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256 pages, Hardcover
First published March 25, 2008
"First, the world warms over short intervals of time because of a sudden increase in carbon dioxide and methane, caused initially by the formation of vast volcanic provinces called flood basalts. The warmer world affects the ocean circulation systems and disrupts the position of the conveyor currents. Bottom waters begin to have warm, low-oxygen water dumped into them. Warming continues, and the decrease of equator-to-pole temperature differences reduces ocean winds and surface currents to a near standstill. Mixing of oxygenated surface waters with the deeper, and volumetrically increasing, low-oxygen bottom waters decreases, causing ever shallower water to change from oxygenated to anoxic. Finally, the bottom water is at depths where light can penetrate, and the combination of low oxygen and light allows green sulfur bacteria to expand in numbers and fill the low-oxygen shallows. They live amid other bacteria that produce toxic amounts of hydrogen sulfide, and the flux of this gas into the atmosphere is as much as 2,000 times what it is today. The gas rises into the high atmosphere, where it breaks down the ozone layer, and the subsequent increase in ultraviolet radiation from the sun kills much of the photosynthetic green plant phytoplankton. On its way up into the sky, the hydrogen sulfide also kills some plant and animal life, and the combination of high heat and hydrogen sulfide creates a mass extinction on land. These are the greenhouse extinctions."Ward identifies three different states of the ocean through time. The well mixed ocean of today, with animal life at all levels, is only present during the geologically short periods when there is permanent ice at the poles. The temperature difference between the equator and the poles is required drive the ocean circulation that oxygenates the deep ocean. In warmer times the temperature difference is less, ocean is more stratified, and the bottom layers are anoxic with little non-bacterial life. Throughout the long pre-Cambrian era the oceans were in a third state called a Canfield ocean, which is dominated by sulfur metabolizing bacteria. Ward's hypothesis is that the Canfield oceans return in response to greenhouse warming and cause mass extinctions. This leads to the question of whether the present greenhouse warming will eventually lead to the same result.