Read / Purchase the Report Ocean Acidification: A National Strategy to Meet the Challenges of A Changing Ocean (2010) Excess carbon dioxide in the atmosphere — in addition to contributing to climate change — is absorbed by the ocean, making sea water more acidic and leading to a suite
of changes in ocean chemistry.
Excess carbon dioxide in the atmosphere — in addition to contributing to climate change — is absorbed by the ocean, making sea water more acidic and leading to a suite
of changes in ocean chemistry.
Not exact matches
Now, a 15 - year, 30 - nation research collective called Geotraces is embarking on an ambitious global survey
of ocean chemistry to quantify trace elements and shed light on how chemical concentrations fluctuate
in response to
changing environmental conditions.
This means that the sudden appearance
of rangeomorphs at large size could have been a direct result
of major
changes in climate and
ocean chemistry.
«When tiny bacteria
in the
ocean began producing oxygen, it was a major turning point and
changed the
chemistry of the Earth,» explained Katsev.
Instead, the team points out that similar swings
in different isotopes» levels, occurring
in both parts
of the world, suggest that the two regions were experiencing the same
changes in ocean chemistry at the same time.
At a global level, the excess
of atmospheric CO2 is absorbed by
ocean waters and it causes
changes in water
chemistry (pH decrease or
ocean acidification).
Scientists conducting fieldwork
in the region are reporting massive chick die - offs and nests with abandoned eggs, reports National Geographic's Winged Warnings series, which lays out the many threats facing the island's seabirds: warming
oceans, earlier thaws,
changing ocean chemistry and food webs, and increasing levels
of ocean pollutants from PCBs to mercury.
«
Changes to the chemistry of the Arctic Ocean could lead to changes in currents and weather patterns worldwide,» h
Changes to the
chemistry of the Arctic
Ocean could lead to
changes in currents and weather patterns worldwide,» h
changes in currents and weather patterns worldwide,» he said.
As atmospheric CO2 levels rise, those
in the
oceans do too,
changing the
chemistry of the seawater.
By studying the
chemistry of growth rings
in the shells
of the quahog clam, an international team led by experts from Cardiff University and Bangor University have pieced together the history
of the North Atlantic
Ocean over the past 1000 years and discovered how its role
in driving the atmospheric climate has drastically
changed.
The
chemistry in the growth rings
in the shells
of the clam — which occur much like the annual growth rings
in the centre
of trees — can act as a proxy for the chemical make - up
of the
oceans, enabling researchers to reconstruct a history
of how the
oceans have
changed over the past 1000 years with unprecedented dating precision.
A McGill - led international research team has now completed the first global study
of changes that occurred
in a crucial component
of ocean chemistry, the nitrogen cycle, at the end
of the last ice age.
Enter the toy octopus: A team
of researchers
in California is exploring how the
changing ocean chemistry affects a hermit crab's fight - or - flight response by simulating octopus attacks
in the laboratory.
Seagrasses also undergo a high rate
of photosynthesis that may serve to buffer
changes in ocean chemistry that affect shell - building organisms.
The team analyzed little studied factors that play a role
in ocean acidification (OA)--
changes in water
chemistry that threaten the ability
of shellfish such as oysters, clams and scallops to create and maintain their shells, among other impacts.
Beyond the sea level rise itself, the ancient geologic and geographic
changes probably led to a buildup
of oxygen
in the atmosphere and a
change in ocean chemistry, allowing more complex life - forms to evolve, he said.
How are humans driving
changes in the
chemistry of the
ocean, and what might this mean for marine ecosystems
in the future?
«The other carbon dioxide problem», «the evil twin
of global warming», or part
of a «deadly trio», together with increasing temperatures and loss
of oxygen: Many names have been coined to describe the problem
of ocean acidification — a
change in the
ocean chemistry that occurs when carbon dioxide (CO2) from the atmosphere dissolves
in seawater.
Such priorities include: 1) establishing an
ocean carbon
chemistry baseline; 2) establishing ecological baselines; 3) determining species / habitat / community sensitivity to
ocean acidification; 4) projecting
changes in seawater carbonate
chemistry; and 5) identifying potentially synergistic effects
of multiple stressors.
ref Such
changes in the carbon
chemistry of the open
ocean probably have not occurred for more than 20 million years.
ref It will also be important to encourage socioeconomic research on the impacts
of ocean acidification, the projected timing
of impacts, and the ways to increase adaptability and resilience
of socioeconomic systems
in the face
of changing ocean chemistry.
Oceanic uptake
of anthropogenic carbon dioxide (CO2) causes pronounced shifts
in marine carbonate
chemistry and a decrease
in seawater pH. Increasing evidence indicates that these
changes — summarized by the term
ocean acidification (OA)-- can significantly affect marine food webs and biogeochemical cycles.
