Impact production of CO2 by the Cretaceous/Tertiary extinction bolide and the resultant heating of the earth

Computer Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

52

Atmospheric Composition, Atmospheric Moisture, Bolides, Carbon Dioxide Concentration, Atmospheric Temperature, Greenhouse Effect

Scientific paper

Various observations and data demonstrate that sea level at the end of the Cretaceous was 150-200 m higher than at present, suggesting the possibility that the extinction bolide struck a shallow marine carbonate-rich sedimentary section. It is shown here that the impact of such a bolide (about 5 km in radius) onto a carbonate-rich terrane would increase the CO2 content of the atmosphere by a factor of two to ten. Additional dissolution of CO2 from the ocean's photic zone could release much larger quantities of CO2. The impact-induced release of CO2, by itself, would enhance atmospheric greenhouse heating and give rise to a worldwide increase in temperature from 2 K to 10 K for periods of 10,000 to 100,000 years.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Impact production of CO2 by the Cretaceous/Tertiary extinction bolide and the resultant heating of the earth does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Impact production of CO2 by the Cretaceous/Tertiary extinction bolide and the resultant heating of the earth, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Impact production of CO2 by the Cretaceous/Tertiary extinction bolide and the resultant heating of the earth will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1527407

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.