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author Gulick, S.P.S.
Bralower, T.J.
Ormö, J.
Hall, B.
Grice, Kliti
Schaefer, Bettina
Lyons, S.
Freeman, K.H.
Morgan, J.V.
Artemieva, N.
Kaskes, P.
De Graaff, S.J.
Whalen, M.T.
Collins, G.S.
Tikoo, S.M.
Verhagen, C.
Christeson, G.L.
Claeys, P.
Coolen, Marco
Goderis, S.
Goto, K.
Grieve, R.A.F.
McCall, N.
Osinski, G.R.
Rae, A.S.P.
Riller, U.
Smit, J.
Vajda, V.
Wittmann, A.
author_facet Gulick, S.P.S.
Bralower, T.J.
Ormö, J.
Hall, B.
Grice, Kliti
Schaefer, Bettina
Lyons, S.
Freeman, K.H.
Morgan, J.V.
Artemieva, N.
Kaskes, P.
De Graaff, S.J.
Whalen, M.T.
Collins, G.S.
Tikoo, S.M.
Verhagen, C.
Christeson, G.L.
Claeys, P.
Coolen, Marco
Goderis, S.
Goto, K.
Grieve, R.A.F.
McCall, N.
Osinski, G.R.
Rae, A.S.P.
Riller, U.
Smit, J.
Vajda, V.
Wittmann, A.
author_sort Gulick, S.P.S.
building Curtin Institutional Repository
collection Online Access
description Highly expanded Cretaceous-Paleogene (K-Pg) boundary section from the Chicxulub peak ring, recovered by International Ocean Discovery Program (IODP)-International Continental Scientific Drilling Program (ICDP) Expedition 364, provides an unprecedented window into the immediate aftermath of the impact. Site M0077 includes ∼130 m of impact melt rock and suevite deposited the first day of the Cenozoic covered by <1 m of micrite-rich carbonate deposited over subsequent weeks to years. We present an interpreted series of events based on analyses of these drill cores. Within minutes of the impact, centrally uplifted basement rock collapsed outward to forma peak ring capped in melt rock. Within tens of minutes, the peak ring was covered in ∼40 m of brecciated impact melt rock and coarsegrained suevite, including clasts possibly generated by melt-water interactions during ocean resurge. Within an hour, resurge crested the peak ring, depositing a 10-m-thick layer of suevite with increased particle roundness and sorting.Within hours, the full resurge deposit formed through settling and seiches, resulting in an 80-m-thick fining-upward, sorted suevite in the flooded crater. Within a day, the reflected rim-wave tsunami reached the crater, depositing a cross-bedded sand-to-fine gravel layer enriched in polycyclic aromatic hydrocarbons overlain by charcoal fragments. Generation of a deep crater open to the ocean allowed rapid flooding and sediment accumulation rates among the highest known in the geologic record. The high-resolution section provides insight into the impact environmental effects, including charcoal as evidence for impactinduced wildfires and a paucity of sulfur-rich evaporites from the target supporting rapid global cooling and darkness as extinction mechanisms.
