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There was time during the age of dinosaurs when the polar regions were ice free. The earth was obviously much warmer but a run-away greenhouse effect did not occur.

This was most likely because the continents were so configured that ocean currents more adequately transfered heat around the globe. And The particulate dust from volcanic activity (more active back then) accumulated in the stratosphere, reflecting solar heat and light back into space.

One reason creatures of immense size such as dinosaurs were able to evolve is the oxygen requirements for the respiration and metabolism for such massive bodies were present in the atmosphere during this period.

Similarly, the fossil record indicates vegetation size was much greater during this period than today due to the higher amount of CO2.

This atmosphere would have to have greater percentage composition of oxygen (for dinosaurs) and CO2 (for greenhouse affect and greater plant biomass) or a much denser atmosphere or both.

What was the density of the atmosphere back then either in terms of air pressure at today's sea level and standard temperature Or In kg/square meter at STP (Standard Temperature and Pressure)?

What were the percentages of O2 and CO2?

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    $\begingroup$ I think you make a number of statements in your question that are questionable. For instance, the volcanic activity being enhanced during the Jurassic: earthscience.stackexchange.com/questions/3001/… or that the Jurassic was the "age of dinosaurs". The whole statement about ocean currents is difficult to support. Please provide references to support your statements $\endgroup$ – arkaia Oct 11 '17 at 18:01
  • $\begingroup$ Ok, pending. It's difficult on a smart phone $\endgroup$ – 0tyranny 0poverty Oct 11 '17 at 18:13
  • $\begingroup$ Note most of the super large sauropods lived in the jurassic not the cretaceous. $\endgroup$ – John Apr 4 at 23:26
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Recent analysis of the contents of air bubbles preserved in prehistoric amber reveal the oxygen composition to be 32% back then compared to just under 21% today. These tiny bubbles have remained trapped in these amber samples for about 80 million years, which dates them well into the Cretaceous era when dinosaurs and other huge creatures roamed the earth.

Said analysis also revealed that nitrogen made up the rest save 1% for Argon, CO2, and other trace gases. The percentage of CO2 was not specifically stated but mentioned as similar oxygen to CO2 ratio as today's atmosphere. Whether the total air pressure air density of the atmosphere was greater back then is not mentioned, most likely because this would be difficult to ascertain from the samples.

An atmosphere 50% richer in oxygen but at the same atmospheric pressure and density at sea level as today would have allowed land animals to get by with a lower lungs to total body mass ratio and thus allowed the existence of extra massive creatures such as dinosaurs.

I assert that the asteroid that struck the Yucatan area 65 million years ago caused most of the forests and other terrestrial vegetation to ignite into flames. The whole earth would have been on fire, at the end of which the oxygen levels were depleted to what they are today. This is confirmed by analysis amber air bubbles from 40 million years ago, post asteroid impact, revealing an atmospheric composition and oxygen levels closer to today's.

Dinosaurs and other massive terrestrial animals could not then make a comeback since the lower oxygen content of the atmosphere would have restricted metabolism to maintain massive body sizes.

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  • $\begingroup$ If you are saying that the oxygen was consumed by burning plants, I don't think that could be right. Globally living plants contain 500 billion metric tons of carbon.The total mean mass of the atmosphere is $5.1480×10^{18}$ kg . That is $5×10^{11}$ tons vs. $5×10^{15}$ tons. $\endgroup$ – Keith McClary Feb 3 '18 at 4:49
  • $\begingroup$ @KeithMcClary What about the total mass of fossil fuels? The carbon content of limestone and carbonates in the oceans and on land. The burnt remains of the vegetation plus the surge in CO2 levels would have been sequestered into these forms over the 65 million year period. The statistics of global plant life and atmospheric mass you referenced are for the present. Both were greater back in the Cretaceous. $\endgroup$ – 0tyranny 0poverty Feb 4 '18 at 13:59
  • $\begingroup$ Just FYI, your "Recent analysis" links to a New York Times article from October 28, 1987. $\endgroup$ – plannapus Feb 5 '18 at 9:59
  • $\begingroup$ Limestone and carbonates would not consume O2. This article has estimates of biomass burnt in another (lesser) impact. $\endgroup$ – Keith McClary Feb 6 '18 at 23:33
  • $\begingroup$ @KeithMcClary Limestone and carbonates consume CO2 which is the major end product of biomass burn, the other being H2O. $\endgroup$ – 0tyranny 0poverty Feb 8 '18 at 2:54
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To answer the $p_{CO_2}$ aspect of the question, here is a graph modified from Kent & Muttoni (2013):

graph showing cretaceous to modern pCO2 variations

It is based on compilations from Royer (2010) and Beerling & Royer (2011), using a wide variety of proxies, but mostly fossil leaves stomata for the Cretaceous. It might be a bit outdated now but most articles out there do give values on the same range: ca. 400~500 ppm at the Cretaceous-Paleogene boundary and values fluctuating between 500 and 1500 ppm before that, with a maximum during the mid-Cretaceous.

As for $p_{O_2}$, I couldn't find a recent compilation, but according to Poulsen et al. (2015), estimates for the Cenomanian (i. e. the high $p_{CO_2}$ period from the last graph) vary widely from 10% to (indeed as the other answer suggests) 32%. Here is the quote:

We focused on simulations of the Cenomanian, a mid-Cretaceous stage characterized by high $p_{CO_2}$ [e.g., (12)] and the warmest conditions of the past ~100 million years (13). Paleo-$p_{O_2}$ estimates inferred from stable-isotope carbon compositions indicate that the atmospheric percentage of $O_2$ was as low as 10 to 11% during this interval (7, 9), with one biogeochemical model indicating levels as high as 32.5% (6).

References 7 and 9 are to Falkowski et al. (2005) and Tappert et al. (2013), while reference 6 is to Bergman et al. (2004).

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