Pariuda Kapur atawa Cretaceous adalah salah sabuting pariuda di jangka waktu giulugi nang bamula di akhir pariuda Jura wan balangsung sampai panambayan jaman Paleosen atawa kira-kira 145,5 ± 4 sampai 65,5 ± 0,3 juta tahun nang dahulu. Pariuda naya adalah pariuda giulugi nang paling lawas wan mancapai parak satangah matan eraMesozoikum. Akhir pariuda naya manandai batas matan Mesozoikum wan Kenozoikum.
Neal L Larson, Steven D Jorgensen, Robert A Farrar and Peter L Larson. Ammonites and the other Cephalopods of the Pierre Seaway. Geoscience Press, 1997.
Ogg, Jim; June, 2004, Overview of Global Boundary Stratotype Sections and Points (GSSP's)http://www.stratigraphy.org/gssp.htm Accessed April 30, 2006.
Ovechkina, M.N. and Alekseev, A.S. 2005. Quantitative changes of calcareous nannoflora in the Saratov region (Russian Platform) during the late Maastrichtian warming event. Journal of Iberian Geology31 (1): 149-165. PDF
Rasnitsyn, A.P. and Quicke, D.L.J. (2002). History of Insects. Kluwer Academic Publishers. ISBN 1-4020-0026-X.Periksa nilai tanggal di: |year= (bantuan)Pemeliharaan CS1: Banyak nama: authors list (link)
Skinner, Brian J., and Stephen C. Porter. The Dynamic Earth: An Introduction to Physical Geology. 3rd ed. New York: John Wiley & Sons, Inc., 1995. ISBN 0-471-60618-9}
Stanley, Steven M. Earth System History. New York: W.H. Freeman and Company, 1999. ISBN 0-7167-2882-6
Taylor, P.D. and Wilson, M.A., 2003. Palaeoecology and evolution of marine hard substrate communities. Earth-Science Reviews 62: 1-103.Archived 2009-03-25 at the Wayback Machine