Seawater carbonate chemistry and calcification in the Bahama Bank, 1964-1965
Carbon dioxide is lost from the ocean by calcium carbonate precipitation (-p), photosynthesis (-b) and gas evasion at the sea surface (-g). Among the most active sites are warm shallow seas. In this paper seasonal studies on the Great Bahama Bank relate these processes in an equation which takes int...
Main Author: | |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1967
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.755149 https://doi.org/10.1594/PANGAEA.755149 |