Watch 7000 years ago it was pretty hot !
Dry air contains roughly (by volume) 78.08% nitrogen, 20.95% oxygen, 0.93% argon, 0.038% carbon dioxide, and trace amounts of other gases. Air also contains a variable amount of water vapor, on average around 1%.
( Above 2,000 PPM, CO2 starts to become toxic to plants and above 4,000 PPM it becomes toxic to people. )
78% - Nitrogen
21% - Oxygen
1% - Argon
380 ppm CO2 0.038%
scientists are fairly certain that a 100 million years ago carbon dioxide values were many times higher than now.
long-term reconstructions of atmospheric CO2 levels going back in time show that 500 million years ago atmospheric CO2 was some 20 times higher than present values. It dropped, then rose again some 200 million years ago to 4-5 times present levels--a period that saw the rise of giant fern forests--and then continued a slow decline until recent pre-industrial time.
History of Atmospheric CO2 through geological time (past 550 million years: from Berner, Science, 1997). The parameter RCO2 is defined as the ratio of the mass of CO2 in the atmosphere at some time in the past to that at present (with a pre-industrial value of 300 parts per million). The heavier line joining small squares represents the best estimate of past atmospheric CO2 levels based on geochemical modeling and updated to have the effect of land plants on weathering introduced 380 to 350 million years ago. The shaded area encloses the approximate range of error of the modeling based on sensitivity analysis. Vertical bars represent independent estimates of CO2 level based on the study of ancient soils.
How much greenhouse gas was there in the ancient atmosphere? A 1993 model by Jim Kasting of Pennsylvania State University estimates that carbon dioxide (CO2) levels in the Earth's early atmosphere must have been 10 times to as much as 10,000 times today's level, in order to compensate for the young (and fainter) sun. Now, a measurement of the fossil record using a new instrument has confirmed a portion of the model. Atmospheric CO2 level 1.4 billion years ago was at least ten to 200 times greater than today, according to the new research.
The findings are reported in the September 18, 2003, issue of Nature by Alan Jay Kaufman of the geology department at the University of Maryland and Shuhai Xiao of the geosciences department at Virginia Tech ("High CO2 levels in the Proterozoic atmosphere estimated from analyses of individual microfossils").
So presently the co2 levels are at lowest levels …. ??
Having a closer look in a few 100 thousand years the Atmospheric CO2 looks like …
Plants would benefit from more CO2 in the air today, and actually are benefitting as we burn more fuels, one by-product being carbon dioxide. CO2 in the air has increased from 270 PPM to over 300 PPM, more than an 11% increase, in just the last 40 years!
Trees grow better at higher CO2 levels. Artificially “ green houses “ are created in polythene tents with high CO2 gas in them.
Biologists and plant physiologists have long recognized the benefits of higher CO2 content in the air for plant growth. Horticulturists and greenhouse growers have used CO generators to enhance growth rates on plants for many years with good results.
With the advent of home greenhouses and indoor growing under artificial lights and the developments in hydroponics in recent years, the need for CO2 generation has drastically increased. Plants growing in a sealed greenhouse or indoor grow room will often deplete the available CO2 and stop growing. The following graph will show what depletion and enrichment does to plant growth:
Below 200 PPM, plants do not have enough CO2 to carry on the photosynthesis process and essentially stop growing. Because 300 PPM is the atmospheric CO content, this amount is chosen as the 100% growth point. You can see from the chart that increased CO can double or more the growth rate on most normal plants. Above 2,000 PPM, CO2 starts to become toxic to plants and above 4,000 PPM it becomes toxic to people.
Dry air contains roughly (by volume) 78.08% nitrogen, 20.95% oxygen, 0.93% argon, 0.038% carbon dioxide, and trace amounts of other gases. Air also contains a variable amount of water vapor, on average around 1%.
The largest consumer of carbon dioxide (and maker of oxygen) is not trees, it's planktons in the sea.