The South China Sea (SCS) is said to be
ocean - dominated at depth, and its CaCO3 records should reflect and preserve the effects of changes in the carbonate chemistry of the (western) Pacific O
ocean - dominated at depth, and its CaCO3 records should reflect and preserve the effects
of changes in the carbonate
chemistry of the (western) Pacific
OceanOcean.
We also have modellers that project future
changes of ocean chemistry and biology
in the next decades and century.
«Documenting an effect
of OA [
ocean acidification] involves showing a
change in a species (e.g. population abundance or distribution) as a consequence
of anthropogenic
changes in marine carbonate
chemistry.
The carbon dioxide buildup is
changing the
chemistry of surface seawater, lowering its pH
in a way that,
in theory, could be harmful to the shell - forming and reef - forming marine organisms
of today's
ocean ecosystem.
There's plenty more
in the report summary,
of course, on everything from
changes in sea ice to
ocean chemistry.
Hales» pioneering research
in ocean carbon
chemistry underlies much
of what we know about the role carbon dioxide from fossil fuel emissions plays
in changing the
chemistry of Northwest seas.
Even with almost no chance
of the high end
of climate sensitivity estimates being right, the odds
of substantial, prolonged and disruptive climate
change (and
changes in ocean chemistry) are still plenty high enough to justify a sustained push toward an energy menu that works for the long haul.
Climate
change, rising atmospheric carbon dioxide, excess nutrient inputs, and pollution
in its many forms are fundamentally altering the
chemistry of the
ocean, often on a global scale and,
in some cases, at rates greatly exceeding those
in the historical and recent geological record.
Changes in the
ocean,
ocean chemistry and biology on land and
ocean need a lot
of study.
This
change in ocean chemistry can strip away the building blocks
of coral reefs, weakening an important link
in the oceanic food chain.
It's been enough to raise the levels
of the
ocean — and the extra carbon
in the atmosphere has also
changed the
chemistry of that seawater, making it more acidic and beginning to threaten the base
of the marine food chain.
«I've been surprised by the scarcity
of direct data on the
changes in pH and
ocean chemistry more generally.
The
ocean uptake
of excess atmospheric carbon dioxide, the excess above preindustrial levels driven by human emissions, causes well - understood and substantial
changes in seawater
chemistry that can affect marine organisms and ecosystems.
The rate
of that process reacts rather weakly to modest
changes in pH and that
change affects the
ocean chemistry significantly only on very long term.
As long as I have tried to learn about
ocean acidification I've been surprised by the scarcity
of direct data on the
changes in pH and
ocean chemistry more generally.
It will be harder to get such a clear sign
in a shell from other
ocean regions — as variables like temperature and the amount
of minerals available can significantly
change the
chemistry of a given
ocean region.
«We knew there were
changes in carbonate
chemistry of the surface
ocean associated with the large - scale glacial - interglacial cycles
in CO2 [levels], and that these past
changes were
of similar magnitude to the anthropogenic
changes we are seeing now,» says study co-author William Howard, a marine geologist at ACE.
Finding a way to reverse climate
change is the foremost challenge
of our time and the first step is collecting
ocean data
in order to help us understand how seawater
chemistry is
changing.
While scientific models can tell us what is going to happen as the earth warms, climate
change will also be influenced by small so far neglected fluctuations
in chemistry such as these pH
changes in our
oceans, affecting billions
of creatures, and
of course, us.
IANS: Climate
change is causing toxic metals trapped
in the sediment beds
of the Hooghly estuary
in the Indian Sunderbans to leach out into the water system due to
changes in ocean chemistry, say scientists, warning
of potential human health hazards.
There is a risk that small
changes in the radiative properties
of the atmosphere,
in terrestrial hydrology and
in ocean chemistry can trigger large responses
in the Earth system.
But the
change in carbon
chemistry of the
ocean and ultimately the atmosphere need to be transparently documented, also, if we are to trade carbon offsets based on iron fertilization.
Changes in ocean chemistry, which can be described through the Revelle buffer factor [1], limit oceanic removal
of CO2 [2], while the potential for terrestrial vegetation to take up CO2 is also predicted by some models to fall as the climate warms [3], although the size
of this feedback is uncertain [4].
And the
changes in ocean chemistry are the sort
of thing that can be expected to have a direct effect on the geological record if carbon levels rise far enough.
«
Ocean acidification» (OA), a
change in seawater
chemistry driven by increased uptake
of atmospheric CO2 by the
oceans, has probably been the most - studied single topic
in marine science
in recent times.
Accumulating strong evidence suggests that these
changes in ocean temperature and
chemistry, including pH, will likely affect major Alaska marine fisheries, although the relative importance
of these
changes and the exact nature
of response
of each fishery are uncertain.16, 17,18,122,19,20,21
Current and projected increases
in Alaska's
ocean temperatures and
changes in ocean chemistry are expected to alter the distribution and productivity
of Alaska's marine fisheries, which lead the U.S.
in commercial value.