OCEAN 210 Lecture 10: Radiocarbon

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School
Department
Course
Ocean 210
Lecture 10
Radiocarbon
All diagrams taken from "Ocn210_topic1_lect4.ppt" on the course Canvas website or
created by me.
Half life
Half-life: the time it takes an initial concentration to decay by half
14C has a half life of approx. 5000 years
This can be used to determine deep-ocean water age
Radiocarbon
Pacific deep ocean water is much older than Atlantic water
Tells us how the water in the ocean moves and circulates
Enters the deep ocean in the North Atlantic and moves southward until it reaches
Antarctica and moves northward through the Pacific
Biological Productivity
Dissolved Phosphorus Profile
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