Most people think that most of our oxygen comes from trees. But with two-thirds of the Earth's surface covered with water, it actually comes from oceans full of plant plankton, who dutifully convert 94% of CO2 to oxygen through photosynthesis.
[ So theoretically even if all the trees of the world is cut off, it hardly affects the Oxygen balance ! while oil spill or sea mining is very injurious to marine life and planktons, thus to oxygen recycling ]
Temperatures over the last 4.6 billion years
So several times the average temp of Earth became hotter and cooler due to environmental reasons.
Permian extinction 250 million years ago, when about 90% of all species died out. This was much more serious extinction than the "end of the age of the dinosaurs", in which about half of all species died out.
Dinosaur extinction at the end of the Cretaceous was only one of the 5 big extinctions life on Earth has suffered throughout the Phanerozoic eon, which began with the Cambrian period 540 million years ago. You can see the "Big Five" as sudden declines in this graph of biodiversity:
This graph shows how many "families" of marine animals there have been as a function of time. A "family" is a grouping of organisms that's bigger than a genus but smaller than an order.
It is “ high “ human ego to “ preserve “ the status quo. Even though in past due to geological / natural reasons so many species died / got extinct, today most humans would like to see all the species around itself as thriving.
Same thought process works for CO2 levels or Temperature. The status quo must be maintained and nothing should change is the “ common “ opinion.
- The Ordovician-Silurian Extinction, 440-450 million years ago at the end of the Ordovician Period.
27% of all families and 57% of all genera went extinct.
This was the second biggest extinction of marine life, ranking only below the Permian extinction. There was only life in the seas at this time, and more than one hundred families of marine invertebrates died, including two-thirds of all brachiopod and bryozoan families. One theory is that as the continent Gondwana drifted over the south pole, there was a phase of global cooling, and so much glaciation took place that sea levels were drastically lowered.
- The Devonian Extinction, 375 million years ago at the end of the Frasnian Age in the later part of the Devonian Period.
19% of all families and 50% of all genera went extinct.
By this point there were plants, insects and amphibians on land, fish in the seas, and huge reefs built by corals and stromatoporoids. The continents of Uramerica and Gondwana were just beginning to move together to form Pangea. The extinction seems to have only affected marine life, but 70% of marine species went extinct! Reef-building organisms were almost completely wiped out, so that coral reefs returned only with the development of modern corals in the Mesozoic. Brachiopods, trilobites, and other sorts got hit hard. Since warm water species were the most severely affected, many scientists suspect another bout of global cooling. There may have also been a meteorite impact, but it seems this extinction was not a sudden event.
- The Permian-Triassic Extinction, 251 million years ago at the end of the Permian Period.
57% of all families and 83% of all genera went extinct.
Temperatures over the last 65 million years
This shows the Earth's temperature since the extinction of the dinosaurs about 65 million years ago - the end of the Mesozoic and beginning of the Cenozoic.
Global ice mass over the last 6 million and 1 million years
The amount of ice is estimated by the amount of oxygen-18. In these charts up means "cold"!
Ocean temperatures over the last 2.5 million years
These temperatures are estimated by the amount of oxygen-18;
The larger fluctuations are Ice Ages, mostly during the Pleistocene Epoch, which began 1.8 million years ago.
Temperatures over the last 1.35 million years
Temperatures over the last 1 million, 150 thousand, 16 thousand and 150 years
Sea levels over the last 150,000 years
Higher sea levels correspond to warmer temperatures, since these make the ice caps melt.
The dip in sea levels from 120 to 20 thousand years ago is due to the last Ice Age.
Greenland temperatures over the last 130,000 years
Greenland temperatures over the last 100,000 years
So since 10,000 years it is HOT ….
Greenland temperatures over the last 18,000 years
So since 10,000 years it is HOT ….
Now the details ( To see very recent local variation )
Temperature in the Northern Hemisphere over the last 1000 years
The warming since 1850 is evident here, as is the "Little Ice Age" around 1450
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