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?
From June to September, the whale shark population takes advantage of the large amounts
of plankton in the water.
In some areas, the amount of plastic outweighs the
amount of plankton by a ratio of six to one.
If several important
species of plankton thrive as a result of more carbon dioxide, that's fabulous.
The result is changes in the distribution and
abundance of plankton species, as well as shifts in their seasonal cycles.3 For example, in the northeast Atlantic, both warmer - water and colder - water plankton moved 10 ° latitude farther north over a four - decade period at the end of the twentieth century.3, 8
In this study we combined results from various in - situ mesocosm studies in two different ocean regions (Arctic and temperate waters) to reveal general patterns
of plankton community shifts in response to OA and how these changes are modulated by inorganic nutrient availability.
While some
types of plankton bloomed 30 days earlier at the beginning of this century than in the middle of the twentieth century, other types maintained their seasonal cycles throughout that period.7 Mismatches in marine communities and disruption of the food chain are the result.
In some areas, the amount of plastic outweighs the amount
of plankton by a ratio of six to one.
More fresh water in the surface water layers makes it harder for the nutrient - rich bottom water to rise to the upper layers where the sunlight ensures the
production of plankton algae in summer.
So while warmer oceans and a more fertile atmosphere might accelerate some
kinds of plankton bloom, the seas could become too acidic for tropical micro-organisms.
It seems likely that depletion of the ozone layer near the PETM led to a
loss of plankton and resulting collapse of marine ecosystems.
A
lot of plankton attracts a lot of tiny creatures that come to feed on them.
The nutrient could stimulate growth
of plankton at the base of the ocean food web that could impact birds, fish and marine mammals higher up the food chain.
The simulated ocean acidification led to unexpectedly large changes in the production activity
of the plankton with considerable impacts on the release of climate - relevant gases and in turnover rates of important elements in the seawater.
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.
Another problem with your suggestion (again this is just my opinion) is that you say «significant
number of plankton species».
During the summer months (June to September) hundreds of whale sharks gather just north of Isla Mujeres in a seven mile radius to take advantage
of the plankton rich waters created by the joining of the Gulf of Mexico and the Caribbean Sea.
Ask the students to take notes on what they learn about the critical role
of plankton as they view the video.
Whale sharks feed on the tiny
bits of plankton and swarm the area where the Caribbean Sea and Gulf of Mexico waters combine.
But the instrumental
value of plankton for the whole system of life in the ocean is enormous.
In turn, killer whales that feed on seals consume the equivalent of five tons
of plankton for each pound of their body weight.12 This phenomenon would explain why Weston Price found seal oil, which he estimated to constitute 200 calories per day of the Inuit diet, to be several times higher in the fat - soluble vitamins than ordinary cod liver oil.30
The metabolic activity and genetic diversity peaked around sea floor layers packed with the
remains of plankton called diatoms, which presumably provide the carbon and other nutrients for the more complex ecology.
But dictating the species
composition of a plankton bloom and its aftermath remains beyond the ken of marine biology, causing one researcher involved in the successful 2004 effort, marine biologist Victor Smetacek of the Alfred Wegener Institute for Polar and Marine Research in Germany, to call it beyond control at this stage.
According to a 2006 report from the U.N. Environment Programme, every
pound of plankton in the central Pacific Ocean is offset by about 6 pounds of litter.
Greater numbers of bugs could also deplete
populations of the plankton they feed on, throwing a wrench into the ecosystem, Goldstein adds.
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.
Local factors such as ocean streams, temperature, depth, and acidity determine the composition
of plankton ecosystems, Karsenti said.
Minute organisms originating in the mangroves may be blown offshore and become
part of the plankton which attracts such pelagics as the manta ray and the whale shark.
In 1956 the carbon - 14 expert Hans Suess, studying the
shells of plankton embedded in cores of clay pulled from the seabed by Columbia University's Lamont Geological Observatory, discovered a change at the fastest speed that anyone expected.
«Different teams investigate the development and
productivity of the plankton community, changes in the food web, in the material and energy cycles and in the production of climate - active gases», Riebesell describes the wide range of scientific questions addressed in this mesocosm campaign.
Because of their physical characteristics and strong localized currents, they accumulate enormous
quantities of plankton.
In an unprecedented long - term experiment, 69 scientists from 12 European research institutes and universities studied the
development of the plankton community and fish larvae in acidified waters.
Six, K.D., and E. Maier - Reimer, 1996: Effects
of plankton dynamics on seasonal carbon fluxes in an ocean general circulation model.
By feeding on fish, seals consume the equivalent of half a
ton of plankton to produce each pound of their body weight.
Despite the fact that they appear huge, they are quite amazing sea creatures and count on their staple
diet of plankton.
The
upwelling of plankton rich cooler water at this deeper site means it is a good place for larger pelagics.
Thousands of seagoing scientists have collected
millions of plankton observations that can provide us with a deeper understanding of marine plankton trends.
Although there are lots of dive sites in Thailand where you can see whale sharks, the nutrient rich waters contain loads
of planktons which attracts whale sharks all the time.
But we reject the view that this limits our knowledge
of plankton trends to the satellite era (1979 - 86, 1997 - present).
Now, though, a new laboratory study has shown that some types
of plankton thrive in water with a low pH created by greatly raising concentrations of carbon dioxide.