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Oxygen : A Four Billion Year History / Donald Eugene Canfield.

By: Series: Science essentials (National Academy of Sciences (U.S.))Publisher: Princeton : Princeton University Press, [2014] Copyright date: �2014Description: xv, 196 pages : illustrations (some color) ; 24 cmContent type:
  • text
Media type:
  • unmediated
Carrier type:
  • volume
ISBN:
  • 9780691145020 (hbk. : alk. paper)
  • 0691145024 (hbk. : alk. paper)
Subject(s): LOC classification:
  • QD181.O1 .C36 2014
Contents:
What is it about planet Earth? -- Life before oxygen -- Evolution of oxygenic photosynthesis -- Cyanobacteria: the great liberators -- What controls atmospheric oxygen concentrations? -- The early history of atmospheric oxygen: biological evidence -- The early history of atmospheric oxygen: geological evidence -- The great oxidation -- Earth's Middle Ages: what came after the GOE -- Neoproterozoic oxygen and the rise of animals -- Phanerozoic oxygen -- Epilogue.
Awards:
  • ASLI Choice Award
Summary: "The air we breathe is twenty-one percent oxygen, an amount higher than on any other known world. While we may take our air for granted, Earth was not always an oxygenated planet. How did it become this way? Oxygen is the most current account of the history of atmospheric oxygen on Earth"-- Provided by publisher.
Holdings
Item type Current library Call number Copy number Status Date due Barcode Item holds
BOOK BOOK NCAR Library Mesa Lab QD181 .O1 .C36 2014 1 Available 50583020005959
Total holds: 0

Includes bibliographical references (pages 175-188) and index.

What is it about planet Earth? -- Life before oxygen -- Evolution of oxygenic photosynthesis -- Cyanobacteria: the great liberators -- What controls atmospheric oxygen concentrations? -- The early history of atmospheric oxygen: biological evidence -- The early history of atmospheric oxygen: geological evidence -- The great oxidation -- Earth's Middle Ages: what came after the GOE -- Neoproterozoic oxygen and the rise of animals -- Phanerozoic oxygen -- Epilogue.

"The air we breathe is twenty-one percent oxygen, an amount higher than on any other known world. While we may take our air for granted, Earth was not always an oxygenated planet. How did it become this way? Oxygen is the most current account of the history of atmospheric oxygen on Earth"-- Provided by publisher.

ASLI Choice Award

Questions? Email library@ucar.edu.

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