Not exact matches
Other
living organisms indicating the Earth is far more than a few thousands of years old include Posidonia oceanica, a species of seagrass found in the Mediterranean
Sea.
The team analysed the chemical composition of tiny shells built by
organisms (foraminifera) that had
lived in the water column and at the
sea bottom before their shells became embedded in the seafloor sediments.
Sea spray is a complex mixture of inorganic salts, organic material present in the ocean and
living organisms such as bacteria, viruses and fungi.
A throng of reef - dwelling
organisms live on the edge of the Gulf of Mexico's continental shelf some 200 kilometers offshore, from corals in the shallower regions to sponges,
sea fans and other soft corals, and numerous fish species in the deep.
That began to change last year with the discovery of DNA sequences for an
organism that no one has ever actually seen
living near a deep -
sea vent on the ocean floor.
If the structure of Martian water is highly pressurised, perhaps we might expect to find
organisms adapted to high pressure
life similar to piezophiles on Earth, such as deep
sea bacteria and other
organisms that thrive at high pressure.
«The discovery of microscopic shells of
organisms that
lived in warm shallow
seas, and of spores and pollen from land plants, reveal that the geography and climate of Zealandia were dramatically different in the past.»
What we see as a mere light in the
sea is a phenomenon occurring in nearly all the
organisms living in the
seas and oceans, from bacteria to large fish, and which impacts the behaviour and dynamics of the entire system.
Using the most comprehensive conservation data available for both marine and non-marine
organisms, research led by Dr Thomas Webb, from the University's Department of Animal and Plant Sciences, has shown that 20 to 25 per cent of the well - known species
living in our
seas are now threatened with extinction — the same figure as land
living plants and animals.
For decades marine biologists have gotten glimpses of this glittering
life by casting nets and retrieving deep -
sea organisms.
In a new study recently published in the journal Global Biogeochemical Cycles, scientists of Kiel University (CAU) with colleagues from GEOMAR Helmholtz Centre for Ocean Research Kiel and international partners from the USA, New Zealand, and Great Britain studied marine benthic shell - forming
organisms around the world in relation to the chemical conditions they currently experience — with a surprising result: 24 percent, almost a quarter of the analyzed species, including
sea urchins,
sea stars, coralline algae or snails, already
live in seawater unfavorable to the maintenance of their calcareous skeletons and shells (a condition referred to as CaCO3 - undersaturation).
To untangle the impacts that these three climate stressors will have on seafloor diversity in the future, the researchers examined existing published data and collected new data on
organisms living in deep -
sea sediments in upwelling regions along continental margins, where the ocean and continental crusts meet along the seafloor.
During this time, large (up to meter - sized) soft - bodied
organisms, often shaped like discs or fronds, had
lived on or in shallow horizontal burrows beneath thick mats of bacteria which, unlike today, coated the
sea floor.
Van Dover is a specialist in the ecology of deep -
sea ecosystems that are powered by chemistry rather than sunlight, and Eggleston studies the ecology of
organisms that
live on the seafloor.
They studied regenerative capacity in three species of
sea urchins with long, intermediate and short
life expectancies: the red
sea urchin, Mesocentrotus franciscanus, one of the world's longest -
lived organisms with a
life expectancy of more than 100 years; the purple
sea urchin, Strongylocentrotus purpuratus, with a
life expectancy of more than 50 years; and the variegated
sea urchin, Lytechinus variegatus, with a
life expectancy of only four years.
Hundreds of studies on bottom trawl impacts, including those on soft sediment habitats, have shown that trawling can remove or damage structure - forming
organisms, alter the composition of communities
living in the
sea bed (infauna) and reduce their productivity.
«These are the same precursors seen in biominerals from
sea urchin and abalone, which are different
organisms from completely different branches in the tree of
life, so the fact that they used exactly the same mechanism to form their skeletons is really surprising,» Gilbert explains.
The bottom of the
sea is a biologist's wonderland, but scientists are only beginning to understand the even more mysterious
organisms that
live deep under its floorboards.
«We know very little about deep -
sea organisms and their
life - cycle patterns, in particular in the water column of the deep
sea,» Hoving says.
Microbes such as bacteria are the most numerous
organisms on Earth, and about 90 % of them
live in sediments buried under the
sea floor.
The archaea, single - celled
organisms confused with bacteria until Dr. Woese's discovery, are of interest to biologists studying the origin of
life because they have certain primitive features and a liking for extreme environments, like the boiling springs of Yellowstone National Park and the superheated waters that swirl from deep -
sea volcanoes.
Scientists think Titan may also be able to support microbial
life (though if that
life teems in the hydrocarbon
seas, it will be very different than
organisms here on Earth).
But a siphonophore colony is made up of many parts that are each equivalent to free
living organisms such as
sea anemones and «true» jellyfish.
