[1] Shukolyukov A., Lugmair G.W., Isotopic evidence for the Cretaceous-Tertiary impactor and its type. Science, 1998, 282, 927–930 http://dx.doi.org/10.1126/science.282.5390.927CrossrefGoogle Scholar

[2] Wolbach W.S., Lewis R.S., Anders E., Cretaceous extinctions: evidence for wildfires and search for meteoritic material. Science, 1985, 230, 167–170 http://dx.doi.org/10.1126/science.230.4722.167CrossrefGoogle Scholar

[3] Wolbach W.S., Gilmour I., Anders E., Orth C.J., Brooks R.R., Global fire at the Cretaceous-Tertiary boundary. Nature, 1988, 334, 665–669 http://dx.doi.org/10.1038/334665a0CrossrefGoogle Scholar

[4] Wolbach W.S., Anders E., Nazarov M.A., Fires at the K-T boundary: carbon at the Sumbar, Turkmenia, site. Geochim. Cosmochim. Acta, 1990, 54, 1133–1146 http://dx.doi.org/10.1016/0016-7037(90)90444-PCrossrefGoogle Scholar

[5] Wolbach W.S., Gilmour I., Anders E., Major wildfires at the Cretaceous-Tertiary boundary. In: Sharpton B., Ward P. (Eds.), Global catastrophes in Earth history. Geological Society of America, Boulder, Special Paper 247, 1990, 391–400 Google Scholar

[6] Wolbach W.S., Widicus S.L., Kyte F.T., A search for soot from global wildfires in Central Pacific Cretaceous-Tertiary boundary and other extinction and impact horizon sediments. Astrobiology, 2003, 3, 91–97 http://dx.doi.org/10.1089/153110703321632444CrossrefGoogle Scholar

[7] Belcher C.M., Collinson M.E., Sweet A.R., Hildebrand A.R., Scott A.C., Constraints on the thermal energy released from the Chixculub impactor: new evidence from multi method charcoal analysis. J. Geol. Soc. London, 2005, 162, 591–602 http://dx.doi.org/10.1144/0016-764904-104CrossrefGoogle Scholar

[8] Gilmour I., Sephton M.A., Morgan J.V., Organic geochemistry of a hydrocarbon-rich calcarenite from the Chicxulub scientific drilling program. In: Proceedings of the 34th Lunar and Planetary Science Conference. Lunar and Planetary Institute, Houston, 2003, abs. 1771 Google Scholar

[9] Belcher C.M., Collinson M.E., Sweet A.R., Hildebrand A.R., Scott A.C., Fireball passes and nothing burnsthe role of thermal radiation in the K-T event: evidence from the charcoal record of North America. Geology, 2003, 31, 1061–1064 http://dx.doi.org/10.1130/G19989.1CrossrefGoogle Scholar

[10] Belcher C.M., Impacts and Wildfires 210 — An analysis of the K-T Event. In: Koeberl C., Gilmour I. (Eds.), Biological processes associated with impact events. Springer, Berlin, 2006, 221–243 http://dx.doi.org/10.1007/3-540-25736-5_10CrossrefGoogle Scholar

[11] Belcher C.M., Reigniting the Cretaceous-Palaeogene firestorm debate. Geology, 2009, 37, 1147–1148 http://dx.doi.org/10.1130/focus122009.1.CrossrefWeb of ScienceGoogle Scholar

[12] Harvey M.C., Brassell S.C., Belcher C.M., Montanari A., Combustion of fossil organic matter at the Cretaceous-Paleogene (K-P) boundary. Geology, 2008, 36, 355–358 http://dx.doi.org/10.1130/G24646A.1Web of ScienceCrossrefGoogle Scholar

[13] Ransohoff L.M., Knudson K., Bush B.W., Small R.D., Material inventories and smoke properties for U.S. target areas. Pacific-Sierra Research Corporation, Los Angeles, 1989 Google Scholar

[14] Turco R.P., Toon O.B., Ackerman T.P., Pollack J.B., Sagan C., Climate and smoke: an appraisal of nuclear winter. Science, 1990, 247, 166–176 http://dx.doi.org/10.1126/science.11538069CrossrefGoogle Scholar

[15] Shuvalov V.V., Artemieva N.A., Numerical modeling of Tunguska-like impacts. Planet. Space Sci., 2002, 50, 181–192 http://dx.doi.org/10.1016/S0032-0633(01)00079-4CrossrefGoogle Scholar

[16] Ebel D.S., Grossman L., Spinel-bearing spherules condensed from the Chicxulub impact-vapor plume. Geology, 2005, 33, 293–296 http://dx.doi.org/10.1130/G21136.1CrossrefGoogle Scholar

[17] Durda D.D., Kring D.A., Pierazzo E., Melosh H. J., Model calculations of the proximal and globally distributed distal ejecta from the Chicxulub impact crater. In: Proceedings of the 28th Lunar and Planetary Science Conference. Lunar and Planetary Institute, Houston, 1997, 315–316 Google Scholar

[18] Grajales-Nishimura J.M., Cedillo-Pardo E., Rosales-Domínguez C., Morán-Zenteno D.J., Alvarez W., Claeys P., Ruíz-Morales J., García-Hernández J., Padilla-Avila P., Sánchez-Ríos A., Chicxulub impact: the origin of reservoir and seal facies in the southeastern Mexico oil fields. Geology, 2000, 28, 307–310 http://dx.doi.org/10.1130/0091-7613(2000)28<307:CITOOR>2.0.CO;2CrossrefGoogle Scholar

[19] Heymann D., Yancey T.E, Wolbach W.S, Thiemens M.H, Johnson E.A, Roach D., Moecker S., Geochemical markers of the Cretaceous-Tertiary boundary event at Brazos River, Texas, USA. Geochim. Cosmochim. Acta, 1998, 62, 173–181 http://dx.doi.org/10.1016/S0016-7037(97)00330-XCrossrefGoogle Scholar

[20] Toon O.B., Zahnle K., Morrison D., Turco R.P., Covey C., Environmental perturbations caused by the impacts of asteroids and comets. Rev. Geophys., 1997, 35, 41–78 http://dx.doi.org/10.1029/96RG03038CrossrefGoogle Scholar

[21] Magoon L.B., Hudson T.L., Cook H.E., Pimienta-Tamabra(!)-a giant supercharged petroleum system in the southern Gulf of Mexico, onshore and offshore Mexico. In: Bartolini C., Buffler R.T., Cantu-Chapa A. (Eds.), The western Gulf of Mexico basin: tectonics, sedimentary basins, and petroleum systems. The American Association of Petroleum Geologists, USA, 75, 2001, 83–125 Google Scholar