Skip to main content

IMIS

A new integrated search interface will become available in the next phase of marineinfo.org.
For the time being, please use IMIS to search available data

 

[ report an error in this record ]basket (1): add | show Print this page

one publication added to basket [338075]
An extraterrestrial trigger for the mid-Ordovician ice age: dust from the breakup of the L-chondrite parent body
Schmitz, B.; Farley, K.A.; Goderis, S.; Heck, P.R.; Bergström, S.M.; Boschi, S.; Claeys, P.; Debaille, V.; Dronov, A.; van Ginneken, M.; Harper, D.A.T.; Iqbal, F.; Friberg, J.; Liao, S.; Martin, E.; Meier, M.M.M.; Peucker-Ehrenbrink, B.; Soens, B.; Wieler, R.; Terfelt, F. (2019). An extraterrestrial trigger for the mid-Ordovician ice age: dust from the breakup of the L-chondrite parent body. Science Advances 5(9): eaax4184. https://hdl.handle.net/10.1126/sciadv.aax4184
In: Science Advances. AAAS: New York. e-ISSN 2375-2548, more
Peer reviewed article  

Available in  Authors 

Authors  Top 
  • Schmitz, B.
  • Farley, K.A.
  • Goderis, S., more
  • Heck, P.R.
  • Bergström, S.M.
  • Boschi, S.
  • Claeys, P., more
  • Debaille, V., more
  • Dronov, A.
  • van Ginneken, M., more
  • Harper, D.A.T.
  • Iqbal, F.
  • Friberg, J.
  • Liao, S.
  • Martin, E.
  • Meier, M.M.M.
  • Peucker-Ehrenbrink, B.
  • Soens, B., more
  • Wieler, R.
  • Terfelt, F.

Abstract
    The breakup of the L-chondrite parent body in the asteroid belt 466 million years (Ma) ago still delivers almost a third of all meteorites falling on Earth. Our new extraterrestrial chromite and 3He data for Ordovician sediments show that the breakup took place just at the onset of a major, eustatic sea level fall previously attributed to an Ordovician ice age. Shortly after the breakup, the flux to Earth of the most fine-grained, extraterrestrial material increased by three to four orders of magnitude. In the present stratosphere, extraterrestrial dust represents 1% of all the dust and has no climatic significance. Extraordinary amounts of dust in the entire inner solar system during >2 Ma following the L-chondrite breakup cooled Earth and triggered Ordovician icehouse conditions, sea level fall, and major faunal turnovers related to the Great Ordovician Biodiversification Event.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors