; Preface --; 1 The Origin of the Solar System --; 2 Inputs to the Earliest Atmosphere --; 3 Release and Recycling of Volatiles during Earth History --; 4 The Chemistry of the Earliest Atmosphere and Ocean --; 5 The Acid-Base Balance of the Atmosphere-Ocean- Crust System --; 6 Carbonates, Clays, and Exchange Reactions --; 7 Oxygen in the Precambrian Atmosphere: Evidence from Terrestrial Environments --; 8 Oxygen in the Precambrian Atmosphere: Evidence from Marine Environments --; 9 The Composition of the Atmosphere and Oceans during the Phanerozoic Eon --; Index
• Format: Mode of access: Internet via World Wide Web.
• ISBN: 9780691220239; 9783110442496
• DOI: 10.1515/9780691220239?locatt=mode:legacy
• Access: restricted access
• Hierarchical level: Monograph
• Statement of Responsibility: Heinrich D. Holland.

In this first full-scale attempt to reconstruct the chemical evolution of the Earth's atmosphere and oceans, Heinrich Holland assembles data from a wide spectrum of fields to trace the history of the ocean-atmosphere system. A pioneer in an increasingly important area of scholarship, he presents a comprehensive treatment of knowledge on this subject, provides an extensive bibliography, and outlines problems and approaches for further research.The first four chapters deal with the turbulent first half billion years of Earth history. The next four chapters, devoted largely to the Earth from 3.9 to 0.6 b.y.b.p., demonstrate that changes in the atmosphere and oceans during this period were not dramatic. The last chapter of the book deals with the Phanerozoic Eon; although the isotopic composition of sulfur and strontium in seawater varied greatly during this period of Earth history, the chemical composition of seawater did not.