USGS - science for a changing world

Understanding Our Planet Through Chemistry

Air Bubbles, Amber, and Dinosaurs

picture of mosquito trapped in amber
Amber --the fossilized resin of conifer trees-- provides a unique means of protecting intricate samples of the past. This mosquito, lying trapped for 45 million years in a piece of amber, is almost perfectly preserved. [148k]

Ages of ice samples found on the Earth cover a span approaching 200,000 years. But how can we tell what the Earth s atmosphere was like before that? Recently, USGS scientists have used a gas QMS to determine the oxygen level of ancient samples of Earth's atmosphere from a most unlikely place amber. The fossilized resin of conifer trees, amber is interesting to scientists as a medium that traps insects, small animals, and plants, preserving them through geologic time for future study.

image of air bubble trapped in amber

The recent extraction by scientists, of ancient DNA from organisms entombed in amber much like in the science-fiction novel and movie, Jurassic Park is an example of why scientists are intensely interested in amber. Minute bubbles of ancient air trapped by successive flows of tree resin during the life of the tree are preserved in the amber. Analyses of the gases in these bubbles show that the earth s atmosphere, 67 million years ago, contained nearly 35 percent oxygen compared to present levels of 21 percent. Results are based upon more than 300 analyses by USGS scientists of Cretaceous, Tertiary, and recent-age amber from 16 world sites.* The oldest amber in this study is about 130 million years old.

The consequences of an elevated oxygen level during Cretaceous time are speculative. Did the higher oxygen support the now extinct dinosaurs? Their demise was gradual in the transition from late Cretaceous to early Tertiary times, as was the decrease in oxygen content of the atmosphere.

* Citations

Landis, G.P., Rigby, J.K.,Jr., Sloan, R.E., Hengst, R.A., and Snee, L.W., 1996, Pelé Hypothesis: Ancient atmospheres and geologic-geochemical controls on evolution, survival, and extinction, in G. Keller and N. MacLeod, eds., Cretaceous-Tertiary Mass Extinctions. Biotic and Environmental Changes, W.W. Norton, pp. 519-556.

Landis, G.P., and Snee, L.W., 1991, 40Ar/39Ar Systematics and argon diffusion in Amber; implications for ancient earth atmospheres: in Kump, L.R., Kasting, J.F., Robinson, J.M., Atmospheric oxygen variation through geologic time. Global and Planetary Change. v. 5, p.63-67.

Chart showing major decrease atmospheric oxygen content at the boundary of Cretaceous to Tertiary time
This chart shows a major decrease in oxygen content in the atmosphere from 35 percent to the present day level of 21 percent. This decrease occured about the same time that the dinosaurs disappeared--65 million years ago. [51k]

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