Construct · 1 fields · 1 citations

Cretaceous-Paleogene mass extinction: a standalone construct

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Cretaceous-Paleogenemass extinction1 CONSTRUCTCretaceous-PaleogeneSCHULTE · PALEONTOLOGY

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Paleontology

mass extinction about 66 million years ago, including non-avian dinosaurs, linked to the Chicxulub impact.

In paleontology, Cretaceous-Paleogene mass extinction refers to mass extinction about 66 million years ago, including non-avian dinosaurs, linked to the Chicxulub impact. This meaning comes from Schulte (2010) in Science.[1]

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Nearby constructs

Alvarez impact hypothesis1 fields · 1 citationsanchor · a standalone constructextinction4 fields · 5 citationsjingle · one word, four constructsimpact6 fields · 11 citationsjingle · one name, six constructs

References

  1. Schulte, P., Alegret, L., Arenillas, I., Arz, J. A., Barton, P. J., Bown, P. R., Bralower, T. J., Christeson, G. L., Claeys, P., Cockell, C. S., Collins, G. S., Deutsch, A., Goldin, T. J., Goto, K., Grajales-Nishimura, J. M., Grieve, R. A. F., Gulick, S. P. S., Johnson, K. R., Kiessling, W., Koeberl, C., Kring, D. A., MacLeod, K. G., Matsui, T., Melosh, J., Montanari, A., Morgan, J. V., Neal, C. R., Nichols, D. J., Norris, R. D., Pierazzo, E., Ravizza, G., Rebolledo-Vieyra, M., Reimold, W. U., Robin, E., Salge, T., Speijer, R. P., Sweet, A. R., Urrutia-Fucugauchi, J., Vajda, V., Whalen, M. T., & Willumsen, P. S. (2010). The Chicxulub Asteroid Impact and Mass Extinction at the Cretaceous-Paleogene Boundary. Science, 327(5970), 1214-1218. https://doi.org/10.1126/science.1177265

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