Lesson 32 Mineral Cycling - Alaska Geobotany Center
Lesson 32 Mineral Cycling - Alaska Geobotany Center
Lesson 32 Mineral Cycling - Alaska Geobotany Center
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A sedimentary cycle: the phosphorus cycle<br />
• Marine sediments and<br />
volcanic apatite are the<br />
source of P in phosphate<br />
rocks and soils.<br />
• P is taken up by plants as<br />
H 2 PO - 4 or HPO -2 4 , where it<br />
becomes a component of<br />
energy-carrying phosphate<br />
compounds (ATP and ADP),<br />
nucleic acids, several<br />
essential coenzymes, and<br />
phospholipids.<br />
http://arnica.csustan.edu/carosella<br />
/Biol4050W03/figures/phosphoru<br />
s_cycle.htm<br />
• Chemical erosion has<br />
reduced P 2 O 5 content of<br />
midwest soils by 36% in the<br />
last 50 y.<br />
Odum and Odum 1959