Based on a century
of ocean plankton science and the 10 international experiments on iron fertilization over the last 15 years we are confident that the scale, methods and technologies of the work we are planning will have positive impacts on all fronts, improving water quality, buffering surface water acidity, recharging the marine food chain, and safely sequestering enormous amounts of CO2 to help slow climate change.
Whales are the gardeners and shepherds
of our ocean plankton pastures we need them they need us http://russgeorge.net/2013/04/10/whales-are-worms/
Not exact matches
June 6, 2013 — Spindle - shaped inclusions in three - billion - year - old rocks are microfossils
of plankton that probably inhabited the
oceans around the globe during that time, according to an international team
of researchers.
Now the flood is supposed to have happened about 4361 years ago (2013)[1] so that means that if we go down that number
of layers we should find on or about that layer evidence
of the flood in the form
of dead
plankton, salt, and other
ocean detritus.
But the instrumental value
of plankton for the whole system
of life in the
ocean is enormous.
Organic bivalve shellfish (mussels, clams, oysters) are fed by natural
plankton and algae in tidal zones, so this industry is relatively easy in clean
oceans, such as those near the south coast
of Australia, where there are already certified operators for mussels and oysters.
Juveniles lose the bright,
plankton - filtering gills seen on this individual when they mature and descend into some
of the deepest depths
of any known fish, often more than 5,000 meters (16,000 feet) beneath the
ocean surface.
Findings published today in the journal Nature Climate Change reveal that water temperature has a direct impact on maintaining the delicate
plankton ecosystem
of our
oceans.
Plankton plays an important role in the
ocean's carbon cycle by removing half
of all CO2 from the atmosphere during photosynthesis and storing it deep under the sea — isolated from the atmosphere for centuries.
When the weather warms and no ice sits upon the seas, the sediment on the
ocean floor is mainly organic: remains
of plankton and diatoms.
They reported this finding in July after analyzing 50 - plus years
of data on light penetration
of the
ocean surface and
plankton abundance in water samples.
Despite the size
of the bloom, however, the
plankton did not take in a record - breaking amount
of carbon dioxide — only about 20 % more carbon than that part
of the
ocean sequesters biologically each year.
Can any scientist who claims to be credible say such a thing in the face
of the long, published history
of plankton blooms in the open
ocean?
When areas
of the
ocean are low in iron, the
plankton population usually remains sparse.
The ash, it turned out, had fertilized the
ocean with thousands
of tons
of iron, on which the
plankton gorged.
Ocean chemist Philip Boyd
of the University
of Otago in New Zealand says many other researchers have tried to link an infusion
of iron from volcanic ash or even dust storms to
plankton blooms, but this study is the first to «verify such a massive event.»
It's coincidentally one
of the best - studied
ocean regions in the world, with data on
plankton going back over 50 years.
An international team
of scientists have discovered two new
plankton - eating fossil fish species
of the genus called Rhinconichthys (Rink - O - nik - thees) from the
oceans of the Cretaceous Period, about 92 million years ago, when dinosaurs roamed the planet.
Out
of the vast diversity
of plankton in the
oceans, the worst offenders are a few species
of diatoms, dinoflagellates and cyanobacteria, collectively called harmful algae.
While a professor at the University
of Kiel, Hensen led a detailed survey
of Atlantic
plankton — which include algae, bacteria, protozoans, crustaceans, mollusks, and coelenterates — that drift with
ocean currents.
Without the ozone layer, ultraviolet rays from the sun would reach the surface at nearly full force, causing skin cancer and, more seriously, killing off the tiny photosynthetic
plankton in the
ocean that provide oxygen to the atmosphere and bolster the bottom
of the food chain.
An international team
of scientists has discovered a new lineage
of extinct
plankton - feeding sharks, Pseudomegachasma, that lived in warm
oceans during the age
of the dinosaurs nearly 100 million years ago.
The
plankton that feed on the dust's minerals can bloom significantly, providing food for other
ocean creatures, but an overgrown bloom can consume much
of the dissolved oxygen in an area and create an anoxic dead zone.
Iron can fuel
plankton blooms and influence how the
ocean responds to climate change, while the lead images show the impact
of past pollution on the
ocean and continuing contamination in some parts
of the world and aluminium is used as a tracer
of desert dust inputs to the
ocean.
Sunlight that penetrates the ice is also critical for algae and
plankton of the Arctic
Ocean.