first_indexed 2025-11-14T11:33:32Z
format Journal Article
id curtin-20.500.11937-90119
institution Curtin University Malaysia
institution_category Local University
language English
last_indexed 2025-11-14T11:33:32Z
publishDate 2019
publisher NATL ACAD SCIENCES
recordtype eprints
repository_type Digital Repository
spelling curtin-20.500.11937-901192023-04-26T09:11:16Z The first day of the Cenozoic Gulick, S.P.S. Bralower, T.J. Ormö, J. Hall, B. Grice, Kliti Schaefer, Bettina Lyons, S. Freeman, K.H. Morgan, J.V. Artemieva, N. Kaskes, P. De Graaff, S.J. Whalen, M.T. Collins, G.S. Tikoo, S.M. Verhagen, C. Christeson, G.L. Claeys, P. Coolen, Marco Goderis, S. Goto, K. Grieve, R.A.F. McCall, N. Osinski, G.R. Rae, A.S.P. Riller, U. Smit, J. Vajda, V. Wittmann, A. Science & Technology Multidisciplinary Sciences Science & Technology - Other Topics Chicxulub impact crater suevite Cretaceous-Paleogene peak ring tsunami CRETACEOUS-PALEOGENE BOUNDARY POLYCYCLIC AROMATIC-HYDROCARBONS SUEVITE REVISITED-OBSERVATIONS CHICXULUB IMPACT EVENT GULF-OF-MEXICO TERTIARY BOUNDARY ONAPING FORMATION ASTEROID IMPACT RIES CRATER EXTINCTION Highly expanded Cretaceous-Paleogene (K-Pg) boundary section from the Chicxulub peak ring, recovered by International Ocean Discovery Program (IODP)-International Continental Scientific Drilling Program (ICDP) Expedition 364, provides an unprecedented window into the immediate aftermath of the impact. Site M0077 includes ∼130 m of impact melt rock and suevite deposited the first day of the Cenozoic covered by <1 m of micrite-rich carbonate deposited over subsequent weeks to years. We present an interpreted series of events based on analyses of these drill cores. Within minutes of the impact, centrally uplifted basement rock collapsed outward to forma peak ring capped in melt rock. Within tens of minutes, the peak ring was covered in ∼40 m of brecciated impact melt rock and coarsegrained suevite, including clasts possibly generated by melt-water interactions during ocean resurge. Within an hour, resurge crested the peak ring, depositing a 10-m-thick layer of suevite with increased particle roundness and sorting.Within hours, the full resurge deposit formed through settling and seiches, resulting in an 80-m-thick fining-upward, sorted suevite in the flooded crater. Within a day, the reflected rim-wave tsunami reached the crater, depositing a cross-bedded sand-to-fine gravel layer enriched in polycyclic aromatic hydrocarbons overlain by charcoal fragments. Generation of a deep crater open to the ocean allowed rapid flooding and sediment accumulation rates among the highest known in the geologic record. The high-resolution section provides insight into the impact environmental effects, including charcoal as evidence for impactinduced wildfires and a paucity of sulfur-rich evaporites from the target supporting rapid global cooling and darkness as extinction mechanisms. 2019 Journal Article http://hdl.handle.net/20.500.11937/90119 10.1073/pnas.1909479116 English https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6765282/ http://purl.org/au-research/grants/arc/DP180100982 NATL ACAD SCIENCES unknown
spellingShingle Science & Technology
Multidisciplinary Sciences
Science & Technology - Other Topics
Chicxulub impact crater
suevite
Cretaceous-Paleogene
peak ring
tsunami
CRETACEOUS-PALEOGENE BOUNDARY
POLYCYCLIC AROMATIC-HYDROCARBONS
SUEVITE REVISITED-OBSERVATIONS
CHICXULUB IMPACT EVENT
GULF-OF-MEXICO
TERTIARY BOUNDARY
ONAPING FORMATION
ASTEROID IMPACT
RIES CRATER
EXTINCTION
Gulick, S.P.S.
Bralower, T.J.
Ormö, J.
Hall, B.
Grice, Kliti
Schaefer, Bettina
Lyons, S.
Freeman, K.H.
Morgan, J.V.
Artemieva, N.
Kaskes, P.
De Graaff, S.J.
Whalen, M.T.
Collins, G.S.
Tikoo, S.M.
Verhagen, C.
Christeson, G.L.
Claeys, P.
Coolen, Marco
Goderis, S.
Goto, K.
Grieve, R.A.F.
McCall, N.
Osinski, G.R.
Rae, A.S.P.
Riller, U.
Smit, J.
Vajda, V.
Wittmann, A.
The first day of the Cenozoic
title The first day of the Cenozoic
title_full The first day of the Cenozoic
title_fullStr The first day of the Cenozoic
title_full_unstemmed The first day of the Cenozoic
title_short The first day of the Cenozoic
title_sort first day of the cenozoic
topic Science & Technology
Multidisciplinary Sciences
Science & Technology - Other Topics
Chicxulub impact crater
suevite
Cretaceous-Paleogene
peak ring
tsunami
CRETACEOUS-PALEOGENE BOUNDARY
POLYCYCLIC AROMATIC-HYDROCARBONS
SUEVITE REVISITED-OBSERVATIONS
CHICXULUB IMPACT EVENT
GULF-OF-MEXICO
TERTIARY BOUNDARY
ONAPING FORMATION
ASTEROID IMPACT
RIES CRATER
EXTINCTION
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6765282/
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6765282/
http://hdl.handle.net/20.500.11937/90119