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Full Description
This title includes a number of Open Access chapters.
This valuable compendium provides an overview of the variables and consequences of oceanic carbon cycling in the context of climate change. The chapters highlight the importance of marine plankton in carbon processing as well as the effects of rising CO2 and temperature in their functioning.
Marine ecosystems are being increasingly threatened by growing human pressures, including climate change. Understanding the consequences that climate change may have is crucial to predict the future of our oceans. Rising temperatures and ocean acidification may profoundly alter the mode of matter and energy transformation in marine ecosystems, which could have irreversible consequences for our planet on ecological timescales. For that reason, the scientific community has engaged in the grand challenge of studying the variables and consequences of oceanic carbon cycling in the context of climate change, which has emerged as a relevant field of science.
The book is broken into four sections:
Understanding the Importance of Ocean Biogeochemistry
Quantifying Oceanic Carbon Variables
Phytoplankton and Oceanic Carbon Cycle
Ocean Acidification
Edited by a researcher with many years of experience and with contributions from scientists from around the world, this volume explores the most important topics on climate change and oceanic carbon cycling.
Contents
Grand Challenges in Marine Biogeochemistry. A Statistical Gap-Filling Method to Interpolate Global Monthly Surface Ocean Carbon Dioxide Data. The Seasonal Sea-Ice Zone in the Glacial Southern Ocean as a Carbon Sink. On the Influence of Interseasonal Sea Surface Temperature on Surface Water pCO2 at 49.0oN/16.5oW and 56.5oN/52.6oW in the North Atlantic Ocean. Carbon Export by Small Particles in the Norwegian Sea. Ubiquitous Healthy Diatoms in the Deep Sea Confirm Deep Carbon Injection by the Biological Pump. Carbon Export Efficiency and Phytoplankton Community Composition in the Atlantic Sector of the Arctic Ocean. Ocean Warming-Acidification Synergism Undermines Dissolved Organic Matter Assembly. Ocean Acidification with (De)Eutrophication Will Alter Future Phytoplankton Growth and Succession. Coccolithophore Calcification Response to Past Ocean Acidification and Climate Change. Near-Shore Antarctic pH Variability has Implications for the Design of Ocean Acidification Experiments.
