The latest results come at a time when scientists are already reconsidering what was happening to
ocean oxygen levels during this crucial period.
Not exact matches
Researchers analyzed the
levels of various trace elements in hundreds of samples of carbon - rich shales that had been deposited in
oxygen - poor regions of the
ocean surrounding ancient continents
during the past 3.5 billion years.
Mild
oxygen levels in shallow seas but
oxygen - poor deep
oceans lasted for some 1.3 billion years
during a time that has been dubbed the «Boring Billion» but eventually led to the development of mitochondria that now power multicellular planet and animal life (Nick Lane, New Scientist, February 10, 2010; Rachel Ehrenberg, Science News, September 29, 2009; Johnston et al, 2009; and H.D. Holland, 2006).
This has potentially broad implications sulfate and
oxygen levels in the
oceans during this time, for the our understanding of Earth's ancient ecosystems.
Add the facts in trend: The
oceans are acidifying, The climate has already shifted 4 degrees of latitude in the past 30 years; the Arctic will likely be virtually ice free
during the summer melt within the decade, all the uncertainty ranges are positive and none of them are negative, CO2 is plant food, but what does that mean when the
oxygen levels are dropping, the Hoover dam is supposed to shut down in 2023 due to no water (latitudinal shift), the Yangtze in China is getting very low, etc. etc..
Enhanced nutrient
levels thus increased
ocean production in the surface and
oxygen consumption in the deep
ocean, causing ~ 50 % and at least 40 % of the
ocean volume to become dysoxic / anoxic
during OAE 1a and OAE 2 respectively.