Seawater carbonate chemistry and community calcification during Shiraha coral reef (Ishigaki Island, Japan) studies, 1995

Only about half of all the CO_2 that has been produced by the burning of fossil fuels now remains in the atmosphere. The CO_2 "missing" from the atmosphere is the subject of an important debate. It was thought that the great majority of the missing CO_2 has invaded the ocean, for this system naturally acts as a giant chemical regulator of the atmosphere. Although it is clear that ocean processes have a major role in the regulation of the carbon dioxide content of the atmosphere through air-sea exchange processes, recent studies of the oceanic carbon cycle and air-sea interaction indicate that oceanic carbon is in a quasi-steady state via the system of biological and physical processes in the ocean interior. It is difficult to determine whether the ocean has the capacity to take up the increasing air-born CO_2 released by human activities over the past five or six decades. To understand this enigma, we need a better understanding of the natural variability of the oceanic carbon cycle.

Data and Resources

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Cite this as

Suzuki, Yoshimi (1995). Dataset: Seawater carbonate chemistry and community calcification during Shiraha coral reef (Ishigaki Island, Japan) studies, 1995. https://doi.org/10.1594/PANGAEA.721925

DOI retrieved: 1995

Additional Info

Field Value
Imported on December 1, 2024
Last update December 1, 2024
License CC-BY-3.0
Source https://doi.org/10.1594/PANGAEA.721925
Author Suzuki, Yoshimi
Given Name Yoshimi
Family Name Suzuki
Source Creation 1995
Publication Year 1995
Resource Type text/tab-separated-values - filename: C_chem_computation_Suzuki_1995
Subject Areas
Name: Chemistry

Related Identifiers
Title: The global carbon cycle and the role of the ocean
Type: DOI
Relation: References
Year: 1995
Source: Geoscience Reports of Shizuoka University
Authors: Suzuki Yoshimi .