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Biological Weathering and the Environment of the Earth [electronic resource] / by Tasuku Akagi.

By: Contributor(s): Material type: TextSeries: Ecological Research MonographsPublisher: Singapore : Springer Nature Singapore : Imprint: Springer, 2024Edition: 1st ed. 2024Description: XVII, 181 p. 67 illus. online resourceContent type:
  • text
Media type:
  • computer
Carrier type:
  • online resource
ISBN:
  • 9789819744268
Subject(s):
Additional physical formats: Printed edition:: No title; Printed edition:: No title; Printed edition:: No titleLOC classification:
  • QH540-549.5
Online resources:
Contents:
Part 1 Biological weathering Chapter 1: Weathering and feedback system -- Chapter 2: Plant-induced weathering -- Chapter 3: Weathering as physiological strategy -- Part 2 Diatom contribution Chapter 4: Diatoms -- Chapter 5: Thickly veiled frustules -- Chapter 6: Extra nerdy proof of dirty frustules -- Chapter 7: Diatoms eat rock -- Chapter 8: Transparent exopolymer particles (TEP) -- Chapter 9: Diatoms and marine chemistry -- Part 3. Weathering in the ocean Chapter 10: Coupling of carbon and silica in the oceans.-Chapter 11: Weathering in the oceans -- Chapter 12: How to store (or release) carbon in (or from) deep ocean Part 4. Ocean weathering and the glacial cycles Chapter 13: Glacial cycles and unresolved questions -- Chapter 14: Ocean weathering as a key to glacial problem -- Part 5. Ocean weathering may save us Chapter 15: Contemporary CO2 problem -- Chapter 16: Ocean weathering as a key to the contemporary CO2 problem -- Chapter 17: An urgent proposal.
In: Springer Nature eBookSummary: This book introduces the concept of 'biological weathering.' Weathering, especially chemical weathering, has been recognized as one of the most important processes on Earth because it influences the circulation of elements, including carbon. Weathering has almost always been considered an abiotic process. The book describes the author’s experiments, proving that plant involvement in weathering is a strategy for plants to ingest nutrients from rocks. It is also shown through cultivation experiments and observation of natural diatoms that diatoms and silica obligate plankton dissolve silicate minerals and incorporate silicon and other elements into their frustules. The weathering reaction has also been successfully applied to the previously unexplained relationship between carbon and silica in the ocean’s interior. Readers of this book will gain a comprehensive understanding of weathering as a reaction catalyzed by both plants and plankton, occurring not only on land but also ubiquitously in the earth’s environment, including the ocean’s interior. This new and novel perspective has significant implications for various scientific fields, including biology, marine chemistry, environmental, and paleoenvironmental sciences. The author underscores the immediate relevance of these findings to pressing issues surrounding atmospheric CO2. The book concludes with a proposal for an efficient and safe method to sequester CO2 in the atmosphere into the ocean interior, offering a practical solution to a global challenge. The target audience for this book includes students and researchers in ecology, evolutionary biology, geochemistry, environment and plant sciences, atmospheric sciences, and Geo-industries.
Item type: List(s) this item appears in: Titluri cărți electronice Springer Nature 2025 (10631 titluri)
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Part 1 Biological weathering Chapter 1: Weathering and feedback system -- Chapter 2: Plant-induced weathering -- Chapter 3: Weathering as physiological strategy -- Part 2 Diatom contribution Chapter 4: Diatoms -- Chapter 5: Thickly veiled frustules -- Chapter 6: Extra nerdy proof of dirty frustules -- Chapter 7: Diatoms eat rock -- Chapter 8: Transparent exopolymer particles (TEP) -- Chapter 9: Diatoms and marine chemistry -- Part 3. Weathering in the ocean Chapter 10: Coupling of carbon and silica in the oceans.-Chapter 11: Weathering in the oceans -- Chapter 12: How to store (or release) carbon in (or from) deep ocean Part 4. Ocean weathering and the glacial cycles Chapter 13: Glacial cycles and unresolved questions -- Chapter 14: Ocean weathering as a key to glacial problem -- Part 5. Ocean weathering may save us Chapter 15: Contemporary CO2 problem -- Chapter 16: Ocean weathering as a key to the contemporary CO2 problem -- Chapter 17: An urgent proposal.

This book introduces the concept of 'biological weathering.' Weathering, especially chemical weathering, has been recognized as one of the most important processes on Earth because it influences the circulation of elements, including carbon. Weathering has almost always been considered an abiotic process. The book describes the author’s experiments, proving that plant involvement in weathering is a strategy for plants to ingest nutrients from rocks. It is also shown through cultivation experiments and observation of natural diatoms that diatoms and silica obligate plankton dissolve silicate minerals and incorporate silicon and other elements into their frustules. The weathering reaction has also been successfully applied to the previously unexplained relationship between carbon and silica in the ocean’s interior. Readers of this book will gain a comprehensive understanding of weathering as a reaction catalyzed by both plants and plankton, occurring not only on land but also ubiquitously in the earth’s environment, including the ocean’s interior. This new and novel perspective has significant implications for various scientific fields, including biology, marine chemistry, environmental, and paleoenvironmental sciences. The author underscores the immediate relevance of these findings to pressing issues surrounding atmospheric CO2. The book concludes with a proposal for an efficient and safe method to sequester CO2 in the atmosphere into the ocean interior, offering a practical solution to a global challenge. The target audience for this book includes students and researchers in ecology, evolutionary biology, geochemistry, environment and plant sciences, atmospheric sciences, and Geo-industries.

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