Most climate change scenarios foresee a shift or expansion of the ranges of many
species of plankton, fish and invertebrates towards higher latitudes, by tens of kilometres per decade, contributing to changes in species richness and altered community composition.
If our climate continues to warm at today's rate, scientists expect North Sea plankton that respond to temperature cues to bloom even earlier in the coming decades.7 With a growing mismatch in life cycles among various
species of plankton, as well as further climate - induced shifts in their abundance and distribution, effects on the North Sea ecosystem — including cod — are projected to be considerable.7, 8
If several important
species of plankton thrive as a result of more carbon dioxide, that's fabulous.
Researcher Peter Ross and his colleagues found plastic litter in the digestive systems of two key
species of plankton that are eaten in large numbers by salmon and baleen whales.
Not exact matches
If we had to choose between the survival
of whales as a
species and that
of plankton, we would rightly choose the
plankton.
The
species, native to the Caspian and Black Sea basins, was well known on that side
of the Atlantic for its ability to fuse to any hard surface, growing in wickedly sharp clusters that can bloody boaters» hands and swimmers» feet, plug pipes, foul boat bottoms and suck the
plankton — the life — out
of the waters they invade.
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.
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.
Tamara Shiganova
of the Russian Academy
of Sciences noted that two
species — one apparently native and the other introduced from the western Atlantic — now appear in often alternating blooms, vacuuming up the
plankton that feeds young fish.
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.
Taxonomists are cleaning up and adding to the book
of life on hundreds
of thousands
of known marine
species — from
plankton to sperm whales
One reason is that the nutrients and
plankton in the waters
of the Great Lakes are not merely limited, they are crashing, due to a different exotic
species, the zebra mussel, and its cousin, the quagga mussel, two invaders that stowed on ships from Europe in the 1980s.
When these
species invade, they reduce the amount
of plankton available to feed native fish.
In recent years, an algae - filled
plankton species has been changing the ecology
of these waters.
One
of the key findings from the research expedition is that temperature shapes which
species are present in a given
plankton ecosystem, a fact that could take on increasing importance in the face
of climate change.
Gipsi Lima - Mendez
of the University
of Leuven in Belgium, and a senior author on another study in the Tara package, and colleagues developed a map
of more than 90,000
plankton species interactions.
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.
Stout infantfish were captured in a
plankton net on the Great Barrier Reef in Australia by a field researcher in 1979, then overlooked for more than two decades until H. J. Walker, a senior museum scientist at the Scripps Institution
of Oceanography, and William Watson
of the National Marine Fisheries Service, realized they were an unknown
species.
Plankton species, the foundation
of the marine food web, have shifted back slightly toward fat - rich, cool - water
species that improve the growth and survival
of salmon and other fish.
With warmer equatorial waters reducing
plankton abundance and spurring many fish
species, notably bigeye and skipjack tuna, to migrate toward the poles, the waters around Wake and Johnston, 1600 kilometers north
of the equator, «are precisely where you want to have a protected area,» says Robert Richmond
of the University
of Hawaii at Mānoa.
Besides Planktophaga minuta (which translates to small
plankton eater), an additional six
species of carp have been discovered in Lake RhinChua.
To test this, Rick Relyea, a biologist at the University
of Pittsburg in Pennsylvania, simulated a pond ecosystem by filling 1000 - liter tanks with well water,
plankton, various tadpole
species, and other organisms at the same densities found in nature.
The report found that ocean warming is affecting a multitude
of ocean processes, including breeding and migration patterns
of ocean
species such as
plankton, whales and fish.
In a study published today in the journal Nature Climate Change, the researchers report that increased ocean acidification by 2100 will spur a range
of responses in phytoplankton: Some
species will die out, while others will flourish, changing the balance
of plankton species around the world.
Ammonites, which were free - swimming molluscs
of the ancient oceans and are common fossils, went extinct at the time
of the end - Cretaceous asteroid impact, as did more than 90 per cent
of species of calcium carbonate - shelled
plankton (coccolithophores and foraminifera).
From microscopic
plankton to
species» interactions in the marine ecosystem and from elemental biogeochemical cycling to the consequences for economy and society: The German project BIOACID (Biological Impacts
of Ocean Acidification) analyses the problem
of ocean acidification in its entire spectrum.
The new research published in the journal Science Advances examined the skin cells
of common dolphins for chemical clues about the length
of the marine food chain, which begins with tiny
plankton and continues as
species eat them, and other
species eat those
species.
«While many branching corals dominate under normal pH conditions offering ample hiding space for the different
species of zooplankton, ocean acidification shifts the community to large, massive bouldering corals, which offer the reef - associated
plankton little opportunity for hiding».
The
plankton, in turn, attracts a vast array
of marine life, providing feeding as well as spawning grounds for myriad pelagic
species, including some that have migrated across wide oceanic areas.