Scientists took nearly 200,000 water,
plankton, atmosphere particles and gases samples in 313 points
of the Indian, Pacific and Atlantic
Oceans at depths
of up to 6,000 meters.
Another high - profile test —
of dumping iron particles into the
ocean to stimulate
plankton growth — failed miserably after being disrupted by protesters.
You report on a successful trial
of ocean iron - seeding to promote
plankton growth and potential carbon sequestration via the sinking...
Your article on adding iron to patches
of ocean to encourage
plankton growth and so capture atmospheric carbon (21 July,...
AS THE world's fisheries ministers promised tough action to conserve the
oceans» fast - diminishing fish stocks last week, researchers were providing still more evidence
of a crisis that threatens everything from
plankton to porpoises.
Tiny
plankton and bits
of plastic commingle in this water sample taken in the vicinity
of the so - called «Great Pacific Garbage Patch,» a large area in the North Pacific
Ocean known for accumulations
of plastic marine debris.
The working group on coupled biogeochemical cycling and controlling factors dealt with questions regarding the role
of plankton diversity, how
ocean biogeochemistry will respond to global changes on decadal to centennial time scales, the key biogeochemical links between the
ocean, atmosphere, and climate, and the role
of estuaries, shelves, and marginal seas in the capturing, transformation, and exchange
of terrestrial and open - marine material.
The shale, named for the town
of Eagle Ford, TX, is a geologic remnant
of the ancient
ocean that covered present day Texas millions
of years ago, when the remains
of sea life (especially ancient
plankton) died and deposited onto the seafloor, were buried by several hundred feet
of sediment, eventually turning into the rich source
of hydrocarbons we have today.The shale was first tapped in 2008 and now has around 20 active fields good producing over 900 million cubic feet per day
of natural gas.
Phosphorus is an essential nutrient that feeds
plankton at the base
of the
ocean food web.
Today's
ocean models typically take an «either / or» approach, grouping
plankton as either photosynthesizers or consumers
of prey.
The scientists developed a mixotrophic model
of the global
ocean food web, at the scale
of marine
plankton, in which they gave each
plankton class the ability to both photosynthesize and consume prey.
Typical
ocean models that incorporate
plankton often group them in 10 general size classes, each
of which fall into a «two - guild» structure, as either photosynthesizers, or consumers
of prey.
These more substantial organisms, compared to smaller and lighter
plankton, were more capable
of sinking to the
ocean floor, as carbon - containing detritus.
The
plankton incorporate different forms
of boron into their shells, depending on the seawater's acidity, so each shell serves as a chemical record
of the
ocean's pH during its occupant's brief life.
But invisible changes may be the most threatening to human food sources, beginning with the tiny species like
plankton that inhabit the bottom
of the
oceans» food chain.
New genetic analyses
of tropical marine microorganisms have revealed that some species
of single - celled
plankton are converting significant amounts
of nitrogen from the air into nutrients, helping to fortify the base
of the
ocean's food pyramid.
By detecting the molecular machinery used by the
plankton to create one
of the enzymes needed to split nitrogen molecules apart, scientists appear to have discovered a new microbial source
of the
ocean's nitrogen - bearing nutrients.
Iron - rich sediment from deserts feeds
plankton blooms in the
ocean and plants in the upper canopy
of tropical rain forests.
For one
of them, you can thank
plankton, in particular the single - celled photosynthetic drifters that comprise the phytoplankton
of the world's
oceans.
A wide range
of smartphone apps could allow citizens to do everything from monitoring air and water quality to tracking
ocean plankton populations from space.
The question
of how Trichodesmium cyanobacteria are reacting to the changing
ocean makes a big difference in predicting how other marine life, from whales to mere specks
of floating
plankton, will react, too.
In places like the North Atlantic, where
plankton bloom lushly in the spring, oceanographers find patches
of green stuff on the
ocean bed, a mile or two below.
At any one time, an estimated 7 billion tonnes
of ballast water is crossing the
oceans — almost all
of it carrying seeds, spores, eggs, larvae, bacteria and
plankton native to wherever the water was loaded.
Across the world's
oceans, seas and coasts, tens
of millions
of tonnes
of it are released by microbes that live near
plankton and marine plants, including seaweeds and some salt - marsh grasses.
The same mechanism would likely also mobilize and deliver more nutrients, carbon, and other chemicals into the Arctic
Ocean, fueling the growth
of plankton at the bottom
of the food chain.