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Understanding rapid climate variations during the Late Ordovician in terms of astronomical forcing.
2015Cyclostratigraphy comprises the study of astronomically forced climate cycles as expressed in the sedimentary record. Such studies are particularly challenging when applied to the deep geological time. Recent studies (De Vleeschouwer & Parnell, 2014) however, have now successfully demonstrated the astronomical rhythm of climate changes as far as the ...
Sinnesael, Matthias +4 more
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Astronomically driven short-term climate change, a factor controlling Eocene turbidite accumulation
Rendiconti online della Società Geologica Italiana, 2014Payros, Aitor, Martinez-Braceras, Naroa
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2015
The Late Ordovician (450 million years ago) is characterized by major glaciations and a mass extinction event. The CO2 concentrations were up to ten times higher than today and there was a virtual lack of vegetation on the continents. Most of the land masses were located south of the equator and a gigantic ocean occupied the Northern Hemisphere.
Sinnesael, Matthias, Claeys, Philippe
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The Late Ordovician (450 million years ago) is characterized by major glaciations and a mass extinction event. The CO2 concentrations were up to ten times higher than today and there was a virtual lack of vegetation on the continents. Most of the land masses were located south of the equator and a gigantic ocean occupied the Northern Hemisphere.
Sinnesael, Matthias, Claeys, Philippe
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Long‐term astronomical cycles as a consequence of cyclic time structure
Journal of Interdisciplinary Cycle Research, 1977openaire +1 more source
Compensation of photon noise bias terms in speckle masking and astronomical applications
16th Congress of the International Commission for Optics: Optics as a Key to High Technology, 1993openaire +1 more source