One problem is that researchers haven't been
studying ocean oxygen levels that long, so there isn't an extensive history of data collection to draw on.
Not exact matches
Curtis Deutsch, associate professor at the University of Washington's School of Oceanography,
studies how increasing global temperatures are altering the
levels of dissolved
oxygen in the world's
oceans.
That is the conclusion of a
study simulating a little - discussed consequence of climate change: it could choke entire ecosystems by cutting
oxygen levels in the
ocean.
It is perfectly possible that sponges came before, and helped bring about, fully oxygenated
oceans, says Timothy Lyons at the University of California, Riverside, who
studies the variation in
oxygen levels on early Earth.
A new
study found that vulnerability of deep - sea biodiversity to climate change's triple threat — rising water temperatures, and decreased
oxygen, and pH
levels — is not uniform across the world's
oceans.
A
study of the 15 - mile length of Coos Bay, from the
ocean to the city of the same name, finds the bay is free of toxic
levels of reduced
oxygen that often affect other Oregon locations.
Previous research has shown that global warming will cause changes in
ocean temperatures, sea ice extent, salinity, and
oxygen levels, among other impacts, that are likely to lead to significant shifts in the distribution range and productivity of marine species, the
study notes.
The
study, published in the journal Nature Communications, tender geochemical evidence that a rise in
oxygen levels in the
oceans coincided with the appearance of complex animals.
Rising
levels of
oxygen in the
oceans were a key causative factor in the emergence of skeletal animals 550 million years ago, according to a new
study.
(Fingerprint
studies draw conclusions about human causation that can be deduced from: (a) how the Earth warms in the upper and lower atmosphere, (b) warming in the
oceans, (c) night - time vs day - time temperature increases, (d) energy escaping from the upper atmosphere versus energy trapped, (e) isotopes of CO2 in the atmosphere and coral that distinguish fossil CO2 from non-fossil CO2, (f) the height of the boundary between the lower and upper atmosphere, and (g) atmospheric
oxygen levels decrease as CO2
levels increase.