Marine mollusks can embed photonic structures into their curved shells without compromising shell strength; deep
sea sponges evolved fiber optic cables to direct light to symbiotically
living organisms; and brittlestars cover their skeletons with lenses to focus light into the body to «see» at night.
While a 300 - year - old tubeworm sounds impressive, it wouldn't be the longest
living organism on Earth, or even in the
sea.
This same «web of
life» was thought to exist in the
sea, whereby the carcasses or feces of
organisms living in the euphotic, or lighted, region of the
seas, descended to the bottom where they became a source of food for bottom dwellers.
Because this food supply was limited, it was thought that the numbers of
organisms living in the deep -
sea were limited.
The carbon captured by
living organisms in oceans is stored in the form of biomass and sediments from mangroves, salt marshes,
sea grasses and potentially algae.»
Up until this time, it was thought that
organisms living in the deep
sea depended on a constant «rain» of food from above, i.e. from the lighted regions of the ocean.
An international study to understand and predict the likely impact of ocean acidification on shellfish and other marine
organisms living in
seas from the tropics to the p...
From the opening on the
sea floor to a few feet away from the vent, a temperature gradient is formed along which different
organisms might
live, depending on their temperature preference.
We will enclose in these mesocosms all the
organisms that
live in the
sea water, including bacteria and plankton and will subject each bag to a different CO2 level in order to mimic what will happen up to 2100.
«The discovery of microscopic shells of
organisms that
lived in warm shallow
seas, and of spores and pollen from land plants, reveal that the geography and climate of Zealandia were dramatically different in the past,» adds co-chief scientist Gerald Dickens.
Amoeba - like tiny
organisms that
live in the
sea.
The carbonate sand (of which the beaches are made) is composed of broken skeletal fragments of the
organisms that
live in the reef and on the
sea floor behind the reef.
THE OLDEST
LIVING THINGS IN THE WORLD Rachel Sussman, essays by Carl Zimmer and Hans Ulrich Obrist University of Chicago Press Price: $ 45 A bulbous green blob of flowering plants in the Chilean desert and a «living fossil» in Namibia that resembles a collapsed sea monster — these are a few of the organisms Rachel Sussman photographed for this fascinating
LIVING THINGS IN THE WORLD Rachel Sussman, essays by Carl Zimmer and Hans Ulrich Obrist University of Chicago Press Price: $ 45 A bulbous green blob of flowering plants in the Chilean desert and a «
living fossil» in Namibia that resembles a collapsed sea monster — these are a few of the organisms Rachel Sussman photographed for this fascinating
living fossil» in Namibia that resembles a collapsed
sea monster — these are a few of the
organisms Rachel Sussman photographed for this fascinating book.
Food for thought, at the end of the Permian period, about 250 million years ago, approximately 90 % of
life in the
seas and 70 % of land dwelling
organisms went extinct.
And the loss of the
sea ice will mean the loss of an entire ecosystem, with repercussions that could include a major food chain, because of
organisms that
live on the underside of the
sea ice.
The first data series — from calcareous shells of marine
organisms that
live 50 to 200 metres below the
sea surface in the northern Atlantic — shows the temperature conditions there.
But seen the environmental global CRISIS of GLOBAL WARMING and its devastating climatological impact, I would recommend as an environmental policy - expert that Both NATURAL plankton will be bred in shallow waters as carbondioxide inhibitors in a large volume on the one hand and let nature goes its course in the
seas and oceans so that
sea -
organisms /
life - forms / mamals will not become extinct due to (for them) food poisoning.
Now imagine all of that — and all the plastic you deal with tomorrow, and the next day, and the nest — all of it here thousands of years from now, existing not only across land and
sea, but in the bodies of
living organisms.
Most Antarctic marine
organisms, from microscopic phytoplankton to the Adélie penguin, depend on
sea ice to
live and reproduce.
Sea - ice biome - The biome formed by all marine organisms living within or on the floating sea ice (frozen sea water) of the polar ocea
Sea - ice biome - The biome formed by all marine
organisms living within or on the floating
sea ice (frozen sea water) of the polar ocea
sea ice (frozen
sea water) of the polar ocea
sea water) of the polar oceans.
Background Ocean acidification is considered by climate alarmists to be detrimental to nearly all
sea creatures; and the early
life - stages of these
organisms are generally thought to be the most sensitive stages to this environmental change.
If that will have any impact on
sea life is doubtful as the main calcifying
organisms evolved at much higher CO2 levels during the Cretaceous, witnessed by the white cliffs of Dover and many such places all over the world...
Organisms living in areas where upwelling of cool, low pH water occurs (e.g. Eastern Pacific and Baltic
Sea) may be acclimatized / adapted to acidification [31 — 34], whereas those
living in areas with strong warming (e.g. Eastern Australia) may be acclimatized / adapted to increased temperature [7,35].
What they brought back are some of the most fascinating photographs of Antarctic
sea life ever seen — portraits of
organisms on the front - line of global climate change.