SEE ALSO Algal Blooms, Harmful; Algal Blooms in the Ocean; Carbon Dioxide in the Ocean and Atmosphere; El NiÑo and La NiÑA; Food from the Sea; Life in Extreme Water Environments; Human Health and the Ocean; Human Health and Water; Ocean Biogeochemistry; Ocean Currents;
Plankton; Pollution by Invasive
Species; Pollution
of the Ocean by Sewage, Nutrients, AND Chemicals.
At the start
of the experiment in late September, the conditions were truly oligotrophic: «The nutrient concentrations were hardly above the detection limit, and the
plankton community was dominated by tiny algal cells and microzooplankton
species.
The
plankton - rich waters are home to a number
of species of fish, sea turtles, and even whales.
There are several popular diving sites around Muscat because
of the water being
Plankton - rich and attracting several
species of fish..
Elsewhere in the oceans, the environmental changes during the PETM led to shifts in the distribution
of plankton groups, with tropical
species invading the high latitudes and high - latitude
species dwindling in abundance.
The
species is an extinct form
of dinoflagellate — a group
of single - celled
plankton, some
of which today give rise to toxic blooms known as red tides.
At least one past global hot spell widely attributed to a natural spike in greenhouse gases, the Paleocene - Eocene Thermal Maximum 55.8 million years ago, appeared to cause a mass die - off
of some marine
plankton, but other forms thrived, as did mammals and other terrestrial
species, specialists on that period say.
I wonder, given the recent news about the various ways
plankton actively affect the oceans, including churning the upper 100 meters, if any
of the cycles could reflect big changes in which
species predominate over time.
We don't have good information on the base
of the food chain for most
of the past — that's just «noise» but now that we start having ways to track trends in primary productivity — what's being made out
of sunlight, water and CO2, by which organisms, and how fast do their populations change (remembering that some
plankton populations turn over a new generation in a couple
of weeks so relative numbers
of different
species can change that fast across the oceans).
Modern
plankton foraminifera become inhibited below pH 7.6 - 7.8, thus only if some
of these
species recover their ability to grow in less alkaline, CO2 - rich waters, then there will be no problem over the centuries to come.
Other aspects
of global warming's broad footprint on the world's ecosystems include changes in the abundance
of more than 80 percent
of the thousands
of species included in population studies; major poleward shifts in living ranges as warm regions become hot, and cold regions become warmer; major increases (in the south) and decreases (in the north)
of the abundance
of plankton, which forms the critical base
of the ocean's food chain; the transformation
of previously innocuous insect
species like the Aspen leaf miner into pests that have damaged millions
of acres
of forest; and an increase in the range and abundance
of human pathogens like the cholera - causing bacteria Vibrio, the mosquito - borne dengue virus, and the ticks that carry Lyme disease - causing bacteria.
«Southern Ocean acidification via anthropogenic CO2 uptake is expected to be detrimental to multiple calcifying
plankton species by lowering the concentration
of carbonate ion (CO32 − to levels where calcium carbonate (both aragonite and calcite) shells begin to dissolve.
Warming
of the North Sea and its effects on
plankton can influence commercially important
species further along the food chain that rely on
plankton for food.
Plankton forms the main food
of many ocean
species, and fisheries could be badly hit by the loss
of these micro-organisms as a result
of warmer waters, according to the paper, published this week in the British journal Nature... Other factors that influence phytoplankton growth include [iron] dust blown from the land, and variations in solar radiation.
The loss
of sea ice changes ecosystems, opening the door to invasive
species, and alters habitat and
plankton blooms, affecting Alaska's commercial fishing industry, which leads the United States in the value
of its catch.
Acidity reduces the capacity
of key
plankton species and shelled animals to form and maintain shells and other hard parts, and therefore alters the food available to important fish
species.136, 139,140 The rising acidity will have particularly strong societal effects on the Bering Sea on Alaska's west coast because
of its high - productivity commercial and subsistence fisheries.17, 141
Increased carbon dioxide has already lowered the pH
of the surface ocean; this is expected to have a negative effect on survival
of plankton, the base
of the marine food chain, and the growth and health
of corals, which form biodiverse reefs in shallow waters
of the Hawaiian Islands and Florida, and deep reefs in Alaska and the Southeast U.S. Invasive
species are increasingly being recognized.
Areas occupied by marine
species including fish, corals and
plankton are moving by an average
of 72 kilometers (45 miles) a decade, typically toward the poles, the study by researchers at 17 institutions in 8 countries said today.
ArcOD has begun such research, barcoding 360 Arctic
species of benthos,
plankton, and fish, many from Alaska [322].
That puts we humans in the position
of competing directly with whales and all the other
plankton grazers, even endangered
species.