Using god for science is wrong.Materials be came present after the big bang as atoms.Eventually processes started which created rock.Our planet came together with many materials, such as gold, platinum and others.When a rainforest dies when it dries up, gets buried and compresses to form coal.Oil is made
from sea organisms that die and get buried.The brain uses algorithms to process information.God does not need to be included.
Not exact matches
All
organisms eventually die and are decomposed by microorganisms which return the mineral nutrients, that are broken down
from their tissues, back to the soil or river or
sea.
We started finding the same
organisms that people were reporting
from deep -
sea hydrothermal vents [where hot, mineral - laden fluid flows through volcanic rock into the ocean
from deep within the Earth].
2017 revealed some surprising biology of
organisms large and small,
from quick - dozing elephants to sex - changing lizards and carbon - dumping
sea creatures.
This means they could spread microplastic pollution throughout the marine ecosystem, by carrying microplastics
from the surface down to deeper waters, affecting deep -
sea organisms.
Excess amounts
from human activities often end up in rivers, streams and coastal environments, causing algal blooms, loss of
sea grass and low oxygen levels in the water, which can kill large numbers of fish and other
organisms.
The team were able to draw these conclusions by analysing new data
from the chemical composition of the fossilised shells of
sea surface and seafloor
organisms from that period, taken
from drilling cores
from the ocean floor in the South Atlantic.
In 1998, a bot known as ROPOS («Remotely Operated Platform for Ocean Science») sawed a black smoker free
from the
sea floor and hauled it up to allow scientists to examine its structure and unique
organisms.
Organisms ranging
from sea anemone to humans utilize RNA editing to express different mRNAs at various times in development.
The team collected aquatic
organisms from the
sea floor and placed them in cages underwater.
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.
The original samples were excavated
from the deep
sea, where oxygen is scarce and the
organisms» metabolism is extremely slow.
«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.
Most
sea sponges feed on single - celled
organisms, which they filter
from water, but some are more voracious, catching small crustaceans.
If the marine
organisms had been scooped up
from below
sea level and dumped on the elevated promontory, something much bigger than a storm surge must have pounded the coast of ancient Crete.
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.
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).
For years, scientists have been unable to reconcile the nutritional requirements of crustaceans,
sea cucumbers, snails, and tube worms nearly a mile beneath the surface with the amount of nourishment — microscopic
organisms and other organic matter — that rains down
from above.
Scientists have been isolating marine natural compounds
from sea sponges and other marine
organisms to find treatments for diseases such as cancer and tuberculosis.
«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.
Simultaneous sequence analysis of all
organisms in filtered samples
from the Sargasso
Sea indicates the presence of over 1800 species, with unexpectedly large microbial diversity.
«The patterns we know
from coastal and shallow - water
organisms may not apply to deep -
sea species.
The ocean waters that are cleared of
sea ice by strong winds blowing
from the coast carve out a suitable enclave where marine
organisms can thrive, unlike the rest of the icy cold Antarctic region.
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.
Those same sediments held another clue as well — the fossilized shells of plankton (small floating
sea organisms)
from the dinosaur days.
bacteria Microscopic, single - celled
organisms that dwell nearly everywhere on Earth,
from the bottom of the
sea to inside animals.
Evidence
from Southwestern deserts suggests that oxygen - breathing
organisms arose on land rather than in the
seas.
But in
sea water, the gas reacts to produce carbonic acid - a threat for
organisms building their shells and skeletons
from calcium carbonate.
These tools will help to better understand ongoing changes in chemical and biological state of the North
Sea from alkalinity fluxes originating
from the Wadden
Sea over a synthesis model that integrates OA sensitivities at
organism level into a North
Sea ecosystem model (5.1) to an economical impact assessment.
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 prefere
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 prefere
from the vent, a temperature gradient is formed along which different
organisms might live, depending on their temperature preference.
«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.
The
organism is now infecting whales, dolphins, seals, and
sea lions
from the Arctic to Australia; and is a major cause of death in California
sea otters.
Marine biologist and University of California, Santa Barbara (UCSB) professor Dr. Gretchen Hofmann discussed how marine
organisms in the Santa Barbara Channel are adapting to a changing ocean environment, during the January
From Shore to
Sea lecture.
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.
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.
It should also be pointed out that the
sea temp along the GBR varies quite a bit
from its most northerly point to its most southerly, and in general is much cooler than reefs further into the tropics along Indonesia and PNG with almost identical species of coral and marine
organisms.
The recent marine biota in the Mediterranean
Sea is primarily derived
from the Atlantic Ocean, but the wide range of climate and hydrology have contributed to the co-occurrence and survival of both temperate and subtropical
organisms [18], [19].
Sea organisms have already more than enough CO2
from the surrounding waters, but the effect of a 100 % increase of CO2 in the atmosphere is only a 10 % increase in total CO2 in the surface waters.
In New Bedford, Mass., upward of 80 percent of fishing revenues come
from sea scallops, another shelled
organism that may be threatened by increasingly corrosive waters.
The conclusion is based on a finding that bromine and iodine oxide, natural chemicals produced by
sea spray and emissions
from microscopic
sea organisms, destroyed ozone in the atmosphere west of equatorial Africa — destroyed 50 % more ozone than than expected.
From sharks to whales, giant clams,
sea turtles, and tuna, the disproportionate threat to larger marine
organisms reflects the «unique human propensity to cull the largest members of a population,» the authors write.
The above quote
from it references a 2007 study, «Climate - related increases in jellyfish frequency suggest a more gelatinous future for the North
Sea,» that points out acidification will «severely affect calcifying plankton and other skeleton - forming
organisms, so would potentially favor noncalcifying
organisms such as jellyfish.»